A. CRUISE NARRATIVE - WOCE S04P (updated 8/1/05) A.1. HIGHLIGHTS WHP CRUISE SUMMARY INFORMATION WOCE section designation S04P Expedition designation (EXPOCODE) 90KDIOFFE6_1 Chief Scientists Mikhail H. Koshlyakov/Shirshov IO*, James G. Richman/OSU** Dates 1992.02.14 - 1992.04.06 Ship R/V Akademik Ioffe Ports of call Montevideo, Uruguay; Wellington, NZ Number of stations 113 CTD/rosette stations 65¡ 19.12' S Station geographic boundaries 70¡ 5.17' W 162¡ 39.91' E 70¡ 38.92' S Floats and drifters deployed none Moorings deployed or recovered none Contributing Authors Marie-Claude BeauprŽ ODF/SIO J.C. Jennings Robert M. Key Eugene Morozov Eugene Morozov ---------------------------------------------------------------------------------- * Russian Academy of Sciences ** Oregon State University P. Shirshov Institute of Oceanology College of Oceanic & Atmospheric Sciences Nakhimovski Ave. 36 Oceanography Admin. Bldg. 104 117218 Moscow RUSSIA Corvallis OR 97331-5503 Phone: 7-095-129-2363 Phone: 1-541-737-3328 Fax: 7-095-124-5983 Fax: 1-541-737-2064 e-mail: koshl@stream.sio.rssi.ru e-mail: jrichman@oce.orst.edu jr@oce.orst.edu A.2. Cruise Summary Cruise track The cruise track included WHP stations beginning on the continental shelf of the Antarctic Peninsula at 67¡ 28S 71¡ 5W on 22 February, 1992, continuing west along ca. 67¡S (S4 Pacific) at nominally 30 nautical mile intervals. The first ten stations were made along a northwesterly line approximately perpendicular to the continental slope with stations over the shelf break and slope located on isobaths separated by approximately 800 m. Over the Bellingshausen Abyssal Plain between 91¡34W and 130¡41W and over the Amundsen Abyssal Plain between 142¡11W and 157¡41W, the station spacing was increased to nominally 40 nautical miles. At 174¡15E, the track was turned southwestward to run perpendicular to the Antarctic continental shelf. The section was completed with a station in 200 m of water off Cap Daemon at 70¡39S 168¡04E. The section was restarted with a repeat station at 67¡S 174¡15E and continued east-northeast to end in 400 m of water off Young Island of the Balleny Islands at 66¡25S 162¡41E. The last station will be the eastern terminus for the continuation of WHP line S4 into the Indian Ocean. Stations occupied There were 113 CTD/rosette stations, in all but one case each close to the bottom. No large volume casts were made. There were 3 surface samples for Ge isotopes and one complete profile with 24 samples. Floats and drifters deployed No floats nor surface drifters were deployed. Moorings deployed or recovered No moorings were deployed or recovered. S04P ð Koshlyakov/Richman ð 1992 ð R/V Akademik Ioffe A.3. List of Principal Investigators Measurement Institution or Name responsibility affiliation -------------------------- -------------------- -------------------- A. Berezutski & J. Richman ADCP Shirshov Inst .& OSU A. Berezutski MultiBeam Bathymetry Shirshov Inst. J. Bullister CFCs PMEL G. Rau carbon isotopes NASA Ames Res Center P. Schlosser AMS 14C LDGO P. Schlosser helium, tritium LDGO P. Schlosser 18O LDGO J. Swift CTD/O2/nutrients SIO T. Takahashi & D. Chipman TCO2, pCO2 LDGO N. Voronina Biological sampling Shirshov Inst. A.4. Scientific Program a. Narrative The R/V Akademik Ioffe Cruise 6 (WHP line S4 Pacific) left Montevideo, Uruguay on 14 February, 1992 and ended in Wellington, New Zealand on 6 April, 1992. The chief Scientists were Mikhail H. Koshlyakov (Shirshov Institute of Oceanology) and James G. Richman (Oregon State University). The purpose of this cruise was to determine the strength and extent of the cyclonic circulation in the Pacific Ocean south of the Polar Front as part of the WOCE Hydrographic Program. The R/V Akademik Ioffe departed Montevideo at 2130 on 14 February 1992, and headed for deep water in the South Atlantic. On the morning of 17 February, the vessel stopped for training and station tests. No reportable data were collected. WHP stations began on the continental shelf of the Antarctic Peninsula 67¡28.1S 70¡05.4W on 22 February (station 682). The first six stations were over the continental shelf and slope along a northwesterly line. The stations over the slope were made on isobaths separated by approximately 800 m. Two more stations were made in deep water along this line and then the track was turned southwestward. Five stations were made along the southwesterly track until 67¡S was reached. The section was then continued along 67¡S at nominally 30 nautical mile spacing. Over the Bellingshausen Abyssal Plain between 91¡34W and 130¡41W and over the Amundsen Abyssal Plain between 142¡11W and 157¡41W, the station spacing was increased to nominally 40 nautical miles. At 174¡15E (station 768), the track was turned southwestward to run perpendicular to the Antarctic continental shelf. The section was completed with a station in 200 m of water off Cap Daemon at 70¡39S 168¡04E on 23 March (station 780). The section was restarted with a repeat station at 67¡S 174¡15E on 25 March and continued east-northeast to end in 400 m of water off Young Island of the Balleny Islands at 66¡25S 162¡41E on 29 March (station 794). The last station will be the eastern terminus for the continuation of WHP line S4 into the Indian Ocean. The principal sampling program consisted of full-depth CTD/O profiles with a maximum of 24 small-volume water samples per cast. Water samples were collected for salinity, dissolved oxygen, silicate, phosphate, nitrate, nitrite, CFC-11, and CFC-12 at all stations, and for 3He, tritium, AMS 14C, CFC-113, 18O, and CO2 system parameters at selected stations. Rosette water samples were collected by the Scripps Oceanographic Data Facility (ODF) from Niskin and ODF-constructed 10-liter sample bottles mounted on an ODF-constructed 24-bottle rosette sampler which used General Oceanics 24- place pylon. The rosette was equipped with ODF-modified NBIS Mark IIIb CTDs for in-situ measurement of conductivity, temperature, pressure, and dissolved oxygen. A transmissometer belonging to Dr. Wilf Gardner, TAMU, was installed on the rosette and used at several stations. A short-range (ca. 100 meter) altimeter was mounted on the rosette frame and its data fed into the CTD data stream. A pinger on the rosette frame gave height above bottom (via a PDR in the CTD console area) throughout the water column. In every case the bottles were closed at selected depths during the up cast, after the winch had stopped at that depth. There were 113 CTD/rosette stations, in all but one case each close to the bottom. Two PRTs were used on most stations for temperature measurements. No reversing thermometers were used during the cruise. Conductivities were measured using ODF Autosal salinometer with an automated logging program. Oxygen samples were run using a Dosimat/UV automatic titration system. Nutrients were run with a Technicon AAII system. While on station and underway a shipboard 75 kHz RDI ADCP system was operated. Underway surface measurements were also obtained: temperature, salinity, fluorescence and pCO2. A multi-beam sonar system was operated between stations Routine weather observations were collected at ten minute intervals by the ship's automated meteorological station with visual observations every four hours by the ship's officers. Along the section, the weather and sea conditions were moderate to very rough. The winds were generally 10-15 m/sec, with five days approaching or exceeding 20 m/sec. Icebergs were present during the entire section which necessitated slowing at night and some extra maneuvering before starting sections. The air temperature averaged slightly below freezing. Near Antarctica, at the end of the section, cold air and wind created problems with freezing in the bottle spigots (stations 773 and 778), but only three salinity samples were lost. No trouble with pack ice occurred during the section. The weather was extremely poor in the vicinity of the the Antarctic Circumpolar Current between the continent and New Zealand which prevented any work on the northward run after the completion of the main zonal section. b. Bottle depth distributions Vertical sections along the ship's track showing the depth distributions for small volume samples are shown in Figures 2 and 3. S04P ð Koshlyakov/Richman ð 1992 ð R/V Akademik Ioffe A.5. Problems This cruise had few problems. The CTD operations were made from the stern A-frame. There were numerous cable problems, kinking and unlaying, associated with the pitching in rough weather conditions when the winds exceeded 15 m/sec or large swells were encountered. Many mire reterminations were made during the cruise. However, little data was lost from these problems. One station, 701, was terminated early on 27 February at 3700 m in 4340m of water during bad weather and excessive ship motion. The rosette hit the ship during recovery stations 705 and 763. The CTD signal was lost at 3650 dbars on station 702 and the cast was aborted. However, the signal returned as the CTD was being raised and the cast was restarted in the water at 3100 dbars. The CTD signal was lost on the upcast at 4337 dbars on station 709. The bottles were tripped based upon wire out for this station. The same CTD was used for the entire cruise. The CTD Sampler Controller and Data Logger was tested from station 781 through station 794. Using the controller, bottles were tripped at preset depths and the CTD data recorded internally. The casts were monitored and data recorded with normal CTD computer. An oxygen sensor was used with the CTD. Problems with the sensor and its spare were encountered at the start of the section. The data are suspect for the first 11 stations (682-692). The sensor failed on station 773. No oxygen sensor was available for stations 773 through 782. The transmissometers had inside lens fogging and temperature compensation problems. Many casts had no transmissometer mounted and the data are suspect for the stations where one was used. South of the Polar Front, the acoustic backscatter sound levels for the 75 kHz ADCP were extremely low. The data from the upper 200 m appear to be contaminated by transducer ringing. The overall quality of the ADCP velocity data is poor. A.6. Other Incidents of Note A.7. Cruise Participants Name Responsibility on cruise Institution ----------------- ---------------------------------------- ------------------ Barstow, Dennis ADCP Oregon State Univ. Chipman, David CO2, underway systems LDGO Clark, Jordan helium, tritium, 18O, AMS 14C LDGO Grabitz, Dorothea helium, tritium, 18O, AMS 14C LDGO Hiller, Scott electronics tech, salts SIO/ODF Low, Clarence 13C NASA Ames Masten, Doug nutrients, deck SIO/ODF Mattson, Carl electronics tech, salts SIO/ODF Menzia, Fred CFCs NOAA/PMEL Muus, David deck, O2, data SIO/ODF Richman, James co-chief scientist physical oceanography Oregon State Univ. Rubin, Stephany CO2 LDGO Swift, James physical oceanography SIO Warner, Mark CFCs Univ. of Washington Williams, Robert deck, O2, data SIO/ODF Leader Group (plus Richman, U.S.) ----------------------- ------------------------------- ------------------ Koshlyakov, Mikhail Chief Scientist Shirshov Institute Sklyarov, Vladimir Ch. Deputy Shirshov Institute Zaytsev, Alexandr Ch. Deputy; CTD deck ops Shirshov Institute Sazhina, Tatyana Sc. Secretary Shirshov Institute Zhukova, Veronika secretary Shirshov Institute Sonde Group (CTD) ----------------------- ------------------------------- ------------------ Yemelyanov, Mikhail CTD console ops Shirshov Institute Maslennikov, Vyacheslay CTD console ops VNIRO Popkov, Valeriy CTD console ops VNIRO Frolov, Mikhail CTD deck ops Shirshov Institute Nesterenko, Yuriy watch stander Shirshov Institute Savelyev, Vitaliy CTD deck ops Shirshov Institute Yakovlev, Evgeniy watch stander Shirshov Institute Mathematical Group (data processing, GFD, models) ----------------------- ------------------------------- ------------------ Yaremchuck, Maxim data processing; interpolations Shirshov Institute Nechayev, Dmitriy GFD, modelling Shirshov Institute Benenson, Mikhail computer system manager Shirshov Institute Chesnokov, Andrey software technician Shirshov Institute Mardashkina, Natalya ocean modelling MFTI Hydrological Group (interpretative) ----------------------- ------------------------------- ------------------ Belkin, Igor interpretative p.o.; fronts Shirshov Institute Burkov, Valentin interpretative p.o. Shirshov Institute Chernyakova, Alla O2, nutrients, CO2 Shirshov Institute Stunzhas, Pavel O2, nutrients, CO2 Shirshov Institute Polyakova, Irina technician Shirshov Institute Meteorological Group ----------------------- ------------------------------- ------------------ Romanov, Yuriy Meteorology Shirshov Institute Lutsenko, Eduard synoptics AANII Radikevich, Vitaliy meteorology LGMI Rodionov, Vyacheslav remote sensing Shirshov Institute Safronov, Alexey actinometry IFA Romashova, Elena actinometry IFA Acoustic Group (ADCP & sound scattering) ----------------------- ------------------------------- ------------------ Berezutski, Alexander ADCP, MultiBeam bathymetry Shirshov Institute Timoshenko, Vladimir MultiBeam bathymetry TRTI Nosov, Alexandr MultiBeam bathymetry Shirshov Institute Shilov, Igor ADCP Shirshov Institute Korolev, Alexander ADCP Shirshov Institute Tikhonova, Natalya MultiBeam bathymetry Shirshov Institute Biological Group ----------------------- ------------------------------- ------------------ Voronina, Natalya zooplankton Shirshov Institute Levin, Lev fluorescence IBSO Sazhin, Andrey microplankton Shirshov Institute Sedelnikov, Sergey bio. hardware technician IBSO Zadorina, Larisa bio. Technician Shirshov Institute Definition of acromyms: VNIRO: Research Institute of Marine Fisheries and Oceanography, Moscow MFTI: Moscow Pysical-Technical Institute AANII: Arctic and Antarctic Institute, Saint Petersburg LGMI: Leningrad Hydro Meteorological Institute IFA: Institute of Atmospheric Physics of Russian Academy of Sciences, Moscow TRTI: Taganrog Radio Engineering Institute IBSO: Institute of biophysics of Siberian Branch of Russian Academy of Sciences, Krasnojarsk ________________________________________________________________________________________________________ ________________________________________________________________________________________________________ S04P ð ODF CTD Data Report ð 1992 ð R/V Akademik Ioffe IOFFE6 (WOCE S4-92) Calibrated Pressure-Series CTD Data Processing Summary and Comments December 28, 1993 R/V Akademik Ioffe 90KDIOFFE6/1 920214 - 920406 Montevideo, Uruguay to Wellington, New Zealand CHIEF SCIENTISTS Mikhail Koshlyakov Shirshov Institute of Oceanology of Russian Academy of Sciences Moscow, RUSSIA and James Richman Oregon State University Corvallis, OREGON DATA SUBMITTED BY: Scripps Institution of Oceanography Oceanographic Data Facility Marie-Claude Beaupre ODF CTD Group Oceanographic Data Facility Scripps Institution of Oceanography UC San Diego, Mail Code 0214 9500 Gilman Drive La Jolla, CA 92093-0214 phone: (619) 534-1906 fax: (619) 534-7383 e-mail: marie@odf.ucsd.edu 1. Introduction In this document we discuss CTDO data acquisition, calibration, corrections, and other processing for the IOFFE6 cruise on the R/V Akademik Ioffe. The final reported values were determined via careful examination and application of the pre- and post-cruise calibrations, and by comparison of CTD data with the water sample data collected during the CTD casts. Our techniques and calibration data are discussed below. 2. CTD Acquisition and Processing Summary 113 CTD casts plus 4 test casts were completed during IOFFE6. The rosette used was an ODF-designed 24-bottle system with a 24-place General Oceanics pylon nested inside a ring of twenty-four 10-liter bottles. A CTD, altimeter, pinger, and transmissometer were mounted on the bottom of the frame. ODF CTD #1 (a modified NBIS Mark III-B instrument) was used during the leg. The ODF CTD acquired data at a maximum rate of 25 Hz. The data consisted of pressure, temperature, conductivity, dissolved oxygen, second temperature, four CTD voltages, trip confirmation, transmissometer, altimeter and elapsed time. Power to the CTD was optimized by applying the minimum current to attain the CTD voltages required to maintain sensor stability. These voltages were monitored throughout the cast. An ODF-designed deck unit demodulated the FSK CTD signal to an RS-232 interface. The raw CTD data server allowed the data to be split into three different paths: to be logged in raw digitized form, to be monitored in real time as raw data, and to be processed and plotted. During the IOFFE6 expedition, an Integrated Solutions Inc. (ISI) Optimum V computer served as the real-time data acquisition processor. Additionally, Sun SPARC computers were used during post- cruise processing. The raw CTD audio signal was recorded on VHS videotape as an ultimate back-up, and all raw binary data were logged on a hard disk and then backed up to magnetic cartridge tape. In addition, all intermediate versions of processed data were backed up to magnetic cartridge tape. CTD data processing consists of a sequence of steps which is modified as needed. Data can be re-processed from any point in this sequence after the raw data are acquired from the sea cable and recorded on videotape and/or hard disk. Each CTD cast is assigned a correction file, and while the corrections are usually determined for groups of stations, it is possible to fine tune the parameters for even a single station. The acquisition and processing steps are as follows: ð Data are acquired from the CTD sea cable and assembled into consecutive .04-second frames containing all data channels. The data are converted to engineering units. ð The raw pressure, temperature and conductivity data are passed through broad absolute value and gradient filters to eliminate noisy data. The entire frame of raw data is omitted, as opposed to interpolating bad points, if any one of the filters is exceed- ed. The filters may be adjusted as needed for each cast. S04P ð ODF CTD Data Report ð 1992 ð R/V Akademik Ioffe TYPICAL IOFFE6 RAW DATA FILTERS Raw Data | | | Frame-to-Frame Channel | Minimum | Maximum | Gradient -------------+---------+---------+--------------- Pressure | -40 | 6400 | 2.0 dbar -------------+---------+---------+--------------- Temperature | -8 | 32.7 | .2 deg.C -------------+---------+---------+--------------- Conductivity | 0 | 64.355 | .3 mmho ð Pressure and conductivity are phase-adjusted to match the temperature response, since the temperature sensor responds more slowly to change. This lag time is determined using raw CTD data from the cruise. Conductivity data are corrected for ceramic compressibility in accordance with the NBIS Mark III-B Reference Manual. ð The data are averaged into 0.5-second blocks. During this step, data falling outside four standard deviations from the mean are rejected and the average is recalculated. Then data falling outside two standard deviations from the new mean are rejected, and the data are re-averaged. The resulting averages, excepting second temperature and CTD voltages, are reported as the 0.5-second time series. Secondary temperature data are used to verify the stability of the primary temperature channel calibration. Secondary temperature data are only filtered, averaged and reported with the time-series data when they are used in place of the primary temperature data due to a sensor malfunction. ð Corrections are applied to the data. The pressure data are corrected using laboratory calibration data. Temperature corrections, typically a quadratic correction as a function of temperature, are based on laboratory calibrations. Conductivity and oxygen corrections are derived from water sample data. Conductivity corrections are typically a linear fit of bottle minus CTD differences as a function of conductivity. Oxygen data are corrected on an individual cast basis. Uncorrected time-series transmissometer data are forwarded to TAMU for final processing and reporting. The averaged data are recorded on hard disk and sent to the real- time display system, where the averaged data can be reported and plotted during a cast. The averaging system also communicates with the CTD acquisition computer for detection of bottle trips, almost always occurring during the up casts. A 3- to 4-second average of the CTD data is stored for each detected bottle trip. A down-cast pressure-series data set is created from the time series by applying a ship-roll filter to the down-cast time-series data, then averaging the data within 2-dbar pressure intervals centered on the reported pressure. The first few seconds of data for each cast are generally excluded from the averages due to sensor adjustment or bubbles during the in-water transition. Pressure intervals with no time-series data can optionally be filled by double- parabolic interpolation. When the down-cast CTD data have excessive noise, gaps or offsets, the up-cast data are used instead. CTD data from down and up casts are not mixed together in the pressure-series data because they do not represent identical water columns (due to ship movement, wire angles, etc.). The CTD time series is always the primary CTD data record for the pressure, conductivity and temperature channels. The final correc- tions to the CTD oxygen data are made by correcting pressure-series CTD oxygen data to match the up-cast oxygen water samples at common isopycnals. The final CTDO pressure-series data are the data reported to the principal investigator and to the WHP Office. Subsequent sections of this document discuss the laboratory calibrations, data processing and corrections for the CTD used during IOFFE6. S04P ð ODF CTD Data Report ð 1992 ð R/V Akademik Ioffe 3. CTD Laboratory Calibrations 3.1. Pressure Transducer Calibration The CTD pressure transducer was calibrated in a temperature- controlled bath to the ODF Ruska deadweight-tester (DWT) pressure standards. The mechanical hysteresis loading and unloading curves were measured both pre- and post-cruise at cold temperature (-1.5 degrees C bath) to a maximum of 8830 psi, and at warmer temperature (15.2 and 6.1 degrees C baths pre-/post-cruise) to a maximum of 2030 psi. The post-cruise deep 8830 psi calibration was done a total of 3 times (in -1.5, -1.4, and -0.7 degrees C baths). CTD pre- and post-cruise pressure calibrations are summarized in Figure 1. 3.2. PRT Temperature Calibration All CTD PRT temperature transducers were calibrated in a temperature-controlled bath. CTD temperatures were compared with temperatures calculated from the resistance of a standard platinum resistance thermometer (SPRT) as measured by a NBIS ATB-1250 resistance bridge. The ultimate temperature standards at ODF are water and diphenyl ether triple-point cells and a gallium cell. Seven or more calibration temperatures, spaced across the range of -2.0 to 20.0 degrees C, were measured both pre- and post-cruise. CTD pre- and post-cruise temperature calibrations are summarized in Figures 2 and 3. It should be noted that ODF CTD PRT temperature transducers are offset approximately +1.5 degrees C in order to avoid a temperature response discontinuity that occurs at 0 degrees C; this offset is taken into account when correcting the data. 4. CTD Data Processing 4.1. Pressure, Temperature, Conductivity/Salinity, and Oxygen Corrections A maximum of 24 salinity and oxygen check samples were collected during each CTD cast. No thermometric pressure or temperature data were collected during this cruise. A 3- to 4-second average of the CTD time-series data was calculated for each sample. The resulting data were then used to derive CTD conductivity/salinity and oxygen corrections. The severe weather conditions encountered during this cruise dictated that shallow bottle stops (in the top 125 meters or so) be very short or omitted altogether, thus leading to smeared bottle-trip data for shallow bottles. Typically the winch does not move during a trip. 4.1.1. CTD Pressure Corrections 4.1.1.1. CTD #1 CTD #1 pre- and post-cruise pressure calibrations, Figures 1a and 1b were compared. The warm/shallow and cold/deep calibration curves both shifted by about 1 to 1.5 decibars from pre- to post-cruise. The slopes of the warm/shallow pressure calibration curves were nearly identical. The slopes of the cold/deep curves were slightly different: shallower points were nearly identical and the deepest points from the two calibrations were about 1.5 decibars apart. Thermometric pressures were not measured during the leg. The pre-cruise pressure calibration was left in place for the pressure data since the pre- and post-cruise pressure calibrations had slope differences well within the sensor accuracy. Any residual offset was compensated for automatically at each station: as the CTD enters the water, the corrected pressure is adjusted to 0 decibars. 4.1.2. CTD Temperature Corrections 4.1.2.1. CTD #1 CTD #1 had two temperature sensors: both PRT-1 and PRT-2 were calibrated pre- and post-cruise. PRT-1 was the main temperature sensor and was used exclusively in all data processing. PRT-2 was used to check for PRT-1 drift during the cruise. A comparison of the pre- and post-cruise laboratory CTD #1 PRT-1 temperature transducer calibrations, Figures 2a and 2b, showed two curves with nearly identical slopes and a -.0008 degrees C temperature shift in the range of -1 to 7 degrees C. For PRT-2, the secondary sensor, a comparison of the two calibrations, Figures 3a and 3b, also showed curves with nearly identical slopes and a +.0006 degrees C temperature shift in the range of -1 to 6 degrees C. The pre-cruise PRT-1 temperature calibration, Figure 2a, remained in effect for the CTD data since any differences between pre- and post-cruise temperature calibrations were negligible and well within the sensor accuracy. No thermometric temperatures were measured during this cruise. The PRT-1 minus PRT-2 differences were monitored during the cruise to check for possible temperature shifts. None were detected, and as expected, the pre- and post-cruise PRT-1 minus PRT-2 differences were consistent. S04P ð ODF CTD Data Report ð 1992 ð R/V Akademik Ioffe 4.1.3. CTD Conductivity Corrections In order to calibrate CTD conductivity, check-sample conductivities were calculated from the bottle salinities using CTD pressures and temperatures. For each cast, the differences between sample and CTD conductivities at all pressures were fit to CTD conductivity using a linear least-squares fit. Values greater than 2 standard deviations from the fits were rejected. The resulting conductivity correction slopes were plotted as a function of station number. The conductivity slopes were then fit as a function of station number to generate smoothed slopes. These smoothed slopes were an average of the slopes for the cruise (0-order). Since the range of conductivities in this part of the ocean is very narrow, the conductivity slope correction does not have a great effect on the data. Conductivity differences were then calculated for each cast after applying the preliminary conductivity slope corrections. Residual conductivity offsets were computed for each cast and fit to station number. Smoothed offsets were determined by groups, based on common conditions (i.e. such factors as pre- and post-conductivity-sensor cleaning). The resulting smoothed offsets were then applied to the data. Then conductivity slope as a function of conductivity was re- checked: no changes were warranted. Some offsets were manually adjusted to account for discontinuous shifts in the conductivity transducer response, or to insure a consistent deep T-S relationship from station to station. Station 711 was the only station showing any discontinuity with surrounding stations in the conductivity transducer response, and it was adjusted to match its own bottle salinities, which also matched the deep Theta-S data of surrounding stations. This cast exhibited strange results which were noted at sea during the cast. The top 340 decibars of this cast are offset, but it was impossible to use the upcast due to multiple offsets. Probably this entire cast is still suspect. We are surmising that the sensor became coated with protoplasmic slime early in the cast, some of which came off around 340 decibars, and which kept gradually washing off during the down and up casts. Plots of the final conductivity slopes and offsets can be found in Figures 4 and 5. Conductivity Correction Summary Stations | CTD# | Cond.Slopes | Cond.Offsets@ ---------+------+-------------+-------------- 682-686 | 1 | -1.5079e-3 | +4.0999e-2 ---------+------+-------------+-------------- 687-690 | 1 | -1.5079e-3 | +4.5252e-2 ---------+------+-------------+-------------- 691-710 | 1 | -1.5079e-3 | +4.3439e-2 ---------+------+-------------+-------------- 711-761 | 1 | -1.5079e-3 | +4.0357e-2 ---------+------+-------------+-------------- 762-769 | 1 | -1.5079e-3 | +3.8297e-2 ---------+------+-------------+-------------- 770-794 | 1 | -1.5079e-3 | +3.6655e-2 @individual stations were adjusted after this for conductivity sensor shifting or to insure a consistent deep T-S relationship from cast to cast. S04P ð ODF CTD Data Report ð 1992 ð R/V Akademik Ioffe 4.1.3.1. Bottle vs. CTD Conductivity Statistical Summary The IOFFE6 calibrated bottle-minus-CTD conductivity statistics include bottle salinity values with quality 3 or 4. There is approxi- mately a 1:1 correspondence between conductivity and salinity residual differences. The following statistical results were generated from the final bottle data set and the final corrected CTD data: IOFFE6 Final Bottle-CTD Conductivity Statistics | | mean conductivity | | cruise | pressure | difference | standard | #values | range(dbars) | (bottle-CTD mmho/cm) | deviation | in mean -------+-----------------+----------------------+-----------+-------- IOFFE6 | all pressures | -.00025@@ | .01758 | 2543 | allp (4,2rej) @ | -.00009 | .00162 | 2437 +-----------------+----------------------+-----------+-------- | press < 1500 | .00022 | .01446 | 1559 | p<1500(4,2rej)@ | -.00011 | .00219 | 1477 +-----------------+----------------------+-----------+-------- | press > 1500 | -.00100@@@ | .02161 | 984 | p>1500(4,2rej)@ | -.00008 | .00075 | 964 @ "4,2rej" means a 4,2 standard-deviation rejection filter was applied to the differences before generating the results. @@ A plot of these differences can be found in Figure 6a. @@@ A plot of these differences can be found in Figure 6b. 4.2. CTD Dissolved Oxygen Data 4.2.1. CTD Oxygen Corrections Dissolved oxygen data were acquired using Sensormedics dissolved oxygen sensors. The ocean area in which this cruise occurred provided harsh conditions for CTD oxygen sensors, especially the freezing temperatures. Due to the severe conditions, only the larger features in the CTD oxygen profiles should be considered realistic. Many profiles are very noisy and/or have extraneous oscillations. CTD oxygen data are corrected after pressure, temperature and conductivity corrections have been determined. CTD raw oxygen currents were extracted from the pressure-series data at isopycnals corresponding to the up-cast check samples. Most pressure-series data were from the down casts, where oxygen data are usually smoother than up-cast data because of the more constant lowering rate, avoiding the flow-dependence problems occurring at up-cast bottle stops. However, the IOFFE6 CTD oxygen data were affected with flow-dependence problems, down or up cast, each time a cast was stopped. There can also be flow-dependence problems if a cast is slowed down, as often happens during bottom approaches. The CTD oxygen correction coefficients were determined by applying a modified Levenberg-Marquardt nonlinear least squares fitting procedure to residual differences between CTD and bottle oxygen values. Bottle oxygen values were weighted as required to optimize the fitting of CTD oxygen to discrete bottle samples. Some bottle levels were omitted from a fit because of large pressure differences between down- and up-cast CTD data at isopycnals. Deep data points were often weighted more heavily than shallower data due to the higher density of shallow sampling on a typical 24-bottle sampling scheme. The IOFFE6 surface oxygen data fitting was adversely affected by the extreme cold conditions. Freezing sensors, combined with the typical going-in-water bubbles/noise, made it difficult to fit CTD oxygens to the bottle data in the surface mixed layer of many casts. The value of data above the second check sample should be very carefully considered. Sometimes, due to freezing of the oxygen sensor, the CTD oxygen data may be suspect for as much as the top 100 decibars. Any station where questionable data goes deeper than about 10 decibars is noted in the "CTD Shipboard and Processing Comments" in Appendix D. S04P ð ODF CTD Data Report ð 1992 ð R/V Akademik Ioffe 4.2.2. Bottle vs. CTD Oxygen Statistical Summary The CTD oxygens are generated by fitting up cast oxygen bottle data to down cast CTD raw oxygen (amps) measurements along isopycnals. Residual oxygen differences are not generated from these comparisons, so no comparison statistics are shown in this report. 4.3. Additional Processing A software filter was used on 35 casts to remove conductivity or temperature spiking problems in about .066% of the time-series data frames. Pressure did not require filtering. Oxygen spikes were filtered out of 6 casts. The filtered oxygen levels affected approximately .008% of the time-series data frames. 58.3% of the filtered oxygen data were shallower than 100 dbars and could possibly be directly related to bubbles trapped during the going-in-water transition or freezing of the sensor. The remaining density inversions in high-gradient regions cannot be accounted for by a mis-match of pressure, temperature and conductivity sensor response. Detailed examination of the raw data shows significant mixing occurring in these areas because of ship roll. The ship-roll filter resulted in a reduction in the amount and size of density inversions. After filtering, the down cast (or up cast - see table below) portion of each time-series was pressure-sequenced into 2-decibar pressure intervals. A ship-roll filter was applied to each cast during pressure sequencing to disallow pressure reversals. 5. General Comments/Problems There is one pressure-sequenced CTD data set, to near the ocean floor, for each of 113 casts at 112 station locations. There was a reoccupation of station 768 (as station 781). There was additionally a 3-cast shakedown station, a freon bottle check station, plus one cast aborted to avoid an iceberg; these were neither processed nor reported. Another CTD cast was done after the aborted cast at the same location. The data reported is from down casts, excepting the stations listed below: UP-CAST PRESSURE-SERIES DATA REPORTED Station(s) | Problem with Down Cast Data -----------+---------------------------- 687,769 | Salinity offset(s); up ok -----------+---------------------------- 702 | CTD signal lost at approxi- | mately 3655 db down (cast | 1); signal came back on way | up. Went back down (called | cast 2) to get a complete | upcast and trip bottles. | Only complete cast is cast | 2 (upcast). S04P ð ODF CTD Data Report ð 1992 ð R/V Akademik Ioffe The top level(s) (0 or 0-2 decibar(s) usually, but up to 16 decibars for a few stations with serious freezing problems) of some casts were extrapolated using a quadratic fit through the next three deeper levels. Recorded surface values were rejected only when it appeared that the drift was caused by sensors adjusting to the in- water transition or freezing/thawing; if there was any question that the that the surface values might be real, the original data were reported. Extrapolated surface levels are identified by a count of "1" in the "Number of Raw Frames in Average" reported with each data record in the files. The pressures for these extrapolated data frames, as well as other cast-by-cast shipboard or processing comments, are listed in the "CTD Shipboard and Processing Comments" in Appendix D. Harsh weather during this cruise combined with working off the stern of the ship led to numerous wire problems. These resulted in many stops, pauses, or yoyos during casts, the most severe of which are documented in Appendix D. In addition, missing data values, such as CTD oxygens in casts where the sensor failed or was not present on the rosette package, are represented as "-9" in the data files. There are 20 such casts in this data set: 687/02,688/01,689/01,690/01,692/01,719/01,720/01,721/01,723/01, 724/01,773/01,774/01,775/01,776/01,777/01,778/01,779/01,780/01, 781/01 and 782/01. There were 35 casts where the oxygen signal seemed to fail only during the top 80 or so decibars (probably due to extreme cold and/or sensor freezing); these are not reported as "-9", but the affected pressure levels are listed in Appendix D for the following stations: 684,686,696,699,702,703,704,705,708,709,710,711,712,713,714,717,718, 722,730,733,734,739,740,743,751,752,759,761,768,770,771,772,783,784 and 792 (all cast 1). The CTD oxygen sensor often requires several seconds in the water before being wet enough to respond properly; this is manifested as low or high CTD oxygen values at the start of some casts. Flow-dependence problems occur when the lowering rate varies, or when the CTD is stopped, as at the cast bottom or bottle trips, where depletion of oxygen at the sensor can cause lower oxygen readings. Appendix C: IOFFE6 Calibration Figures TABLE OF CONTENTS Figure 1a: CTD #1 Pre-cruise Pressure Calibration Figure 1b: CTD #1 Post-cruise Pressure Calibration Figure 2a: CTD #1 Pre-cruise PRT-1 Temperature Calibration Figure 2b: CTD #1 Post-cruise PRT-1 Temperature Calibration Figure 3a: CTD #1 Pre-cruise PRT-2 Temperature Calibration Figure 3b: CTD #1 Post-cruise PRT-2 Temperature Calibration Figure 4: IOFFE6 Conductivity Slopes Figure 5: IOFFE6 Conductivity Offsets Figure 6a: IOFFE6 Residual Conductivity Bottle-CTD Differences - All Pressures Figure 6b: IOFFE6 Residual Conductivity Bottle-CTD Differences - Prs>1500dbar NOTE: some differences fall outside of the plotted limits. Please refer to the bottle data quality codes. S04P ð ODF CTD Data Report ð 1992 ð R/V Akademik Ioffe Appendix D: IOFFE6 Processing Notes (WOCE-S4) TABLE OF CONTENTS 1. CTD Shipboard and Processing Comments 2. Cast Stops Longer Than 1 Minute 3. CTD Temperature and Conductivity Corrections Summary 4. Summary of IOFFE6 CTD Oxygen Time Constants 5. Levenberg-Marquardt Non-linear Least-Squares-Fit Oxygen Coefficients IOFFE6 / WOCE-S4 CTD Shipboard and Processing Comments sta/cast Comments -------- ------------------------------------------------------------ 681/01 shakedown cast, no samples - not part of final data distribution 681/02 shakedown cast, no samples - not part of final data distribution 681/03 shakedown cast, freon & SSW samples - not part of final data distribution; new end termination after cast due to PRT2 problem 682/01 683/01 684/01 delay before cast start (approx 30 min) due to ice "growlers" near ship; top 20 db CTD oxygen questionable 685/01 "steaming on wire on upcast" 686/01 new xmiss; problems with oxygen signal noted during cast; top 15 db CTD oxygen questionable 687/01 delay before cast start to avoid iceberg; cast ABORTED 687/02 UP cast (salinity offset on down cast); no CTD oxygen data (sensor not working properly) 688/01 no CTD oxygen data (sensor not working properly) 689/01 no CTD oxygen data (sensor not working properly); 0-db level extrapolated 690/01 no CTD oxygen data (sensor not working properly) 691/01 new CTD oxygen sensor 692/01 new CTD oxygen sensor; no CTD oxygen data (sensor not working properly) 693/01 new CTD oxygen sensor 694/01 after cast: cut off 50 m CTD cable due to kink & unlays - new end termination and added more weight to rosette 694/03 shallow IOAN biology cast - not part of final data distribution 695/01 696/01 xmiss not working properly?; top 18 db CTD oxygen questionable 697/01 0-db level extrapolated 698/01 need to clean xmiss windows: uptrace very different from down 699/01 top 40 db CTD oxygen questionable 700/01 701/01 swell causing slack wire on deployment; by 3600 m down, wind up to 40 knots & decided to head back up to surface; wire very slack at 10 m stop: kinks in wire - after cast, cut wire & reterminated; approx 3-min pause at 72 db down: data affected in all channels S04P ð ODF CTD Data Report ð 1992 ð R/V Akademik Ioffe sta/cast Comments -------- ------------------------------------------------------------ 702/01 hove to and waited 6 1/2 hrs to start due to wind (35 knots) & swell; added 150 lbs more lead pre-cast; lost CTD signal at 3655 db down but kept going deeper, so incomplete cast - not part of final data distribution 702/02 UP cast: continuation of 702/01 after CTD signal recovered & cast already on its way back up (3240 mwo) - after CTD signal recovery, cast taken back down to bottom before bringing up to have a complete up cast for this station; slack wire at 60 m stop: kink; top 70 db CTD oxygen questionable 703/01 kink in same place as station 702: new end termination after cast; top 120 db CTD oxygen questionable 704/01 strong winds but seas not bad; 20 deg wire angle: no slack wire, no kinks; top 100 db CTD oxygen questionable 705/01 rosette hit A-frame twice on recovery, breaking some bottles; top 100 db CTD oxygen questionable 706/01 little slack but not bad - towing at approx 20 deg angle; kink in wire at same place as before: new end termination after cast 707/01 PRT2 repairs made pre-cast: PRT2 board fixed inside CTD; 0-db level extrapolated 708/01 top 12 db CTD oxygen questionable 709/01 lost CTD signal at 4339 db up: problem in CTD/xmiss bulkhead connector; top 80 db CTD oxygen questionable; 0-db level extrapolated 710/01 no xmiss; top 100 db CTD oxygen questionable 711/01 no xmiss; entire station's data questionable due to salinity/ conductivity shift at 343 db - upcast not usable due to multiple offsets; as noted at sea, this station's CTD data was totally different from surrounding stations and needed a large conductivity offset adjustment to match surrounding stations' deep T/S; top 110 db CTD oxygen questionable 712/01 no xmiss; top 100 db CTD oxygen questionable; 0-db level extrapolated 713/01 no xmiss; top 100 db CTD oxygen questionable; 0-db level extrapolated 714/01 no xmiss; top 70 db CTD oxygen questionable; 0-db level extrapolated 715/01 0-db level extrapolated 716/01 717/01 xmiss ??; top 70 db CTD oxygen questionable (noted at sea that oxygen sensor probably frozen through mixed layer); 0-db level extrapolated 718/01 no xmiss; top 40 db CTD oxygen questionable; 0-db level extrapolated 719/01 no xmiss; no CTD oxygen data (sensor not working properly) S04P ð ODF CTD Data Report ð 1992 ð R/V Akademik Ioffe sta/cast Comments -------- ------------------------------------------------------------ 720/01 no xmiss; no CTD oxygen data (sensor not working properly); 0-db level extrapolated 721/01 no xmiss; no CTD oxygen data (sensor not working properly) 722/01 no xmiss; top 80 db CTD oxygen questionable 723/01 no xmiss; new CTD oxygen sensor; no CTD oxygen data (sensor not working properly); during post-cast rosette recovery too much wire paid out too quickly, resulting in kink: new end termination 724/01 no xmiss; no CTD oxygen data (sensor not working properly); 0-db level extrapolated 725/01 0-db level extrapolated 726/01 0-db level extrapolated 727/01 0,2-db levels extrapolated; -.001 salinity offset area 4174-4222 db 728/01 729/01 after cast in, noticed outer lay of armor looks loose 730/01 top 100 db CTD oxygen questionable; 0-db level extrapolated 731/01 0,2-db levels extrapolated 732/01 0-db level extrapolated 733/01 new end termination after cast; top 70 db CTD oxygen questionable 734/01 recovery ok, but some oil on water surface as rosette came out; top 40 db CTD oxygen questionable; 0-db level extrapolated 735/01 736/01 recovery ok, but outer lay of armor unlaying again - either spin or slack???; some big swells on this station 737/01 738/01 towing, seas up; loose strands to about 60 mwo; 0-db level extrapolated 739/01 voltage problem - "meg" cable: ok; xmiss not working well; after cast, new end termination with guy grip; top 80 db CTD oxygen questionable; 0-db level extrapolated 740/01 ok - wire shows signs of unlaying - block still seems a little skewed with shackles - needs swivel?; top 80 db CTD oxygen questionable; 0-db level extrapolated 741/01 xmiss off-scale & may not be working; 0-db level extrapolated 742/01 surge during recovery: wire kinked - new end termination after cast; 0-db level extrapolated 743/01 towing; wind 35 knots; xmiss off-scale and may not be working properly; top 70 db CTD oxygen questionable; 0-db level extrapolated S04P ð ODF CTD Data Report ð 1992 ð R/V Akademik Ioffe sta/cast Comments -------- ------------------------------------------------------------ 744/01 xmiss off-scale & may not be working properly; supposed to be towing cast but slight forward angle as rosette entered water & some slack wire - wire dropped to deck before bridge got ship moving 3-4 min later; recovery ok but large kink/very loose strand approx 10 m from rosette - new end termination; 0-db level extrapolated 745/01 towing at 2 knots - good-size swell but launch ok; after recovery found 2 kinks - big swell; xmiss not working; 0-db level extrapolated 746/01 waiting on weather - high seas & 39-43 knot winds; trawl wire block rigged in place of CTD block; wind to 29-31 knots & big swell but smoother at cast start - some problem with slack wire - towing at 2 knots; when cast up weather better, but 2 kinks; xmiss not working; 0-db level extrapolated 747/01 no xmiss; pre-cast added weight & found another kink in CTD cable near winch 748/01 no xmiss 749/01 no xmiss 750/01 no xmiss; pinger batteries died during cast (2500 m down); 0-db level extrapolated 751/01 no xmiss; new pinger batteries; top 40 db CTD oxygen questionable 752/01 no xmiss; top 20 db CTD oxygen questionable; 0-db level extrapolated 753/01 no xmiss; 0-db level extrapolated 754/01 no xmiss; bottom depth changing by 400 m at beginning of station from 3300 to 3700 m; 0-db level extrapolated 755/01 xmiss on rosette; towing speed a little slow: block bounced a few times until angle increased, but when cast in, wire ok; 0-db level extrapolated 756/01 757/01 758/01 0-db level extrapolated 759/01 top 80 db CTD oxygen questionable; 0-db level extrapolated 760/01 761/01 top 80 db CTD oxygen questionable; multiple salinity offsets in bottom 150 db caused by temperature and conductivity offsets: .001 to .003 salinity offset from 4132-4154 db, approximately .004 from 4172-4196 db, and .001 to .002 from 4210-4250 db 762/01 0-db level extrapolated 763/01 on recovery, rosette hit A-frame 3 ft off deck, damaging some bottles 764/01 765/01 good tow S04P ð ODF CTD Data Report ð 1992 ð R/V Akademik Ioffe sta/cast Comments -------- ------------------------------------------------------------ 766/01 after in found 1 bad kink - reterminated 767/01 big swell - towing at 2 knots; after in found 4 kinks, probably from slack during launch - new end termination after cast; temperature, conductivity, salinity and oxygen look strange in area between 530 and 800 db, but sigma theta stays smooth - down/up casts very different in this area; 0-db level extrapolated 768/01 towed at 2+ knots - several slack wire surges 50-150 mwo; pinger not working; top 40 db CTD oxygen questionable; 0-db level extrapolated 769/01 UP cast (salinity offset on down cast); wind approx 23 knots & seas about same as station 768 - slack wire to deck about 25 mwo - wire looks ok: no kinks/ strands a little loose; 0-db level extrapolated 770/01 weather better: no slack wire; conductivity sensor cleaned before this station; top 60 db CTD oxygen questionable (noted at sea that oxygen sensor probably frozen as air temp -4.6 deg); 0-db level extrapolated 771/01 good weather; top 60 db CTD oxygen questionable (noted at sea that oxygen sensor probably frozen); 0-6-db levels extrapolated 772/01 top 50 db CTD oxygen questionable; 0-10-db levels extrapolated 773/01 freezing weather on deck; no CTD oxygen data (CTD oxygen sensor failed at 10 m); 0-12-db levels extrapolated 774/01 freezing weather on deck; no CTD oxygen data (no CTD oxygen sensor); 0-8-db levels extrapolated 775/01 freezing weather; no CTD oxygen data (no CTD oxygen sensor); 0,2-db levels extrapolated 776/01 freezing weather; stopped at 10 m to allow sensors to equilibrate; no CTD oxygen data (no CTD oxygen sensor); 0-12-db levels extrapolated 777/01 loose fresh sea ice (pancake ice) - rosette entered in clear water of prop wash/recovery in clear water; no CTD oxygen data (no CTD oxygen sensor); 0-16-db levels extrapolated 778/01 CTD cold-soaked or had ice on sensors - waited 4 min at 10 m to warm up/ thaw sensors; no CTD oxygen data (no CTD oxygen sensor); 0-8-db levels extrapolated 779/01 warmed CTD at 10 m for 3 min - top 10 m of down cast no good - sensors frozen; no CTD oxygen data (no CTD oxygen sensor); 0-8-db levels extrapolated 780/01 held at 10 m down to warm up CTD; no CTD oxygen data (no CTD oxygen sensor); 0-8-db levels extrapolated 781/01 no CTD oxygen data (no CTD oxygen sensor); 0-db level extrapolated S04P ð ODF CTD Data Report ð 1992 ð R/V Akademik Ioffe sta/cast Comments -------- ------------------------------------------------------------ 782/01 no CTD oxygen data (no CTD oxygen sensor); 0-db level extrapolated 783/01 CTD oxygen sensor back on; top 80 db CTD oxygen questionable; 0-db level extrapolated 784/01 top 50 db CTD oxygen questionable; 0-db level extrapolated 785/01 0,2-db levels extrapolated 786/01 0-db level extrapolated 787/01 sampled during blizzard; 0-db level extrapolated 788/01 big swell - tow at 2.5 knots - no slack during launch; slack wire on recovery approx 50 mwo even though no stop - wind 25 knots - rough seas - several bad kinks: new end termination; large wire angle 789/01 wind 21 knots - seas still rough - waiting for seas to die down; launch ok; on recovery, kink in level wind when paying out wire during recovery; 0-db level extrapolated 790/01 0-db level extrapolated 791/01 towing at 2 knots - ok; 0-db level extrapolated 792/01 towing at 1.5 knots, then increasing to 2 knots; top 80 db CTD oxygen questionable; 0-db level extrapolated 793/01 794/01 final S4 station; 0-db level extrapolated 795/01 freon cast - not part of final data distribution; after recovery found 1 bad kink S04P ð ODF CTD Data Report ð 1992 ð R/V Akademik Ioffe IOFFE6: CAST STOPS LONGER THAN 1-MINUTE station down #minutes avg.pressure pressure /cast /up stopped (decibars) range ------------------------------------------------------ 682/01 DOWN 3.3 12 (10 - 14) 5.5 34 (32 - 36) 7.1 74 (72 - 76) 683/01 DOWN 3.4 12 (10 - 14) 1.9 74 (72 - 76) 684/01 DOWN 3.6 11 (8 - 14) 2.1 72 (70 - 74) 685/01 DOWN 2.1 12 (10 - 14) 3.3 73 (70 - 76) 686/01 DOWN 1.5 12 (10 - 14) 2.9 74 (72 - 76) 687/02 UP 2.6 11 (8 - 14) 1.0 32 (30 - 34) 688/01 DOWN 4.0 9 (2 - 16) 689/01 DOWN 1.6 12 (10 - 14) 2.0 72 (70 - 74) 690/01 DOWN 2.6 11 (8 - 14) 2.1 71 (68 - 74) 691/01 DOWN 1.5 10 (8 - 12) 4.7 74 (72 - 76) 1.2 3998 (3996 - 4000) 692/01 DOWN 3.3 7 (2 - 12) 693/01 DOWN 1.3 11 (8 - 14) 694/01 DOWN 3.2 7 (2 - 12) 2.6 70 (68 - 72) 697/01 DOWN 1.7 72 (70 - 74) 698/01 DOWN 3.9 103 (100 - 106) 1.7 203 (202 - 204) 1.3 4221 (4218 - 4224) 701/01 DOWN 3.2 72 (70 - 74) 702/02 UP 1.6 70 (68 - 72) 703/01 DOWN 1.2 149 (148 - 150) 704/01 DOWN 3.1 196 (194 - 198) 2.4 495 (490 - 500) 711/01 DOWN 4.4 4251 (4248 - 4254) 712/01 DOWN 1.4 4145 (4144 - 4146) 768/01 DOWN 1.5 1257 (1252 - 1262) 1.5 1297 (1294 - 1300) 787/01 DOWN 1.0 2350 (2348 - 2352) 1.2 2784 (2782 - 2786) S04P ð ODF CTD Data Report ð 1992 ð R/V Akademik Ioffe IOFFE6: CTD Temperature and Conductivity Corrections Summary PRT Temperature Coefficients Conductivity Coefficients Sta/ Response corT = t2*T2 + t1*T + t0 corC = c1*C + c0 Cast Time (secs) t2 t1 t0 c1 c0 ------------------------------------------------------------------------ 682/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0410 683/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0410 684/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0410 685/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0410 686/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0410 687/02 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0453 688/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0463 689/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0468 690/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0453 691/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0434 692/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0434 693/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0434 694/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0434 695/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0434 696/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0434 697/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0434 698/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0434 699/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0434 700/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0434 701/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0434 702/02 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0449 703/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0434 704/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0434 705/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0434 706/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0434 707/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0434 708/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0434 709/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0434 710/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0434 711/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0754 712/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0404 713/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0404 714/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0404 715/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0404 716/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0404 717/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0404 718/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0404 719/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0404 720/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0404 721/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0404 722/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0404 723/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0404 724/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0404 725/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0404 726/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0404 727/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0404 728/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0404 729/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0404 730/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0404 731/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0404 732/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0404 733/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0404 734/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0404 735/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0404 736/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0404 737/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0404 738/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0404 739/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0404 740/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0404 741/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0404 742/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0404 743/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0404 744/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0404 745/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0404 746/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0394 747/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0404 748/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0404 749/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0404 750/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0404 751/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0404 752/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0419 753/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0404 754/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0404 755/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0414 756/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0404 757/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0404 758/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0404 759/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0404 760/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0404 761/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0404 762/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0383 763/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0383 764/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0383 765/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0383 766/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0383 767/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0383 768/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0383 769/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0398 770/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0367 771/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0367 772/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0367 773/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0367 774/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0367 775/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0367 776/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0367 777/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0367 778/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0367 779/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0367 780/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0367 781/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0367 782/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0367 783/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0367 784/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0367 785/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0367 786/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0367 787/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0357 788/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0357 789/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0367 790/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0367 791/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0367 792/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0367 793/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0367 794/01 .325 2.18853e-05 -8.35260e-04 -1.4839 -1.50792e-03 0.0367 S04P ð ODF CTD Data Report ð 1992 ð R/V Akademik Ioffe Summary of IOFFE6 CTD Oxygen Time Constants Temperature | Press. | O2 Grad. --------------------------------------------- Fast(tauTF) | Slow(tauTS) | (tauP) | (tauOG) ------------+-------------+--------+--------- 32.0 | 363.0 | 19.4 | 60.0 IOFFE6 CTD Oxygen: Levenberg-Marquardt Non-linear Least-Squares-Fit Coefficients Sta/ Slope Offset Pcoeff TFcoeff TScoeff OGcoeff Cast (c1) (c2) (c3) (c4/fast) (c5/slow) (c6) ----------------------------------------------------------------------------------------- 682/01 4.41656e-04 2.81506e-01 2.59066e-04 -1.18066e-01 8.75760e-02 -5.92099e-05 683/01 1.12553e-03 -3.49833e-01 -8.22970e-05 3.68271e-02 -3.19311e-03 -5.34368e-03 684/01 6.16649e-04 1.61790e-01 -4.60659e-04 -5.03203e-02 2.24278e-02 1.04247e-02 685/01 7.08322e-04 -7.98769e-02 -5.66257e-05 -3.27601e-02 9.56105e-02 -2.11736e-03 686/01 6.81419e-04 -1.51064e-01 1.80425e-04 -2.71929e-02 -1.50646e-02 1.83377e-05 691/01 1.06698e-03 -2.53905e-02 1.63225e-04 -1.37322e-02 -7.67522e-03 -4.78056e-04 693/01 1.24055e-03 -8.53240e-02 1.75683e-04 1.35587e-02 -6.06646e-02 3.96825e-03 694/01 1.13914e-03 -4.54231e-02 1.67281e-04 1.90263e-02 -3.38050e-02 -2.89906e-03 695/01 1.25086e-03 -1.49895e-01 2.24898e-04 4.22672e-02 -2.73415e-02 -1.12904e-02 696/01 1.15387e-03 2.69581e-02 1.19573e-04 -3.07104e-02 -4.85211e-02 2.10160e-02 697/01 1.25846e-03 -8.04296e-02 1.69573e-04 1.06062e-02 -5.16751e-02 7.56906e-03 698/01 9.97905e-04 2.12734e-02 1.50025e-04 -1.26084e-02 2.83711e-03 -5.24004e-04 699/01 1.13006e-03 -4.24718e-02 1.68862e-04 -5.55727e-04 -1.61875e-02 4.39058e-03 700/01 1.09283e-03 -2.81896e-03 1.51030e-04 9.62159e-03 -3.68770e-02 2.03188e-03 701/01 1.20881e-03 -1.13564e-01 2.04570e-04 1.35117e-02 -7.07136e-03 7.47335e-04 702/02 1.13335e-03 -4.48679e-02 1.66911e-04 -1.47351e-02 2.48849e-02 -4.93871e-03 703/01 4.95642e-04 3.41654e-01 5.72309e-05 -1.30936e-01 8.31153e-02 -1.47493e-02 704/01 1.08428e-03 -4.90157e-02 1.81499e-04 -2.35185e-03 9.69122e-03 -3.51149e-03 705/01 9.51020e-04 1.23543e-01 9.83544e-05 -8.45067e-02 2.29196e-02 1.99789e-02 706/01 1.12179e-03 -7.51298e-02 1.95906e-04 -5.71601e-04 1.78119e-02 -3.25526e-03 707/01 1.13968e-03 -3.36107e-02 1.61342e-04 -1.24755e-02 -1.05295e-02 4.88687e-03 708/01 1.09264e-03 2.40151e-02 1.32699e-04 -3.40506e-02 -1.43238e-02 1.33208e-02 709/01 1.17928e-03 -8.47251e-02 1.89398e-04 2.05195e-02 -2.48384e-02 1.17111e-02 710/01 9.80998e-04 1.20630e-01 1.00686e-04 -5.23040e-02 -1.81247e-02 2.19228e-02 711/01 9.96184e-04 1.34570e-01 9.13930e-05 -6.80733e-02 -1.92439e-02 2.94639e-02 712/01 1.15907e-03 -5.53703e-03 1.43922e-04 -2.32606e-02 -1.47306e-02 -1.78617e-04 713/01 1.21997e-03 -6.29919e-02 1.73581e-04 -1.66829e-02 -5.79670e-03 -3.99356e-03 714/01 1.31936e-03 -1.47018e-01 2.10924e-04 -2.05979e-02 3.30750e-02 1.19064e-03 715/01 1.33844e-03 -1.31428e-01 1.91589e-04 3.60549e-02 -3.88092e-02 -4.04108e-04 716/01 1.29558e-03 -1.21359e-01 1.95892e-04 2.69460e-02 -3.68500e-02 5.28753e-03 717/01 6.17421e-04 3.18335e-01 5.54860e-05 -7.22565e-02 -1.39745e-03 -5.12861e-03 718/01 1.25441e-03 -1.27688e-01 2.11262e-04 3.90072e-02 -2.30022e-02 -2.28054e-02 722/01 1.02297e-03 4.00209e-02 1.37768e-04 -2.67640e-02 8.86520e-03 -3.32302e-03 725/01 1.01728e-03 1.24892e-02 1.51013e-04 -4.12244e-02 -1.07148e-02 1.59435e-02 726/01 9.22823e-04 8.80208e-02 1.25605e-04 -1.34292e-02 -2.12598e-02 4.10653e-03 727/01 9.43562e-04 9.17664e-02 1.18396e-04 -3.85186e-02 -1.00319e-02 6.38133e-03 728/01 1.02918e-03 1.84145e-02 1.48880e-04 -1.35024e-02 -1.25400e-02 4.99005e-03 729/01 1.04585e-03 4.14905e-02 1.32547e-04 -2.11893e-02 -2.34922e-02 7.62123e-03 730/01 9.30988e-04 9.30923e-02 1.20562e-04 -3.05369e-02 6.00394e-03 -8.30193e-03 731/01 9.87435e-04 5.70260e-02 1.32424e-04 -2.90472e-02 -2.43773e-03 3.13893e-03 732/01 9.66307e-04 8.32789e-02 1.23135e-04 -2.28400e-02 -1.56844e-02 3.33191e-03 733/01 1.00736e-03 5.15322e-02 1.34336e-04 -2.11251e-02 -8.56873e-03 1.91424e-03 734/01 1.06679e-03 9.28361e-04 1.55277e-04 -1.09244e-02 -2.94109e-03 3.02109e-03 735/01 1.07422e-03 1.63055e-02 1.43831e-04 -1.60743e-02 -1.17162e-02 5.20765e-03 736/01 1.06161e-03 3.51262e-02 1.36107e-04 -1.49699e-02 -2.47393e-02 4.63908e-03 737/01 9.43655e-04 9.54865e-02 1.22031e-04 -2.35100e-02 -1.29253e-02 1.03330e-03 738/01 1.01605e-03 4.69968e-02 1.36045e-04 -2.45487e-02 -4.42285e-03 6.98044e-03 739/01 1.04500e-03 4.12862e-02 1.34994e-04 -2.21867e-02 -2.67270e-02 6.59985e-03 740/01 1.00722e-03 4.68610e-02 1.37644e-04 -2.82343e-02 -1.27683e-02 9.70662e-03 741/01 1.07689e-03 6.21134e-03 1.51098e-04 -2.14836e-02 -2.29251e-03 1.66719e-03 742/01 1.11749e-03 -1.99199e-02 1.59652e-04 -2.32734e-02 -2.91259e-03 5.71045e-03 743/01 1.08062e-03 2.41658e-03 1.54384e-04 -5.48815e-04 -1.51616e-02 2.73304e-03 744/01 7.92861e-04 2.03175e-01 8.83111e-05 -7.48440e-02 -6.32590e-03 1.05644e-02 745/01 9.78509e-04 1.29462e-01 9.39197e-05 -8.56711e-02 -2.68440e-02 1.76821e-02 746/01 1.06157e-03 3.33899e-02 1.34159e-04 -4.94038e-02 -3.17785e-02 1.07234e-02 747/01 1.03218e-03 4.64828e-02 1.33465e-04 -3.57133e-02 -2.10449e-02 1.25009e-02 748/01 1.00945e-03 5.05572e-02 1.36613e-04 -2.77915e-02 -1.18835e-03 3.90772e-03 749/01 1.08489e-03 -3.15783e-03 1.59603e-04 -7.30272e-03 -5.27910e-03 8.99389e-04 750/01 9.81795e-04 7.61463e-02 1.27556e-04 -2.54811e-02 -9.14099e-03 5.19314e-03 751/01 1.03046e-03 6.21426e-02 1.26067e-04 -2.63776e-02 -3.74864e-02 1.60283e-02 752/01 1.06352e-03 3.38857e-03 1.60193e-04 -6.69881e-03 1.27223e-03 2.82855e-03 753/01 1.19316e-03 -7.14764e-02 1.83943e-04 2.02358e-02 -1.73475e-02 -1.51704e-03 754/01 1.06753e-03 -1.20240e-02 1.71504e-04 -1.47634e-02 1.15604e-02 5.94094e-04 755/01 1.04002e-03 3.34986e-02 1.43687e-04 -3.56100e-02 1.20365e-02 4.30685e-03 756/01 1.11417e-03 -2.90768e-02 1.72046e-04 -6.36752e-03 1.53638e-03 -3.22713e-03 757/01 1.03159e-03 5.17161e-02 1.32950e-04 -2.78426e-02 -1.22045e-02 4.45065e-03 758/01 1.06727e-03 3.26866e-02 1.40032e-04 -2.00083e-02 -2.21015e-02 4.19773e-03 759/01 1.07458e-03 2.32103e-02 1.43934e-04 3.31199e-03 -3.82828e-02 4.30527e-03 760/01 1.03626e-03 4.95339e-02 1.33178e-04 -4.58149e-02 6.18640e-03 6.81963e-03 761/01 1.37846e-03 -1.86038e-01 2.27162e-04 4.58648e-02 -3.96518e-02 1.45495e-03 762/01 1.02235e-03 4.93738e-02 1.35020e-04 -2.86184e-02 -1.67663e-03 3.29039e-03 763/01 9.56944e-04 8.21471e-02 1.27766e-04 -3.08040e-02 -8.93907e-04 4.38508e-03 764/01 9.95644e-04 8.16647e-02 1.20702e-04 5.78796e-03 -4.89629e-02 1.14173e-02 765/01 8.81785e-04 1.59011e-01 9.60669e-05 -7.35669e-02 3.03010e-05 9.06128e-03 766/01 6.66657e-04 3.11005e-01 5.35788e-05 -9.58272e-02 -2.77111e-02 2.20680e-02 767/01 1.00595e-03 8.70842e-02 1.13879e-04 -6.61491e-02 -1.71870e-03 7.47700e-03 768/01 1.00595e-03 8.70842e-02 1.13879e-04 -6.61491e-02 -1.71870e-03 7.47700e-03 769/01 9.60211e-04 1.31875e-01 9.47621e-05 -7.78393e-02 1.85687e-02 5.80810e-03 770/01 2.85714e-04 5.69253e-01 -9.57164e-06 -1.79322e-01 -1.94009e-02 5.99516e-03 771/01 1.43330e-03 -1.49962e-01 1.79819e-04 -1.35956e-02 -4.59710e-02 1.68344e-03 772/01 4.99006e-04 3.08401e-01 8.56742e-05 -5.32395e-02 1.81703e-02 8.53352e-04 783/01 3.99416e-04 3.29057e-01 2.86458e-05 -1.43662e-01 1.22821e-02 1.81898e-02 784/01 8.27242e-04 6.18770e-02 3.80352e-05 -8.66567e-02 -7.50808e-02 2.46716e-02 785/01 5.82952e-04 2.64293e-01 1.51268e-05 -1.72123e-01 5.02482e-04 1.82899e-02 786/01 7.01986e-04 1.30892e-01 5.17891e-05 -1.56562e-01 2.89275e-02 2.24523e-02 787/01 1.13594e-03 -2.45698e-01 2.19656e-04 4.84864e-02 -1.08180e-02 -8.06271e-03 788/01 4.41362e-04 3.93432e-01 2.77288e-05 -1.32294e-01 -2.46089e-02 1.92975e-02 789/01 8.56845e-04 4.45344e-02 1.25687e-04 -5.25621e-02 -1.12070e-02 7.20958e-03 790/01 7.66731e-04 1.10904e-01 1.19183e-04 -9.05424e-03 -5.64651e-02 1.77683e-02 791/01 5.69547e-04 2.64954e-01 7.08795e-05 -9.53088e-02 -2.07165e-03 9.90014e-03 792/01 4.29547e-04 3.91761e-01 1.75663e-05 -9.66987e-02 -2.63754e-03 1.92703e-02 793/01 8.69680e-04 1.75433e-02 1.48746e-04 -4.27301e-02 5.44298e-03 -1.32688e-03 794/01 8.85232e-04 2.84766e-01 -6.96094e-04 -1.20620e-02 1.18321e-01 -1.52724e-03 ________________________________________________________________________________________________________ ________________________________________________________________________________________________________ S04P ð ODF BTL Data Report ð 1992 ð R/V Akademik Ioffe World Ocean Circulation Experiment (WOCE) S4P R/V Akademik Ioffe RUKDIOFFE6/1 920214 - 920406 Montevideo, Uruguay to Wellington, New Zealand CHIEF SCIENTIST Mikhail Koshlyakov Shirshov Institute of Oceanology of Russian Academy of Sciences Moscow and James Richman Oregon State University Corvallis, OR DATA SUBMITTED BY: Scripps Institution of Oceanography Oceanographic Data Facility Scripps Institution of Oceanography UC San Diego, Mail Code 0214 9500 Gilman Drive La Jolla, CA 92093-0214 phone: (619) 534-1903 fax: (619) 534-7383 e-mail: ksanborn@ucsd.edu DESCRIPTION OF MEASUREMENT TECHNIQUES AND CALIBRATIONS ODF CTD/rosette casts were carried out with a 24 bottle rosette sampler of ODF manufacture using General Oceanics pylons. An ODF-modified NBIS Mark 3 CTD, a Benthos altimeter and a SeaTech transmissometer provided by Texas A&M University (TAMU) were mounted on the rosette frame. Seawater samples were collected in 10-liter PVC Niskin and ODF bottles mounted on the rosette frame. A Benthos pinger with a self-contained battery pack was mounted separately on the rosette frame; its signal was displayed on the precision depth recorder (PDR) in the ship's laboratory. The rosette/CTD was suspended from a three-conductor wire which provided power to the CTD and relayed the CTD signal to the laboratory. Each CTD cast extended to within approximately 10 meters of the bottom unless the bottom returns from both the pinger and the altimeter were extremely poor. The bottles were numbered 1 through 24. When one of these 24 bottles needed servicing and repairs could not be accomplished by the next cast, the replacement bottle was given a new number. The replacement bottles were numbered 25 through 30. Subsets of CTD data taken at the time of water sample collection were transmitted to the bottle data files immediately after each cast to provide pressure and temperature at the sampling depth, and to facilitate the examination and quality control of the bottle data as the laboratory analyses were completed. The CTD data and documentation are submitted separately to the chief scientist. After each rosette cast was brought on board, water samples were drawn in the following order: Freon (CFC-11 and CFC-12), Helium-3, Oxygen, Total CO2, Alkalinity, AMS 14C, Tritium, Nutrients (silicate, phosphate, nitrate and nitrite), and Salinity. The samples and the ODF or Niskin sampler they were drawn from were recorded on the Sample Log sheet. Comments regarding integrity of the water sample (valve open, lanyard caught in lid, etc.) were also noted on the Sample Log sheets. The discrete hydrographic data were entered into the shipboard data system and processed as the analyses were completed. The bottle data were brought to a useable, though not final, state at sea. ODF data checking procedures included verification that the sample was assigned to the correct depth. This was accomplished by checking the raw data sheets, which included the raw data value and the water sample bottle, versus the sample log sheets. Any comments regarding the water samples were investigated. The raw data computer files were also checked for entry errors. Investigation of data included comparison of bottle salinity and oxygen with CTD data, and review of data plots of the station profile alone and compared to nearby stations. If a data value did not either agree satisfactorily with the CTD or with other nearby data, then analysis and sampling notes, plots, and nearby data were reviewed. If any problem was indicated, the data value was flagged. Appendix C, the Bottle Data Processing Notes, includes comments regarding missing samples and investigative remarks for comments made on the Sample Log sheets, as well as all flagged (WOCE coded) data values. S04P ð ODF BTL Data Report ð 1992 ð R/V Akademik Ioffe The WOCE codes were assigned to the water data using the criteria: code 4 = Does not fit station profile and/or adjoining station comparisons. There are analytical notes indicating a problem, but data values are reported. ODF recommends deletion of these data values. Analytical notes for salinity and/or oxygen may include large differences between the water sample and CTD profiles. Sampling errors are also coded 4. code 3 = Does not fit station profile or adjoining station comparisons. No notes from analyst indicating a problem. Datum could be real, but the decision as to whether it is acceptable will be made by a scientist rather than ODF's technicians. code 2 = Acceptable measurement. code 1 = Sample for this measurement was drawn from water bottle, but results of analysis not received. The quality flags assigned to the bottle as defined in the WOCE Operations manual are further clarified as follows: If the bottle tripped at a different level than planned, ODF assigned it a code 4. If the bottle tripped between the scheduled trip and the next trip, as indicated by the water sample data, ODF coded these bottles 3. If there is a 4 code on the bottle, and 2 codes on the salinity, oxygen and nutrients then the pressure assignment was probably correct. An air leak is identified by a 3 code on the bottle and 4 code on the oxygen. Air leaks only affect the gas samples. The following table shows the number of ODF samples drawn and the number of times each WOCE sample code was assigned. ------------------------------------------------------------------- Rosette Samples Stations 682-794 ------------------------------------------------------------------- Reported WHP Quality Codes levels 1 2 3 4 5 7 9 ----------++--------+---------------------------------------------- Bottle || 2612 | 0 2500 30 71 0 0 11 CTD Salt || 2590 | 0 2565 24 1 0 0 22 CTD Oxy || 2099 | 0 2040 59 0 24 0 489 Salinity || 2565 | 0 2493 35 37 0 0 47 Oxygen || 2553 | 0 2515 9 29 9 0 50 Silicate || 2561 | 0 2533 6 22 3 0 48 Nitrate || 2561 | 0 2484 56 21 3 0 48 Nitrite || 2561 | 0 2538 2 21 3 0 48 Phosphate || 2560 | 0 2532 7 21 4 0 48 Pressure and Temperature All pressures and temperatures for the bottle data tabulations on the rosette casts were obtained by averaging CTD data for a brief interval at the time the bottle was closed on the rosette. All reported CTD data are calibrated and processed with the methodology described in the documentation accompanying the CTD data submission. The temperatures are based on the International Temperature Scale of 1990. S04P ð ODF BTL Data Report ð 1992 ð R/V Akademik Ioffe Salinity The water sample salinities were measured with an ODF-modified Guildline Autosal Model 8400A salinometer (Serial Number 57-396) that was standardized for each cast with IAPSO Standard Seawater (SSW) Batch P-108. Salinity samples were drawn into 200 ml Kimax high alumina borosilicate bottles with custom-made plastic insert thimbles and Nalgene screw caps. This assembly provides very low container dissolution and sample evaporation. Salinity was determined after sample equilibration to laboratory temperature, usually within 8-36 hours of collection. Salinometers were located in a temperature-controlled laboratory. Only one salinometer was used for the salinity samples. This salinometer was connected to a computer to automate the data aquisition. Salinity bottles were rinsed three times before filling. Salinity has been calculated according to the equations of the Practical Salinity Scale of 1978 (UNESCO, 1981). This calculation uses the conductivity ratio determined from bottle samples analyzed (minimum of two recorded analyses per sample bottle after flushing). The Autosal salinometer was calibrated against a single batch of Wormley IAPSO standard seawater, P-108, with at least one fresh vial opened per cast. Accuracy estimates of bottle salinities run at sea are usually better than 0.002 psu relative to the specified batch of standard. Although laboratory precision of the Autosal can be as small as 0.0002 psu when running replicate samples under ideal conditions, at sea the expected precision is about 0.001 psu under normal conditions, with a stable lab temperature. Oxygen Samples were collected for dissolved oxygen analyses soon after the rosette sampler was brought on board and after CFC and helium were drawn. Nominal 125 ml volume iodine flasks were rinsed carefully 3 times using sample seawater with minimal agitation, then filled via a drawing tube, and allowed to overflow for at least 2 flask volumes. The draw temperature was measured and reagents were added to fix the oxygen before stoppering. The flasks were shaken twice; immediately after drawing, and then again after 20 minutes, to assure thorough dispersion of the Mn(OH)2 precipitate. The samples were analyzed within 4-36 hours of collection. Dissolved oxygen analyses, reported in micromoles per kilogram, were performed via titration in the volume-calibrated iodine flasks with an SIO automated oxygen titrator with a Dosimat 665 buret driver fitted with a 1.0 ml buret, using the whole-bottle Winkler titration following the technique of Carpenter (1965) with modifications by Culberson et al. (1991). Standardizations were performed with 0.01N potassium iodate solutions prepared from preweighed potassium iodate crystals. Standards were run at the beginning of each session of analyses, which typically included from 1 to 3 stations. Several standards were made up and compared to assure that the results were reproducible, and to preclude the possibility of a weighing error. A correction was made for the amount of oxygen introduced with the reagents. Combined reagent/distilled water blanks were determined to account for oxidizing or reducing materials in the reagents. The data processor and/or analyst plotted the oxygen standards and blanks and reviewed the data for possible problems with standards and/or blanks. Oxygens were converted from milliliters per liter to micromoles per kilogram using the in-situ temperature. Ideally, for whole-bottle titrations, the conversion temperature should be the temperature of the water issuing from the Niskin bottle spigot. The temperature of the samples was measured at the time the sample was drawn from the bottle, but were not used in the conversion from milliliters per liter to micromoles per kilogram because the software is not available. Aberrant temperatures provided an additional flag indicating that a bottle may not have tripped properly. Measured sample temperatures from mid-deep water samples were about 4-7 degree C warmer than in-situ temperature. Had the conversion with the measured sample temperature been made, converted oxygen values, would be about 0.08% higher for a 6 degree C warming (or about 0.2umol/kg for a 250umol/kg sample). S04P ð ODF BTL Data Report ð 1992 ð R/V Akademik Ioffe Nutrients The nutrient analyses were performed by an analyst from Scripps Institution of Oceanography, Shipboard Technical Support/Oceanographic Data Facility (STS/ODF). Nutrients (phosphate, silicate, nitrate and nitrite) analyses, reported in micromoles/kilogram, were performed on a modified AutoAnalyzer II. The procedures used are described in Gordon et al. (1992). Standardizations were performed with solutions prepared aboard ship from preweighed standards. These solutions were used as working standards before and after each cast (approximately 24 samples) to correct for instrumental drift during analyses. Sets of 4-6 different concentrations of shipboard standards were analyzed periodically to determine the linearity of colorimeter response and the resulting correction factors. Phosphate was analyzed using hydrazine reduction of phosphomolybdic acid as described by Bernhardt & Wilhelms (1967). Silicate was analyzed using stannous chloride reduction of silicomolybdic acid. Nitrite was analyzed using diazotization and coupling to form dye; nitrate was reduced by copperized cadmium and then analyzed as nitrite. These three analyses use the methods of Armstrong et al. (1967). Samples were drawn into 45 ml high density polypropylene, narrow mouth, screw-capped centrifuge tubes which were rinsed twice before filling. Some samples may have been refrigerated at 2 to 6 degree C for a maximum of 12 hours. Nutrients were converted from micromoles per liter to micromoles per kilogram by dividing by sample density calculated at a laboratory temperature measured at 25 degree C. DATA COMPARISONS AND COMMENTS The oxygen and nutrient data were compared by ODF with those from adjacent stations. Dr. James Swift did comparisons with historical data sets. Data checking procedures included verification of sample depth, accuracy of data entry, and data comparisons. Checking the raw data recordings, which included the raw data value and the water sample bottle, versus the sample log sheets verified sample trip depths. The raw data computer files were also checked against data sheets and logs for entry errors. Investigation of data included comparison of bottle salinity and oxygen with CTD data, and review of data plots of the station profile alone and compared to nearby stations. If a data value did not either agree satisfactorily with the CTD or with other nearby data (for example in a plot comparison), analysis and sampling notes, plots, and nearby data were reviewed. If any problem was indicated the data value was flagged. ODF preserved all bottle data values. Historically, most failures to return a validated water sample can be traced to the rosette pylon, with ship's wire and CTD cable end termination the next most frequent leading cause. However, on this expedition the pylons and wire worked nearly perfectly, and the leading causes of failure to return a reportable water sample were miscellaneous mechanical problems with the rosette bottles, i.e., a lanyard hanging up in a lid, open spigot and/or vent. S04P ð ODF BTL Data Report ð 1992 ð R/V Akademik Ioffe REFERENCES AND UNCITED SUPPORTING DOCUMENTATION Armstrong, F. A. J., C. R. Stearns, and J. D. H. Strickland, 1967. The measurement of upwelling and subsequent biological processes by means of the Technicon Autoanalyzer and associated equipment, Deep-Sea Research, 1144, 381-389. Atlas, E. L., S. W. Hager, L. I. Gordon and P. K. Park, 1971. A Practical Manual for Use of the Technicon(R) AutoAnalyzer(R) in Seawater Nutrient Analyses; Revised. Technical Report 215, Reference 71-22. Oregon State University, Department of Oceanography. 49 pp. Bernhardt, H. and A. Wilhelms, 1967. The continuous determination of low level iron, soluble phosphate and total phosphate with the AutoAnalyzer, Technicon Symposia, Volume I, 385-389. Brewer, P. G. and G. T. F. Wong, 1974. The determination and distribution of iodate in South Atlantic waters. Journal of Marine Research, 3322,1:25-36. Bryden, H. L., 1973. New Polynomials for Thermal Expansion, Adiabatic Temperature Gradient, Deep-Sea Research, 2200, 401-408. Carpenter, J. H., 1965. The Chesapeake Bay Institute technique for the Winkler dissolved oxygen method, Limnology and Oceanography, 1100, 141-143. Carter, D. J. T., 1980 (Third Edition). Echo-Sounding Correction Tables, Hydrographic Department, Ministry of Defence, Taunton Somerset. Chen, C.-T. and F. J. Millero, 1977. Speed of sound in seawater at high pressures. Journal Acoustical Society of America, 6622, No. 5, 1129-1135. Culberson, C. H., Williams, R. T., et al, August, 1991. A comparison of methods for the determination of dissolved oxygen in seawater, WHP Office Report WHPO 91-2. Fofonoff, N. P., 1977. Computation of Potential Temperature of Seawater for an Arbitrary Reference Pressure. Deep-Sea Research, 2244, 489-491. Fofonoff, N. P. and R. C. Millard, 1983. Algorithms for Computation of Fundamental Properties of Seawater. UNESCO Report No. 44, 15-24. Gordon, L. I., Jennings, Joe C. Jr, Ross, Andrew A., Krest, James M., 1992. A suggested Protocol for Continuous Flow Automated Analysis of Seawater Nutrients in the WOCE Hydrographic Program and the Joint Global Ocean Fluxes Study. OSU College of Oceanography Descr. Chem Oc. Grp. Tech Rpt 92-1. Hager, S. W., E. L. Atlas, L. D. Gordon, A. W. Mantyla, and P. K. Park, 1972. A comparison at sea of manual and autoanalyzer analyses of phosphate, nitrate, and silicate. Limnology and Oceanography, 1177, 931-937. Lewis, E. L., 1980. The Practical Salinity Scale 1978 and Its Antecedents. IEEE Journal of Oceanographic Engineering, OE-5, 3-8. Mantyla, A. W., 1982-1983. Private correspondence. Millero, F. J., C.-T. Chen, A. Bradshaw and K. Schleicher, 1980. A New High Pressure Equation of State for Seawater. Deep-Sea Research, 2277AA, 255-264. Saunders, P. M., 1981. Practical Conversion of Pressure to Depth. Journal of Physical Oceanography, 1111, 573-574. Sverdrup, H. U., M. W. Johnson, and R. H. Fleming, 1942. The Oceans, Their Physics, Chemistry and General Biology, Prentice-Hall, Inc., Englewood Cliff, N.J. UNESCO, 1981. Background papers and supporting data on the Practical Salinity Scale, 1978. UNESCO Technical Papers in Marine Science, No. 37, 144 p. S04P ð ODF BTL Data Report ð 1992 ð R/V Akademik Ioffe APPENDIX C Data comments: Hydrographic data Remarks for deleted samples, missing samples, and WOCE codes other than 2 from RUKDIOFFE6/1 WOCE S4P. Investigation of data may include comparison of bottle salinity and oxygen data with CTD data, review of data plots of the station profile and adjoining stations, and rereading of charts (i.e., nutrients). Comments from the Sample Logs and the results of ODF's investi- gations are included in this report. Units stated in these comments are milliliters per liter for oxygen and micromoles per liter for Silicate, Nitrate, and Phosphate, unless otherwise noted. The first number before the comment is the cast number (CASTNO) times 100 plus the bottle number (BTLNBR). STATION 684 111 CTDO Processor: "Top 20db CTD oxygen questionable." 106 Not enough water left for salt. Salt sample logged and run. Delta-S .022 low at 162db. Calc ok. High gradient. Footnote salinity questionable. 103 Sample log:"Bad air vent leak-not tight" Delta-S .002 low at 303db. Other water samples also ok. 102 Sample log:"Not enough left for salt" Salt sample logged and run. Delta-S .006 low at 363db. Good agreement with CTD S. Footnote salinity questionable. STATION 686 118 CTDO Processor: "Top 15db CTD oxygen questionable." 113 Sample log: "No water." Lanyard hangup. 101 Sample log: "Leak" type not specified. Delta-S .000 at 1524db. Other water samples also ok. STATION 687 Cast 2 CTDO Processor: "No CTD oxygen data (sensor not working properly)." 208 Sample log: "Small leak." Delta-S .002 low at 1060db. PO4 .07 low, chart rechecked, but other water samples ok. Good O2 & SIL gradients. JHS: "OA agrees PO4 at least 0.06 low." Nutrient processor: "Looks real, NO3 also little lower." Footnote bottle leaking. Footnote po4 questionable. 207 Delta-S .005 high at 1207db. Calc ok. No corresponding bump in CTD trace. Other water samples have normal gradient. JHS: "OA agrees S ca. 0.006 high." Footnote salinity questionable. 201 Delta-S .004 low at 2410db. Calc ok.Other water samples look ok. SIL max. Footnote salinity questionable. Cast 1 aborted due data acquisition problem after rosette brought out of water due tag line problem. STATION 688 Cast 1 CTDO Processor: "no CTD oxygen data (sensor not working properly)." 108 Sample log: "Dripping from spigot, can't be stopped." Delta-S .000 at 1511db. Other water samples also ok. 103 JHS: "OA says PO4 low by ca. 0.02." Nutrient Analyst: "Low on chart." Footnote phosphate questionable. STATION 689 Cast 1 CTDO Processor: "no CTD oxygen data (sensor not working properly)." 111 Delta-S at 1261db is -0.0074, salinity is 34.722. See 105 salinity comment. Assume related to 5 & 8 Autosal problem. Footnote salinity bad. 110 See 105 salinity comment. Delta-S .02 low at 1513db. Calc ok. Assume related to 5 & 8 Autosal problem. Footnote salinity bad. 109 See 105 salinity comment. Delta-S .03 low at 1765db. Calc ok. Assume related to 5 & 8 Autosal problem. Footnote salinity bad. 108 See 105 salinity comment. Delta-S .025 low at 2016db. Calc ok. Footnote salinity bad. 107 Delta-S at 2270db is -0.0055, salinity is 34.706. See 105 salinity comment. Assume related to 5 & 8 Autosal problem. Footnote salinity bad. 106 Delta-S at 2527db is -0.005, salinity is 34.703. See 105 salinity comment. Assume related to 5 & 8 Autosal problem. Footnote salinity bad. 105 Salinity data sheet: "Bottle 5 & 8 would not read correctly." Salinity data sheet: 5 1.98412 > 1.98438. Salinity data sheet: 8 1.98404 > 1.98441. Delta-S .012 low at 2781db. Calc ok. Footnote salinity bad. S04P ð ODF BTL Data Report ð 1992 ð R/V Akademik Ioffe STATION 690 Cast 1 CTDO Processor: "no CTD oxygen data (sensor not working properly)." 104 No hydro oxygen. Titration error. Footnote oxygen lost. 103 Sample log: "Air vent open." Delta-S .000 at 3452db. Other water samples also ok. Footnote salinity questionable. JHS: "OA suggests O2 0.02 low." Calc ok. Footnote oxygen questionable, footnote bottle leaking. 102 Delta-S .003 low @ 3758 db. Calc OK. Footnote salinity questionable. STATION 691 124 Sample log: "Air vent open." Delta-S .000 at 17db. Other samples look reasonable for near surface sample. 108-112 See 101-112 comments. Footnote salinity questionable. 107 Sample log: "No water. Lanyard caught up." Footnote bottle samples not drawn. 106 See 101-112 comments. Footnote salinity questionable. 105 Delta-S at 2940db is -0.0037, salinity is 34.699. See 101-112 comments. Footnote salinity questionable. 104 Delta-S at 3242db is -0.005, salinity is 34.697. See 101-112 comments. Footnote salinity questionable. 103 JHS: "OA suggests NO3 ca. 0.2 low." Nutrient Analyst: "Bad peak, make it .646 instead of .643." Footnote no3 questionable. DQE suggests NO3 flagged 2, ODF agrees. Delta-S at 3546db is -0.0056, salinity is 34.696. See 101-112 comments. Footnote salinity questionable. 101-112 JHS: "OA shows 1012 db to bottom to have lowest S per theta on entire cruise. O2 in deep water looks a bit high, and SiO3 below 2500 is some of highest of cruise. Acts like double trip at bottom, with skipped trip above. Virtually impossible, of course, but this is a strange station anyway you look at it." Nutrient Analyst: "Can't find any SIL problems." Footnote salinities questionable. 101 Delta-S at 4066db is -0.0039, salinity is 34.697. See 101-112 comments. Footnote salinity questionable. STATION 692 Cast 1 Salinity: "After this salinity run, technician replaced lamp and cell tubing." CTDO Processor: "no CTD oxygen data (sensor not working properly)." 117 Sample log: "No water in 17." "Lanyard hangup." Footnote bottle samples not drawn. 107 Delta-S .87 low. All samples indicate NB 7 closed near surface. Probable lanyard hangup. Footnote bottle leaking, footnote samples bad. ODF recommends deletion of water samples. 101 Delta-S .006 low at 3594db. Calc ok. Other water samples ok. CTD S trace straight at bottom. JHS: "OA suggests S low by at least 0.003." Footnote salinity questionable. STATION 693 101 Delta-S .004 high at 3371db. Calc ok. Other water samples ok. CTD S trace straight at bottom. JHS: "OA suggest S high by 0.006." Footnote salinity questionable. STATION 694 Cast 3 Biology station, no samples. 116 No nutrients. Sample tube empty. Sample log indicates sample should have been drawn. Footnote sil, no3, no2, and po4 lost. 108 Delta-S at 2068db is -0.0039, salinity is 34.708. No action, leave as is. STATION 695 Cast 1 JHS: "OA shows PO4 high while NO3 low over almost all of water column. OA suggests it may be NO3 that is "off"." Nutrient Analyst: "Can't find anything wrong." 122 Sample log: "Small leak." Not specified. Delta-S.385 high at 85db. Other water samples indicate NB22 closed around 175db. Footnote bottle leaking, footnote samples bad. ODF recommends deletion of all water samples. 121 Sample log: "Small leak." Not specified. Samples look ok for high gradient area at 125db. DQE: "124.8db bottle may leak, SALNTY is 0.017 less than upcast CTDSAL, which means water sample could be mixed with shallower waters, as well as for oxygen, OXYGEN is higher than downcast CTDOXY." Based on DQE comment and comment from Sample Log, footnote bottle leaking and samples bad even though DQE indicated only Salinity and oxygen since that was the only data DQE was looking at. S04P ð ODF BTL Data Report ð 1992 ð R/V Akademik Ioffe 105 JHS: "OA suggests S high by ca. 0.003." Delta-S .002 high at 2774db. Calc ok. Footnote salinity questionable. STATION 696 124 CTDO Processor: "Top 18db CTD oxygen questionable." 123 Sample log: "Salt btl has loose thimble" Delta-S .001 high at 54db. 120 Sample log: "Salt btl has loose thimble" Delta-S .012 high at 175db. High grad. 118 Sample log: "Salt btl has loose thimble" Delta-S .007 low at 255db. High gradient. 113 Sample log: "Salt btl has loose thimble" Delta-S .001 high at 759db. No hydro oxygen. "Parity error" on O2 computer before data saved. Footnote oxygen lost. 111 Sample log: "Salt btl has loose thimble" Delta-S .001 low at 1264db. 106 Sample log: "Salt btl has loose thimble" Delta-S .000 at 2627db. 104 Sample log: "Salt btl has loose thimble" Delta-S .000 at 3236db. 103 Sample log: "Air vent leak. Not tight." Delta-S .000 at 3545db. Other water samples also ok. STATION 698 Cast 1 Tripping problem. First trigger had no trip box confirm & 5 ISI confirms. Data indicate NBs 1&2 closed at bottom and no sample at 10db. Possibly ramp shaft turned back from 1 to 24 instead of cocking 24 with 3rd hand to hold ramp shaft. 107 JHS: "OA suggests PO4 high by 0.02-0.03." Nutrient Analyst: "Peak ok, higher." Footnote phosphate questionable. DQE suggests PO4 flagged 2, ODF agrees. 106 Sample log: "Bottom end cap leaked." Delta-S .001 high at 3248db. Other water samples also ok. 101 Sample log: "Air vent closed lightly. bottom end cap leaked." Delta-S .001 high at 4296db. Other water samples also ok. STATION 699 124 CTDO Processor: "Top 40db CTD oxygen questionable." 121 No hydro oxygen. "Parity Error" on computer before data saved. Footnote oxygen lost. STATION 700 113 Delta-S .02 low at 1003db. Calc ok. CTD S trace shows no corresponding bump. Same value at NB14, probable dupe draw or run. Footnote salinity bad. 101 Sample log: "Small leak." Delta-S .001 low at 4407db. Other water samples also look ok. STATION 701 106 Sample log: "Leaking after air vent opened? (Also, there is an unintelligible note on sample log re this bottle) Same note in Russian?" Delta-S .000 at 2171db. Other water samples also ok. STATION 702 224 CTDO Processor: "Top 70db CTD oxygen questionable." 220 Delta-S .3 high at 212db. Other water samples also indicate NB20 closed deeper. Footnote bottle leaking, footnote samples bad. ODF recommends deletion of all water samples. Cast aborted. STATION 703 Cast 1 Tripping problem. 25 confirms. B file indicates 2 trips at 204db. Ramp shaft 1 position too far. 123-124 CTDO Processor: "Top 120db CTD oxygen questionable." 120 lower lanyard permitted lid closure too early Footnote bottle leaking, footnote samples bad. ODF recommends deletion of all water samples. 117 Sample log: "spigot too small for helium tube" 101 Sample log: "1 bot leak" Delta-S .000 at 2635db. Other water samples also ok. Note: NBs 1&7 reversed for freon check. S04P ð ODF BTL Data Report ð 1992 ð R/V Akademik Ioffe STATION 704 123-124 CTDO Processor: "Top 100db CTD oxygen questionable." 120 lower lanyard permitted lid closure too early Footnote bottle leaking, footnote samples bad. ODF recommends deletion of all water samples. 102 JHS: "OA suggests S high by 0.002." Delta-S .002 high at 4184db. Calc ok. Footnote salinity questionable. 101 Delta-S .004 low @ 2618db. Calc OK. Other water samples OK. Same value as NB8 above. Possible dupe draw or run. Note: NBs1&7 reversed for freon check. STATION 705 Cast 1 Rosette hit A-frame on recovery. Tripping problem. First bottle had no confirms on trip box, 5 confirms on ISI. Again looks like 2 bottles closed at bottom and no 10db sample. 124 CTDO Processor: "Top 100db CTD oxygen questionable." 120 Lower lanyard permitted lid closure too early Footnote bottle leaking, footnote samples bad. ODF recommends deletion of all water samples. 118 Delta-S .09 high at 505db. Other water samples indicate NB18 closed early. Possibly long lanyard allowed bottom end cap to close. Footnote bottle leaking, footnote samples bad. ODF recommends deletion of all water samples. 112 Sample log:"damaged on recovery" Broken spigot. Nuts & salt drawn but no oxygen. Nuts & salt look ok. 111 Sample log:"damage on recovery" Barrel broken about half way up. Nuts & salt drawn but no oxygen. Nuts & salinity data look ok. 110 Bottle did not trip as scheduled. SIL, NO3, NO2, PO4 not drawn 109 Sample log:"damaged on recovery." Spigot collar broken. No samples drawn. 108 Sample log:"Damaged on recovery. Missed O2." STATION 706 125 Sample log: "Leaking from bottom end cap." Delta-S .002 low at 2292db. Other water samples also look ok. 108 Delta-S .002 low at 2597db. But only samples with definite gradients, O2 & SIL, indicate NB8 closed at NB7 level. Changed tripping information file to 2894db. Samples appear to be okay and agree with duplicate trip. Footnote bottle didn't trip as scheduled. STATION 707 125 Delta-S .000 at 2161db but other water samples indicate NB25 closed near 1200db. Salinity same at 1200db & 2161db. Footnote bottle leaking, footnote samples bad. ODF recommends deletion of all water samples. 113 Delta-S .028 low at 1010db. Calc ok. Same value as NB14 above. Possible dupe draw or run. 102 JHS: "OA suggests S high by 0.002." Delta-S .002 high at 4636db. Calc ok. Footnote salinity questionable. STATION 708 Cast 1 Tripping problem? 2 ISI confirms on first bottle. Trip box & ramp shaft ok. Data indicates all bottles tripped as intended. JHS: "OA suggests NO3 may be "high" while PO4 is "low". However, may be O.K. (See Sta. 709.)." Nutrient Analyst: "Change PO4 F1E=4.455, B(E)=.068." NO3 column apparently failing; data may be slightly unreliable see Station 709. Footnote no3 questionable. DQE has recoded NO3 as acceptable, with the exception of bottles 25 and 15. Nutrient analyst reply to DQE comment: "NO3 looks okay, agree with DQE, code NO3 acceptable, except 15 code questionable." 125 Delta-S .01 low at 1999db. Other water samples also indicate NB25 leaked. Footnote bottle leaking, footnote water samples bad. ODF recommends deletion of all water samples. 124 CTDO Processor: "Top 12db CTD oxygen questionable." 122 Unintelligible note on sample log. Data ok. 120 Unintelligible note on sample log. Data ok. 115 DQE: "High NO3. Q1 noted whole station as having high NO3. Flag assigned: 3." 104 No hydro oxygen. "Parity error" on computer before data saved. Footnote oxygen lost. 103 Delta-S .004 high at 4292db. Calc ok. No corresponding bump on CTD S trace. JHS: "OA shows S 0.003 high." Footnote salinity questionable. S04P ð ODF BTL Data Report ð 1992 ð R/V Akademik Ioffe STATION 709 Cast 1 Lost CTD signal at 4339db coming up. Two bottles had been tripped with normal confirmations. Tripped remaining bottles on wire out. Problem was in CTD/transmissometer bulkhead connector. Entered estimated pressures for missing trips based on comparing wire out readings on previous station. Entered estimated temp for missing trips based on T-S curve and hydro salinity plus estimated pressure and Delta-S from down cast real-time printout. Footnote CTD pressure and temperature as extrapolated from CTD data down cast. Nutrient data sheet: "large NO3 drift - column?" Nitrates appear higher than adjacent stations. High end base. Replaced Cad column prior station 710 and NO3s back to normal. Nutrient Analyst: " NO3 920306."Base Shift" JHS: "OA sees high NO3 at 708 and 709." Footnote no3 questionable. Nutrient analyst: "After comments by DQE, reinvestigation indicates NO3 is questionable for 8, 25, 10, 26 and 12-19." 126 See Cast 1 Nutrient comment. Footnote NO3 questionable. 125 See Cast 1 Nutrient comment. Footnote NO3 questionable. DQE: "High NO3 with no increase in PO4. Flags assigned: 3." 123-124 CTDO Processor: "Top 80db CTD oxygen questionable." CTDO Processor refers to down trace. Signal lost on CTD, no CTD salinity or oxygen. 112-119 See Cast 1 Nutrient comment. Footnote NO3 questionable. 112-117 DQE: "High NO3 with no increase in PO4. Flags assigned: 3." 110 See Cast 1 Nutrient comment. Footnote NO3 questionable. DQE: "High NO3 with no increase in PO4. Flags assigned: 3." 108 See Cast 1 Nutrient comment. Footnote NO3 questionable. 106-108