*2022/05/30 15:33:49.68 *IOS HEADER VERSION 2.0 2016/04/28 2016/06/13 IVF16 *FILE START TIME : UTC 2009/01/30 01:48:48.000 TIME INCREMENT : 0 0 0 0.416667E-01 0 ! (day hr min sec ms) NUMBER OF RECORDS : 24 DATA DESCRIPTION : Bottle:Rosette:Up:Stop + CTD:Up FILE TYPE : ASCII CRC : D43FA370 NUMBER OF CHANNELS : 10 $TABLE: CHANNELS ! No Name Units Minimum Maximum !--- ----------------------------- --------------- -------------- -------------- 1 Sample_Number n/a 82 105 2 Bottle_Number n/a 1 24 3 Pressure:CTD dbar 497.6 1301.6 4 Temperature:CTD deg_C_(ITS90) 2.7784 5.1256 5 Salinity:CTD PSS-78 34.1213 34.4884 6 Sigma-t:CTD kg/m^3 26.9903 27.5224 7 Transmissivity:CTD %/m 60.6 61.7 8 Oxygen:Dissolved:CTD:Volume ml/l 0.55 0.61 9 Oxygen:Dissolved:CTD:Mass µmol/kg 23.7 26.7 10 Fluorescence:CTD:Seapoint mg/m^3 0.108 0.114 $END $TABLE: CHANNEL DETAIL ! No Pad Start Width Format Type Decimal_Places !--- ---- ----- ----- ------ ---- -------------- 1 -99 ' ' 5 I I 0 2 -99 ' ' 3 I I 0 3 -99 ' ' 7 F ' ' 1 4 -99 ' ' 9 F ' ' 4 5 -99 ' ' 9 F ' ' 4 6 -99 ' ' 9 F R4 4 7 -99 ' ' 6 F ' ' 1 8 -99 ' ' 7 F ' ' 2 9 -99 ' ' 6 F ' ' 1 10 -99 ' ' 8 F ' ' 3 $END *ADMINISTRATION MISSION : 2009-003 AGENCY : IOS, Ocean Sciences Division, Sidney, B.C. COUNTRY : Canada PROJECT : Line P SCIENTIST : Robert M. PLATFORM : John P. Tully *LOCATION GEOGRAPHIC AREA : North-East Pacific STATION : P4 EVENT NUMBER : 13 LATITUDE : 48 39.06000 N ! (deg min) LONGITUDE : 126 40.01000 W ! (deg min) WATER DEPTH : 1317 *INSTRUMENT TYPE : Sea-Bird CTD MODEL : SBE-911plus SERIAL NUMBER : 0443 *COMMENTS Analysis methods: ----------------- Salinity samples were collected in glass bottles and analyzed at IOS on a Guildline model 8400B Autosal standardized with IAPSO standard seawater. See file 2009-003_SAL.pdf information on duplicates. Oxygen samples were analyzed at sea using an automated titration system consisting of a Brinkman Dosimat (model 665) and a PC 950 Colorimeter. For details on precision see file 2009-003_OXY.pdf. Nutrient samples were collected in plastic tubes and analyzed fresh at sea using an Astoria-Pacific autoanalyzer following methods described in Barwell-Clarke and Whitney (1996). For details on nutrient duplicates and precision see file 2009-003_NUT.pdf. Chlorophyll samples were analyzed at sea using a Chemistry Turner Designs 10AU fluorometer which was calibrated in April 2008 using pure chlorophyll a. Chlorophyll precision was determined by analyzing replicate samples drawn from one Niskin. For details on duplicates see file 2009-003_CHL.pdf. The minimum detectable level for DMS is 0.10 nM, so “0” values should be interpreted as <0.10. For details on the collection and analysis of the DMS data see file 2009-003_DMS_report.pdf and for duplicates see 2009-003_DMS.pdf. DMSP-D and DMSP-T: Contamination in the blanks resulted in all data being discarded. For details on analysis see document 2009-003_DMS_report.pdf. HPLC samples were filtered onto 47mm GF/F filters and stored at -80C prior to analysis. Samples were extracted in 95% methanol at -20C for 24 hours and analyzed on a WATERS 2695 HPLC separations system as detailed in Nemcek and Pena, 2014. Analysis was performed ~2 months after collection. The average of two samples is reported. Variability is assessed as the %CV (std dev/mean*100) for duplicate pairs. All pigments below the limit of detection (LOD) are assigned a zero value. TChl-a is the sum of Chl-a, DVchl-a and Chlide-a. References: 1. Carpenter, J.H. 1965. The Chesapeake Bay Institute Technique for the Winkler Dissolved Oxygen Method. Limmnol. & Oceanogr., 10: 141-143. 2. J. Barwell-Clarke and F. Whitney. 1996. Institute of Ocean Sciences Nutrient Methods and Analysis. Canadian Technical Report of Hydrography and Ocean Sciences, No. 182, 43 pp. 3. Nemcek, N. and Peña, M.A. 2014. Institute of Ocean Sciences Protocols for Phytoplankton Pigment Analysis by HPLC. Can. Tech. Rep. Fish. Aquat. Sci. 3117: x + 80 p. Data Processing Notes: ---------------------- Transmissometer #1005DR was calibrated in March 2008, and drifted significantly but steadily until July 2009; then a sudden shift occurred, so that maximum values between September 2009 and July 2010 were very low, ~25%/m. In August 2010 a study was made of transmissivity that led to a decision to apply post-processing corrections to all cruises between March 2008 and June 2010. Transmissivity data from this cruise were corrected by multiplying the original values by a correction factor, which was based on assumptions that deep offshore transmissivity from a June 2009 cruise should be about 62%/m and that drift was linear with time between March 2008 and July 2009. The corrections produced reasonable results for all cruises in that time period. For details on the transmissometer post-processing see: Transmissometer_1005DR_Corrections.pdf These data should be considered estimates. There were a number of problems with the SBE dissolved oxygen sensors that limit the reliability of the data: For casts 0001 to 0040 the data below 1400 dbar are considered less reliable than usual. For casts 0042 and 0044 the Oxygen:Dissolved:CTD channels were removed. For casts 0046 to 0060 there was no bottle sampling so the Oxygen:Dissolved:CTD data were recalibrated based on an intercomparison with casts using a different sensor. For details on the processing see processing report: 2009-003-proc.pdf. NOTE: July 2013: A correction has been applied to Nitrate_plus_Nitrite:Bottle and Phosphate:Bottle data from deep-water cruises analyzed at IOS between 2009 and 2012. For details see the report: Corrections_to_Nitrate_and_Phosphate_Data_2009-2012.pdf $REMARKS Quality flags have the following significance: ---------------------------------------------------------------------------------- 0 = Acceptable measurement with no header comment. 1 = Sample for this measurement was collected but not analyzed. Sample lost. 2 = Acceptable measurement with header comment. 3 = Questionable measurement (probably good). 4 = Poor measurement (probably bad). 5 = Measurement not reported (bad). 6 = Mean of replicate measurements. 7 = Manual chromatographic peak measurement. 8 = Irregular digital chromatographic peak integration. 9 = Sample was planned for this measurement from this bottle but was not collected. ----------------------------------------------------------------------------------- $END !-1-- 2- --3--- ---4---- ---5---- ---6---- --7-- --8--- --9-- ---10-- !Samp Bo Pressu Temperat Salinity Sigma-t: Trans Oxygen Oxyge Fluores !le_ tt re:CTD ure:CTD :CTD CTD missi :Disso n:Dis cence: !Numb ~u vity: lved: solve CTD: !er mb CTD CTD: d:CTD Seapoin ! er Volume :Mass t !---- -- ------ -------- -------- -------- ----- ------ ----- ------- *END OF HEADER 105 24 498.4 5.1256 34.1217 26.9903 61.7 0.61 26.6 0.109 104 23 498.6 5.1235 34.1215 26.9903 61.7 0.61 26.7 0.112 103 22 499.1 5.1244 34.1216 26.9903 61.7 0.61 26.6 0.109 102 21 498.5 5.1240 34.1215 26.9903 61.7 0.61 26.6 0.111 101 20 497.6 5.1224 34.1214 26.9904 61.7 0.61 26.6 0.112 100 19 497.7 5.1217 34.1214 26.9905 61.7 0.61 26.7 0.109 99 18 498.3 5.1231 34.1216 26.9905 61.7 0.61 26.7 0.109 98 17 498.8 5.1227 34.1216 26.9905 61.7 0.61 26.6 0.110 97 16 499.1 5.1243 34.1217 26.9904 61.7 0.61 26.6 0.110 96 15 498.7 5.1236 34.1217 26.9905 61.7 0.61 26.6 0.108 95 14 498.2 5.1210 34.1213 26.9905 61.7 0.61 26.6 0.111 94 13 498.4 5.1205 34.1213 26.9905 61.7 0.61 26.6 0.111 93 12 1299.5 2.7784 34.4884 27.5224 60.6 0.55 23.8 0.114 92 11 1299.6 2.7791 34.4882 27.5222 60.6 0.55 23.8 0.113 91 10 1299.9 2.7791 34.4883 27.5222 60.6 0.55 23.8 0.113 90 9 1301.3 2.7790 34.4882 27.5222 60.6 0.55 23.8 0.114 89 8 1300.4 2.7794 34.4883 27.5222 60.6 0.55 23.7 0.112 88 7 1300.6 2.7794 34.4882 27.5221 60.6 0.55 23.9 0.112 87 6 1300.9 2.7796 34.4883 27.5222 60.6 0.55 23.8 0.114 86 5 1301.4 2.7796 34.4882 27.5221 60.6 0.55 23.8 0.111 85 4 1300.7 2.7796 34.4882 27.5221 60.6 0.55 23.9 0.113 84 3 1299.9 2.7796 34.4881 27.5220 60.6 0.55 23.8 0.114 83 2 1301.6 2.7793 34.4881 27.5221 60.6 0.55 23.8 0.113 82 1 1301.0 2.7796 34.4881 27.5220 60.6 0.55 23.9 0.113