*2013/12/16 15:16:30.23 *IOS HEADER VERSION 1.10 2011/10/26 2011/10/26 *FILE START TIME : UTC 1998/07/20 01:40:54.000 TIME INCREMENT : 0 0 0 0.416667E-01 0 ! (day hr min sec ms) NUMBER OF RECORDS : 21 DATA DESCRIPTION : Bottle:Rosette:Up:Stop FILE TYPE : ASCII NUMBER OF CHANNELS : 4 $TABLE: CHANNELS ! No Name Units Minimum Maximum !--- ------------------ --------- -------------- -------------- 1 Sample_Number n/a 336 356 2 Pressure decibar 2.4 1575.4 3 Oxygen:Dissolved mL/L 0.266 7.425 4 Salinity:Bottle PSS-78 34.3125 34.5219 $END $TABLE: CHANNEL DETAIL ! No Pad Start Width Format Type Decimal_Places !--- ---- ----- ----- ------ ---- -------------- 1 -99 ' ' 5 I I 0 2 -99 ' ' 7 F ' ' 1 3 -99 ' ' 8 F ' ' 3 4 -99 ' ' 9 F ' ' 4 $END *ADMINISTRATION MISSION : 1998-23 AGENCY : IOS, Ocean Science and Productivity, Sidney, B.C. COUNTRY : Canada PROJECT : Laperouse, GLOBEC SCIENTIST : Thomson R.E. PLATFORM : John P. Tully *LOCATION GEOGRAPHIC AREA : West Coast of Vancouver Island STATION : LF09 EVENT NUMBER : 237 LATITUDE : 48 45.85000 N ! (deg min) LONGITUDE : 126 57.00000 W ! (deg min) WATER DEPTH : 1395 *HISTORY $TABLE: PROGRAMS ! Name Vers Date Time Recs In Recs Out ! ------------------------ ------ ---------- -------- --------- --------- CALIB 7.5 1999/04/21 09:36:28 21 21 REMOVECH 3.2 2000/01/11 15:24:12 21 21 HDREDIT2 1.8 2004/01/13 09:47:28 ? ? SORT 3.4.1 2004/01/13 09:49:08 21 21 CLEAN 4.5 2004/01/13 09:49:42 21 21 CHANGE_CTD_CHANNEL_NAMES 1.0 2013/12/16 15:16:30 21 21 $END $REMARKS -The following CALIB parameters were used: Calibration type = C Pressure offset = 0.0 Calibration file = d:\data\1998\9823\9823oxy.cor -The following CHANNEL(S) were removed from file. SALINITY:PRIMARY SALINITY:SECONDARY TEMPERATURE:SECONDARY Temperature:Primary Salinity:T0:C0 Salinity:T1:C1 TEMPERATURE:SAMPLE DISSOLVED_OXYGEN:MASS THIOSULFATE_TITER FLASK_NUMBER FLASK_VOLUME BLANK STANDARD Irradiance_PAR Chl_fluorescence Transmissivity Bottle_Number SALINITY:CTD TEMPERATURE:CTD Temperature -The following SORT parameters were used. Sorted by channel: Pressure Pressure channel sorted according to values in sort channel CLEAN functions: - Reset #RECS, MIN & MAX values in header. - Change Pad Value to -99 in All Channels. - Delete Empty Channels: 0 deleted. - Set channel name post-colon letters to upper case. - Remove Sea-Bird comments from the header. $END *CALIBRATION $TABLE: CORRECTED CHANNELS ! Name Units Fmla Pad Coefficients ! ------------------------- ------ ---- ------ ------------ Dissolved_Oxygen:volume ml/l 10 -99 () (0 0.9988) $END *INSTRUMENT TYPE : Bottle MODEL : Niskin 10 Litre *COMMENTS Collection method: ------------------ A rosette, holding 24 ten-litre water samplers, with a CTD was used. Analysis methods: ----------------- Salinity samples are collected in glass bottles and analyzed on Guildline model 8410 Portasal Salinometers which are standardized with IAPSO standard seawater. Oxygen samples are analyzed on an automated Winkler titration system following the procedures of Carpenter (1965). A Brinkmann model 665 Dosimat and model PC910 Colorimeter is controlled by Visual-Basic program to titrate the oxygen samples. Nutrient samples are analyzed frozen on shore using a Technicon AAII auto- analyzer following methods described in Barwell-Clarke and Whitney (1996). Chlorophyll was extracted with 90% acetone and analyzed fluorimetrically. 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. Minkley, B.G., and F.A. Whitney. 2001. Summary of Hydrographic/CTD Observations Made Along Line P and at Station P: 1991-1999. Canadian Data Report of Hydrography and Ocean Sciences 156: 45 pp. !-1-- --2--- ---3--- ---4---- !Samp Pressu Oxygen: Salinity !le_ re Dissolv :Bottle !Numb ed !er !---- ------ ------- -------- *END OF HEADER 356 2.4 6.111 -99.0000 355 9.7 6.160 -99.0000 354 20.3 7.425 -99.0000 353 31.2 6.353 -99.0000 352 49.7 6.316 -99.0000 351 75.1 6.150 -99.0000 350 100.3 5.690 -99.0000 349 123.0 4.081 -99.0000 348 149.0 2.997 -99.0000 347 173.9 2.718 -99.0000 346 198.1 3.168 -99.0000 345 250.2 2.823 -99.0000 344 302.6 2.357 -99.0000 343 400.9 1.200 -99.0000 342 503.2 0.747 -99.0000 341 604.2 0.430 -99.0000 340 801.6 0.266 34.3125 339 999.9 0.328 34.4047 338 1198.8 0.514 34.4612 337 1500.7 0.675 34.5093 336 1575.4 0.786 34.5219