*2002/07/23 13:47:03.91 *IOS HEADER VERSION 1.3 1999/04/13 1999/12/09 *FILE START TIME : UTC 1986/10/29 05:42:00.000 NUMBER OF RECORDS : 19 DATA DESCRIPTION : Bottle:Wire FILE TYPE : ASCII DATA TYPE : REAL*4 PAD : -99 NUMBER OF CHANNELS : 5 $TABLE: CHANNELS ! No Name Units Minimum Maximum ! -- ----------------------- --------- -------------- -------------- 1 Depth metres 0 1164 2 Temperature:Reversing 'deg C' 3.29 13.25 3 Salinity:Bottle PSS-78 32.157 34.39 4 Oxygen:Dissolved mL/L 0.278 6.603 5 Oxygen:Dissolved umol/kg 12.1 287.6 $END $TABLE: CHANNEL DETAIL ! No Pad Start Width Format Type Decimal_Places ! -- ---- ----- ----- ------ ---- -------------- 1 ' ' ' ' 6 F ' ' 0 2 ' ' ' ' 7 F ' ' 2 3 ' ' ' ' 8 F ' ' 3 4 ' ' ' ' 8 F ' ' 3 5 -99 ' ' 6 F ' ' 1 $END $REMARKS This file converted from STDHYD file STDHYD86.DAT using SUStoIOS.BAS version 2.3 Sep 04/96 rmb Original HEADER: 86 3A 034840.20N12638.80W861029 542GMT 8 4DTSO 1164 190.0H $END *ADMINISTRATION MISSION : 1986-03 AGENCY : IOS, Ocean Physics Division, Sidney, B.C. COUNTRY : Canada PROJECT : Line P SCIENTIST : Bellegay R. PLATFORM : Parizeau *LOCATION GEOGRAPHIC AREA : NE PACIFIC STATION : A 03 EVENT NUMBER : 8 LATITUDE : 48 40.20000 N ! (deg min) LONGITUDE : 126 38.80000 W ! (deg min) *INSTRUMENT TYPE : Bottle MODEL : Niskin *COMMENTS Sample collection methods: -------------------------- Sea Water Temperature: - Reversing thermometers mounted on bottles. Salinity: - Collected in bottles. Dissolved Oxygen: - Collected in bottles. Reactive Nutrients (Phosphate, nitrate, silicate): - Collected in bottles Analyzes methods: ------------------------- Temperatures at depth were measured by deep-sea reversing thermometers of German (Richter and Wiese) and/or Japanese (Yoshimo Keiki Co.) manufacture. Two protected thermometers were used on all bottles, and one unprotected thermometer was used on each bottle at depths of 300 m or greater. The accuracy of protected reversing thermometers is believed to be +-0.02C. Salinity determinations were made at sea with either a Guildline Autosal salinometer. Accuracy using duplicate determinations is estimated to be +-0.003 ppt. Depth determinations were made using the "depth difference" method described in the U.S.N. Hydrographic Office Publication No. 607 (1955). Depth estimates have an approximate accuracy of +-5 m for depths less than 1000 m, and +-0.5% of depth for depths greater than 1000 m. The dissolved oxygen analyses were done in the shipboard laboratory by a modified Winkler method (Carpenter, 1965). Nutrient samples were frozen for analyzes ashore. Chlorophyll and nutrients were analyzed using methods from Bulletin 125 Fisheries Research Board of Canada 1960 "A manual of seawater analysis" J.D.H. Strickland and T.R. Parsons, and subsequent editions. References: 1. Carpenter, J.H. 1965. The Chesapeake Bay Institute Technique for the Winkler Dissolved Oxygen Method. Limmnol. & Oceanogr., 10: 141-143. 2. Strickland, J.D.H., and T.R. Parsons. 1968. A Practical Handbook of Seawater Analysis. Bullettin 167. Fisheries Research Board, Canada. 3. Strickland, J.D.H., and T.R. Parsons. 1972. A Practical Handbook of Seawater Analysis. Bullettin 167 (2nd edition). Fisheries Research Board, Canada. *HISTORY $TABLE: PROGRAMS ! Name Vers Date Time Recs In Recs Out ! -------- ------ ---------- -------- --------- --------- PADZEROS 1.0 1996/09/04 16:58:25 19 19 CHGUNITS 1.3 2002/06/26 16:04:13 19 19 HDREDIT2 1.5 2002/07/23 13:46:52 ? ? CLEAN 3.7 2002/07/23 13:47:03 19 19 $END $REMARKS CHANGE units: - Units changed from ml/l to umol/kg CLEAN functions: - Reset #RECS, MIN & MAX values in header. - Delete Empty Channels: 0 deleted. - Set channel name post-colon letters to upper case. - Set last 4 characters of file name to event $END !--1-- --2--- ---3--- ---4--- --5-- !Depth Temper Salinit Oxygen: Oxyge ! ature: y: Dissolv n: ! Revers Bottle ed Disso ! ing lved !----- ------ ------- ------- ----- *END OF HEADER 0. 13.25 32.157 6.230 271.6 10. 13.24 32.157 6.201 270.3 20. 12.96 32.190 6.192 269.9 30. 10.64 32.434 6.603 287.6 49. 9.04 32.564 6.081 264.8 74. 8.09 32.948 5.042 219.5 99. 7.74 -99.000 4.309 -99.0 124. 7.85 33.697 3.429 149.2 148. 7.60 33.840 3.144 136.7 173. 7.29 33.909 2.887 125.6 198. 7.15 33.952 2.430 105.7 248. 6.44 33.928 3.100 134.8 298. 5.90 33.933 2.494 108.4 398. 5.29 33.975 1.692 73.6 498. 5.12 34.067 0.938 40.8 597. 4.72 34.130 0.601 26.1 792. 4.01 34.264 0.301 13.1 982. 3.68 34.350 0.278 12.1 1164. 3.29 34.390 0.516 22.4