*2004/03/26 10:44:19.62 *IOS HEADER VERSION 1.4 2002/12/04 2002/12/04 *FILE START TIME : UTC 1984/11/10 12:36:00.000 NUMBER OF RECORDS : 21 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 1977 2 Temperature:Reversing 'deg C' 1.93 10.16 3 Salinity:Bottle ppt 32.462 34.584 4 Oxygen:Dissolved mL/L 0.307 6.384 5 Oxygen:Dissolved umol/kg 13.3 278.1 $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 STDHYD84.DAT using SUStoIOS.BAS version 2.3 Sep 04/96 rmb Original HEADER: 84 3P01449 7.40N13240.00W8411101236GMT 20 4DTSO 1977 210.0H $END *ADMINISTRATION MISSION : 1984-03 AGENCY : IOS, Ocean Physics Division, Sidney, B.C. COUNTRY : Canada PROJECT : Line P SCIENTIST : Bellegay R. PLATFORM : Parizeau *LOCATION GEOGRAPHIC AREA : NE PACIFIC STATION : P014 EVENT NUMBER : 20 LATITUDE : 49 7.40000 N ! (deg min) LONGITUDE : 132 40.00000 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 16:55:46 21 21 CHGUNITS 1.3 2002/06/13 11:32:33 21 21 HDREDIT2 1.5 2002/07/23 13:29:53 ? ? CLEAN 3.7 2002/07/23 13:29:58 21 21 HDREDIT2 1.9 2004/03/26 10:44:19 ? ? $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. 10.15 32.462 6.367 277.3 10. 10.16 32.467 6.371 277.5 20. 10.12 32.464 6.373 277.6 30. 10.13 32.468 6.384 278.1 50. 10.08 32.475 6.375 277.7 75. 8.53 32.721 6.007 261.5 99. 7.42 33.150 4.794 208.6 124. 7.05 33.576 3.815 165.9 149. 6.82 33.709 3.656 159.0 174. 6.58 33.797 3.557 154.7 198. 6.26 33.858 3.370 146.5 248. 5.75 33.895 2.751 119.6 297. 5.36 33.923 2.190 95.2 396. 4.72 33.996 1.312 57.0 494. 4.26 34.061 0.917 39.9 593. 3.93 34.134 0.670 29.1 790. 3.48 34.276 0.353 15.3 987. 3.11 34.359 0.307 13.3 1186. 2.76 34.426 0.403 17.5 1483. 2.32 34.505 0.666 28.9 1977. 1.93 34.584 1.373 59.6