*2002/07/23 13:39:42.48 *IOS HEADER VERSION 1.3 1999/04/13 1999/12/09 *FILE START TIME : UTC 1985/11/13 06:30:00.000 NUMBER OF RECORDS : 25 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 1494 2 Temperature:Reversing 'deg C' 2.4 10.14 3 Salinity:Bottle PSS-78 32.418 34.502 4 Oxygen:Dissolved mL/L 0.349 6.671 5 Oxygen:Dissolved umol/kg 15.2 290.4 $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 STDHYD85.DAT using SUStoIOS.BAS version 2.3 Sep 04/96 rmb Original HEADER: 85 4P0124858.20N13040.00W851113 630GMT 54 4DTSO 1494 250.0H $END *ADMINISTRATION MISSION : 1985-04 AGENCY : IOS, Ocean Physics Division, Sidney, B.C. COUNTRY : Canada PROJECT : Line P SCIENTIST : Bellegay R. PLATFORM : John P. Tully *LOCATION GEOGRAPHIC AREA : NE PACIFIC STATION : P012 EVENT NUMBER : 54 LATITUDE : 48 58.20000 N ! (deg min) LONGITUDE : 130 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 16:58:02 25 25 CHGUNITS 1.3 2002/06/24 14:07:00 25 25 HDREDIT2 1.5 2002/07/23 13:39:35 ? ? CLEAN 3.7 2002/07/23 13:39:42 25 25 $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. 10.12 32.419 6.477 282.1 10. 10.09 32.418 6.467 281.7 20. 10.12 32.428 6.471 281.9 30. 10.11 32.421 6.466 281.6 40. 10.14 32.422 6.473 281.9 50. 10.11 32.425 6.468 281.7 60. 8.09 32.590 6.671 290.4 75. 7.40 32.657 6.492 282.6 80. 7.43 32.659 6.495 282.7 100. 7.33 32.879 5.900 256.8 119. 7.11 33.516 4.533 197.2 124. 7.03 -99.000 -99.000 -99.0 149. 6.69 33.841 3.838 166.9 174. 6.40 33.888 3.533 153.6 199. 6.14 33.903 3.114 135.4 249. 5.50 33.917 2.611 113.5 300. 5.37 33.956 1.939 84.3 400. 4.89 34.026 1.170 50.9 500. 4.26 34.077 0.880 38.3 598. 3.97 34.165 0.726 31.6 699. 3.72 34.222 0.520 22.6 797. 3.52 34.291 0.437 19.0 996. 3.17 34.380 0.349 15.2 1195. 2.81 34.438 0.503 21.9 1494. 2.40 34.502 0.773 33.6