*2002/06/27 10:03:49.67 *IOS HEADER VERSION 1.3 1999/04/13 1999/12/09 *FILE START TIME : UTC 1982/11/28 21:30:00.000 NUMBER OF RECORDS : 29 DATA DESCRIPTION : Bottle:Wire FILE TYPE : ASCII DATA TYPE : REAL*4 PAD : -99 NUMBER OF CHANNELS : 3 $TABLE: CHANNELS ! No Name Units Minimum Maximum ! -- ----------------------- -------- -------------- -------------- 1 Depth metres 0 4138 2 Temperature:Reversing 'deg C' 1.5 7.59 3 Salinity:Bottle ppt 32.545 34.683 $END $TABLE: CHANNEL DETAIL ! No Pad Start Width Format Type Decimal_Places ! -- ---- ----- ----- ------ ---- -------------- 1 ' ' ' ' 6 F ' ' 0 2 ' ' ' ' 7 F ' ' 2 3 ' ' ' ' 8 F ' ' 3 $END $REMARKS This file converted from STDHYD file STDHYD82.DAT using SUStoIOS.BAS version 2.3 Sep 04/96 rmb Original HEADER: 82 6P26 50 0.00N145 0.00W8211282130GMT 40 3DTS 4138 29 H $END *ADMINISTRATION MISSION : 1982-06 AGENCY : IOS, Offshore Oceanography, Sidney, B.C. COUNTRY : Canada PROJECT : Line P SCIENTIST : De Jong C. PLATFORM : Endeavour *LOCATION GEOGRAPHIC AREA : NE PACIFIC STATION : P26 EVENT NUMBER : 40 LATITUDE : 50 0.00000 N ! (deg min) LONGITUDE : 145 0.00000 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. 4. S. Tabata and R. M. Brown. 1994. Hydrographic/CTD Observations Made During Ocean Climate Monitoring Study: 1981-1991 - A Summary of Operational Phase of Study. Canadian Data Report of Hydrography and Ocean Sciences, No. 136, 42 pp. *HISTORY $TABLE: PROGRAMS ! Name Vers Date Time Recs In Recs Out ! -------- ------ ---------- -------- --------- --------- PADZEROS 1.0 1996/09/04 16:49:11 29 29 CHGUNITS 1.3 2002/06/11 14:20:07 29 29 HDREDIT2 1.4 2002/06/11 14:20:19 ? ? CLEAN 3.8 2002/06/11 14:20:24 29 29 HDREDIT2 1.5 2002/06/27 10:03:49 ? ? $END $REMARKS CHANGE units: - No units changed 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--- !Depth Temper Salinit ! ature: y: ! Revers Bottle ! ing !----- ------ ------- *END OF HEADER 0. 7.56 32.545 10. 7.53 32.548 20. 7.57 32.563 30. 7.57 32.571 50. 7.59 32.575 75. 5.45 32.768 100. 4.30 32.983 125. 4.10 33.486 150. 3.96 -99.000 174. 3.91 33.747 199. 3.84 33.786 247. 3.80 -99.000 296. 3.75 33.906 394. 3.77 34.040 494. 3.64 34.134 596. 3.48 34.204 797. 3.17 34.313 984. 2.88 34.391 1174. 2.62 34.454 1461. 2.30 34.519 1949. 1.96 34.595 2444. 1.73 34.629 2942. 1.59 34.652 3441. 1.52 34.668 3938. 1.51 34.679 4036. 1.50 -99.000 4125. 1.52 34.680 4134. 1.50 34.682 4138. 1.50 34.683