*2002/06/27 09:58:49.34 *IOS HEADER VERSION 1.3 1999/04/13 1999/12/09 *FILE START TIME : GMT 1981/10/26 19:00:00.000 NUMBER OF RECORDS : 22 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 1999 2 Temperature:Reversing 'deg C' 1.91 12.11 3 Salinity:Bottle ppt 32.228 34.595 $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 12 line header format. $END *ADMINISTRATION MISSION : 1981-06 AGENCY : IOS, Offshore Oceanography, Sidney, B.C. COUNTRY : Canada PROJECT : Line P SCIENTIST : De Jong C. PLATFORM : Parizeau *LOCATION GEOGRAPHIC AREA : NE Pacific STATION : R8 EVENT NUMBER : 52 LATITUDE : 51 21.20000 N ! (deg min) LONGITUDE : 134 32.70000 W ! (deg min) *INSTRUMENT TYPE : Bottle MODEL : Niskin *HISTORY $TABLE: PROGRAMS ! Name Vers Date Time Recs In Recs Out ! -------- ------ ---------- -------- --------- --------- C12L_IOS 3.0 2002/06/10 16:01:39 22 22 HDREDIT2 1.4 2002/06/10 16:07:00 ? ? CHGUNITS 1.3 2002/06/10 16:07:27 22 22 CLEAN 3.8 2002/06/10 16:08:08 22 22 HDREDIT2 1.5 2002/06/27 09:58:49 ? ? $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 *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. !--1-- --2--- ---3--- !Depth Temper Salinit ! ature: y: ! Revers Bottle ! ing !----- ------ ------- *END OF HEADER 0. 12.11 32.229 10. 12.06 32.229 20. 12.06 32.228 30. 12.09 32.236 51. 9.40 32.450 76. 7.54 32.613 101. 7.43 33.086 126. 6.45 33.488 151. 6.24 33.697 176. 6.04 33.801 201. 5.86 33.868 251. 5.55 33.902 300. 5.15 33.920 398. 4.42 33.987 501. 4.12 34.039 602. 3.84 34.145 803. 3.54 34.280 1002. 3.15 34.377 1201. 2.76 34.445 1498. 2.33 34.514 1989. 1.93 34.591 1999. 1.91 34.595