*2003/07/22 11:36:29.34 *IOS HEADER VERSION 1.4 2002/12/04 2002/12/04 *FILE START TIME : GMT 1988/07/19 03:36:00.000 NUMBER OF RECORDS : 18 DATA DESCRIPTION : Bottle:Wire FILE TYPE : ASCII DATA TYPE : REAL*4 NUMBER OF CHANNELS : 2 $TABLE: CHANNELS ! No Name Units Minimum Maximum ! -- ------------------ -------- -------------- -------------- 1 Depth metres 0 1000 2 Oxygen:Dissolved mL/L 0.331 7.095 $END $TABLE: CHANNEL DETAIL ! No Pad Start Width Format Type Decimal_Places ! -- ---- ----- ----- ------ ---- -------------- 1 ' ' ' ' 7 F ' ' 1 2 ' ' ' ' 8 F ' ' 3 $END $REMARKS This file converted from 12 line header format. $END *ADMINISTRATION MISSION : 1988-12 AGENCY : IOS, Ocean Physics Division, Sidney, B.C. COUNTRY : Canada PROJECT : Laperouse SCIENTIST : Spearing L. PLATFORM : Parizeau *LOCATION GEOGRAPHIC AREA : WCVI STATION : LD09 EVENT NUMBER : 36 LATITUDE : 48 35.70000 N ! (deg min) LONGITUDE : 126 30.00000 W ! (deg min) *INSTRUMENT TYPE : Bottle MODEL : Niskin (1.7 litre) *HISTORY $TABLE: PROGRAMS ! Name Vers Date Time Recs In Recs Out ! -------- ------ ---------- -------- --------- --------- C12L_IOS 3.0 2000/11/03 09:27:27 18 18 HDREDIT2 1.6 2003/07/22 11:36:29 ? ? $END *COMMENTS DEPTH/OXYGEN DATA ONLY TAKEN Collection methods: ------------------- Sea Water Temperature: - Reversing thermometers mounted on bottles. Salinity: - Collected in bottles. Dissolved Oxygen: - 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 250 m or greater. The accuracy of protected reversing thermometers is believed to be +-0.02C. Salinity determinations were made at sea with a Guildline model 8400 lab salinometer. 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). !--1--- ---2--- !Depth Oxygen: ! Dissolv ! ed !------ ------- *END OF HEADER 0.0 6.123 10.0 6.137 20.0 7.095 30.0 6.665 50.0 6.513 75.0 6.349 100.0 5.201 125.0 4.432 150.0 3.820 175.0 3.645 200.0 3.283 250.0 3.185 300.0 2.641 400.0 1.361 500.0 0.856 600.0 0.779 800.0 0.331 1000.0 0.397