*2003/07/22 16:24:39.98 *IOS HEADER VERSION 1.4 2002/12/04 2002/12/04 *FILE START TIME : GMT 1989/04/24 11:36:00.000 NUMBER OF RECORDS : 20 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 1500 2 Oxygen:Dissolved mL/L 0.368 7.189 $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 : 1989-10 AGENCY : IOS, Ocean Physics Division, Sidney, B.C. COUNTRY : Canada PROJECT : Laperouse SCIENTIST : Juhasz T. PLATFORM : Parizeau *LOCATION GEOGRAPHIC AREA : WCVI, GEORGIA, JUAN DE FUCA STATION : LC11 EVENT NUMBER : 5 LATITUDE : 48 18.00000 N ! (deg min) LONGITUDE : 126 27.20000 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 09:34:24 20 20 HDREDIT2 1.6 2003/07/22 16:24:39 ? ? $END *COMMENTS 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 6.942 10.0 7.189 20.0 7.110 30.0 6.609 50.0 5.846 75.0 4.468 100.0 3.847 125.0 3.211 150.0 3.015 175.0 2.951 200.0 2.779 250.0 2.377 300.0 2.142 400.0 1.371 500.0 0.834 600.0 0.564 800.0 0.368 1000.0 0.558 1200.0 0.437 1500.0 0.665