*2004/02/23 13:56:55.12 *IOS HEADER VERSION 1.4 2002/12/04 2002/12/04 *FILE START TIME : PST 1978/05/26 07:37:00.000 NUMBER OF RECORDS : 14 DATA DESCRIPTION : Bottle:Wire FILE TYPE : ASCII NUMBER OF CHANNELS : 4 $TABLE: CHANNELS ! No Name Units Minimum Maximum ! -- ----------------------- -------- -------------- -------------- 1 Depth metres 0 400 2 Oxygen:Dissolved mL/L 3.905 38.865 3 Salinity:Bottle ppt 31.511 33.001 4 Temperature:Reversing 'deg C' 7.32 8.8 $END $TABLE: CHANNEL DETAIL ! No Pad Start Width Format Type Decimal_Places ! -- ---- ----- ----- ------ ---- -------------- 1 -9.9 ' ' 6 F R4 0 2 -9.9 ' ' 8 F R4 3 3 -9.9 ' ' 8 F R4 3 4 -9.9 ' ' 7 F R4 2 $END *ADMINISTRATION MISSION : 1978-15 AGENCY : IOS, Offshore Oceanography, Sidney, B.C. COUNTRY : Canada PROJECT : Inner Passage SCIENTIST : Thomson R.E. PLATFORM : Parizeau *LOCATION STATION : QT10 EVENT NUMBER : 45 LATITUDE : 50 48.40000 N ! (deg min) LONGITUDE : 127 35.60000 W ! (deg min) *HISTORY $TABLE: PROGRAMS ! Name Vers Date Time Recs In Recs Out ! -------- ------ ---------- -------- --------- --------- SPRD2IS 3.4.5 2001/12/03 14:31:46 14 14 HDREDIT2 1.9 2004/02/23 13:56:55 ? ? $END *INSTRUMENT TYPE : Bottle MODEL : Niskin (1.7 litre) *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 so that depths could be calculated. 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). References: 1. R.E. Thomson, W.S. Hugget and L.S.C. Kuwahara. 1980. Data Record of Current Observations Volume VIII; Discovery Passage, Johnstone Strait, and Queen Charlotte Strait; Part 1 - Water Property Observations 1976, 1977, 1978,(1979). Institute of Ocean Sciences. 2. R.E. Thomson, W.S. Hugget and L.S.C. Kuwahara. 1980. Data Record of Current Observations Volume VIII; Discovery Passage, Johnstone Strait, and Queen Charlotte Strait; Part 2 - Appendices (listing of Water property data) Appendix A(1) - 1976 and 1977. Institute of Ocean Sciences. 3. R.E. Thomson, W.S. Hugget and L.S.C. Kuwahara. 1980. Data Record of Current Observations Volume VIII; Discovery Passage, Johnstone Strait, and Queen Charlotte Strait; Part 2 - Appendices (listing of Water property data) Appendices C,D,E - 1976,1977,1978,(1979). Institute of Ocean Sciences. !--1-- ---2--- ---3--- --4--- !Depth Oxygen: Salinit Temper ! Dissolv y: ature: ! ed Bottle Revers ! ing !----- ------- ------- ------ *END OF HEADER 0. 6.489 31.511 8.80 10. 6.109 31.686 8.59 20. 6.072 31.855 8.59 30. 6.042 31.957 8.60 50. 5.996 32.132 8.62 75. 5.299 32.329 8.18 100. 4.979 32.470 7.93 125. 4.729 32.609 7.80 150. 4.445 32.717 7.63 175. 4.156 32.869 7.46 200. 4.138 32.903 7.42 250. 4.067 32.943 7.38 300. 3.905 32.984 7.34 400. 38.865 33.001 7.32