*2004/02/23 16:49:17.64 *IOS HEADER VERSION 1.4 2002/12/04 2002/12/04 *FILE START TIME : PST 1977/09/23 22:35:00.000 NUMBER OF RECORDS : 11 DATA DESCRIPTION : Bottle:Wire FILE TYPE : ASCII NUMBER OF CHANNELS : 7 $TABLE: CHANNELS ! No Name Units Minimum Maximum ! -- ----------------------- -------- -------------- -------------- 1 Depth metres 0 200 2 Oxygen:Dissolved mL/L 2.162 6.107 3 Salinity:Bottle ppt 31.532 33.726 4 Temperature:Reversing 'deg C' 5.24 12.73 5 Phosphate umol/L 0.83 2.89 6 Nitrate umol/L 4.1 34.8 7 Silicate umol/L 15.2 60.6 $END $TABLE: CHANNEL DETAIL ! No Pad Start Width Format Type Decimal_Places ! -- ---- ----- ----- ------ ---- -------------- 1 -99 ' ' 6 F R4 0 2 -99 ' ' 8 F R4 3 3 -99 ' ' 8 F R4 3 4 -99 ' ' 7 F R4 2 5 -99 ' ' 7 F R4 2 6 -99 ' ' 6 F R4 1 7 -99 ' ' 6 F R4 1 $END *ADMINISTRATION MISSION : 1977-14 AGENCY : IOS, Offshore Oceanography, Sidney, B.C. COUNTRY : Canada PROJECT : Inner Passage SCIENTIST : Thomson R.E. PLATFORM : Parizeau *LOCATION STATION : QD13 EVENT NUMBER : 23 LATITUDE : 52 53.50000 N ! (deg min) LONGITUDE : 129 55.90000 W ! (deg min) *HISTORY $TABLE: PROGRAMS ! Name Vers Date Time Recs In Recs Out ! -------- ------ ---------- -------- --------- --------- SPRD2IS 3.4.6 2001/12/17 10:57:35 11 11 HDREDIT2 1.6 2003/06/04 14:40:26 ? ? CLEAN 4.2 2003/06/04 14:42:28 11 11 HDREDIT2 1.9 2004/02/23 16:49:17 ? ? $END $REMARKS CLEAN functions: - Reset #RECS, MIN & MAX values in header. - Change Pad Value to -99 in All Channels. - Delete Empty Channels: 0 deleted. $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. 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). Nutrient samples are analyzed frozen using a Technicon autoanalyzer under contract to Seakem Oceanography Ltd. References: 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. !--1-- ---2--- ---3--- --4--- --5--- --6-- --7-- !Depth Oxygen: Salinit Temper Phosph Nitra Silic ! Dissolv y: ature: ate te ate ! ed Bottle Revers ! ing !----- ------- ------- ------ ------ ----- ----- *END OF HEADER 0. 6.107 31.532 12.73 0.86 4.5 15.3 10. 6.050 31.533 12.73 0.83 4.1 15.2 20. 6.046 31.536 12.73 0.85 4.3 16.8 30. 5.836 31.610 12.48 0.92 6.3 15.9 50. 4.030 32.465 8.78 2.03 18.6 30.2 75. 3.329 33.050 7.12 2.36 26.9 44.9 100. 2.833 33.375 6.56 2.33 30.1 52.9 125. 2.633 33.525 5.24 2.66 28.3 52.6 150. 2.362 33.637 6.01 2.74 34.8 57.2 175. 2.251 33.712 5.85 2.75 33.7 59.9 200. 2.162 33.726 5.75 2.89 34.1 60.6