*2003/06/30 17:22:09.53 *IOS HEADER VERSION 1.4 2002/12/04 2002/12/04 *FILE START TIME : UTC 1984/06/24 20:18:00.000 NUMBER OF RECORDS : 12 DATA DESCRIPTION : Bottle:Wire FILE TYPE : ASCII DATA TYPE : REAL*4 PAD : -99 NUMBER OF CHANNELS : 4 $TABLE: CHANNELS ! No Name Units Minimum Maximum ! -- ----------------------- ---------------- -------------- -------------- 1 Depth metres 0 500 2 Temperature:Reversing 'deg C (IPTS68)' 4.78 4.78 3 Salinity:Bottle PSS-78 34.1 34.1 4 Oxygen:Dissolved mL/L 0.86 6.675 $END $TABLE: CHANNEL DETAIL ! No Pad Start Width Format Type Decimal_Places ! -- ---- ----- ----- ------ ---- -------------- 1 -99 ' ' 7 F ' ' 1 2 -99 ' ' 7 F ' ' 2 3 -99 ' ' 8 F ' ' 3 4 -99 ' ' 8 F ' ' 3 $END $REMARKS This file converted from STDHYD file STDHYD84.DAT using SUStoIOS.BAS version 2.3 Sep 04/96 rmb Original HEADER: 8412G00649 3.50N127 1.00W84 6242018GMT 65 4DTSO 500 120.0H $END *ADMINISTRATION MISSION : 1984-12 AGENCY : IOS, Offshore Oceanography, Sidney, B.C. COUNTRY : Canada PROJECT : CCEXP SCIENTIST : Thomson R.E. PLATFORM : Parizeau *LOCATION GEOGRAPHIC AREA : NE PACIFIC STATION : G006 EVENT NUMBER : 65 LATITUDE : 49 3.50000 N ! (deg min) LONGITUDE : 127 1.00000 W ! (deg min) *INSTRUMENT TYPE : Bottle MODEL : Niskin (1.7 litre) *COMMENTS Converted from SUS TABATA's STDHYD data files by Robin Brown 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 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: Thomson,R.E., B.M. Hickey and P.H. LeBlond. 1986. Water Property Observation from the Vancouver Island Coastal Current Experiment: June, July and October 1984. Can. Data Rep. Hydrogr. Ocean Sci. 46: 505p. *HISTORY $TABLE: PROGRAMS ! Name Vers Date Time Recs In Recs Out ! -------- ------ ---------- -------- --------- --------- PADZEROS 1.0 1996/09/04 16:52:50 12 12 HDREDIT2 1.6 2003/06/30 17:22:00 ? ? CLEAN 4.3 2003/06/30 17:22:09 12 12 $END $REMARKS CLEAN functions: - Reset #RECS, MIN & MAX values in header. - Change Pad Value to -99 in All Channels. - Delete Empty Channels: 0 deleted. - Set channel name post-colon letters to upper case. - Set last 4 characters of file name to event $END !--1--- --2--- ---3--- ---4--- !Depth Temper Salinit Oxygen: ! ature: y: Dissolv ! Revers Bottle ed ! ing !------ ------ ------- ------- *END OF HEADER 0.0 -99.00 -99.000 6.675 10.0 -99.00 -99.000 6.667 20.0 -99.00 -99.000 6.545 30.0 -99.00 -99.000 6.603 50.0 -99.00 -99.000 6.434 75.0 -99.00 -99.000 5.464 100.0 -99.00 -99.000 3.819 125.0 -99.00 -99.000 3.387 150.0 -99.00 -99.000 3.293 200.0 -99.00 -99.000 3.095 300.0 -99.00 -99.000 1.956 500.0 4.78 34.100 0.860