*2003/06/30 17:22:10.51 *IOS HEADER VERSION 1.4 2002/12/04 2002/12/04 *FILE START TIME : UTC 1984/06/27 14:06:00.000 NUMBER OF RECORDS : 9 DATA DESCRIPTION : Bottle:Wire FILE TYPE : ASCII DATA TYPE : REAL*4 PAD : -99 NUMBER OF CHANNELS : 2 $TABLE: CHANNELS ! No Name Units Minimum Maximum ! -- ------------------ -------- -------------- -------------- 1 Depth metres 0 150 2 Oxygen:Dissolved mL/L 2.138 7.253 $END $TABLE: CHANNEL DETAIL ! No Pad Start Width Format Type Decimal_Places ! -- ---- ----- ----- ------ ---- -------------- 1 -99 ' ' 7 F ' ' 1 2 -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: 8412R0054818.80N125 4.00W84 62714 6GMT136 4DTSO 150 90.0H $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 : R005 EVENT NUMBER : 136 LATITUDE : 48 18.80000 N ! (deg min) LONGITUDE : 125 4.00000 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 16:54:13 9 9 HDREDIT2 1.6 2003/06/30 17:22:01 ? ? CLEAN 4.3 2003/06/30 17:22:10 9 9 $END $REMARKS CLEAN functions: - Reset #RECS, MIN & MAX values in header. - Change Pad Value to -99 in All Channels. - Delete Empty Channels: 2 deleted. - Set channel name post-colon letters to upper case. - Set last 4 characters of file name to event $END !--1--- ---2--- !Depth Oxygen: ! Dissolv ! ed !------ ------- *END OF HEADER 0.0 7.253 10.0 6.929 20.0 3.880 30.0 3.180 50.0 2.447 75.0 2.345 100.0 2.257 125.0 2.138 150.0 2.342