*2003/07/02 14:40:11.46 *IOS HEADER VERSION 1.4 2002/12/04 2002/12/04 *FILE START TIME : UTC 1985/09/29 06:24:00.000 NUMBER OF RECORDS : 9 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 925 2375 2 Temperature:Reversing 'deg C (IPTS68)' 1.82 3.62 3 Salinity:Bottle PSS-78 34.367 34.621 4 Oxygen:Dissolved mL/L 0.469 1.88 $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 STDHYD85.DAT using SUStoIOS.BAS version 2.3 Sep 04/96 rmb Original HEADER: 8511F0064756.00N12910.20W85 929 624GMT 2 4DTSO 2375 90.0H $END *ADMINISTRATION MISSION : 1985-11 AGENCY : IOS, Ocean Physics Division, Sidney, B.C. COUNTRY : Canada PROJECT : Endeavour Ridge SCIENTIST : Thompson R.E. PLATFORM : Parizeau *LOCATION GEOGRAPHIC AREA : NE PACIFIC STATION : F006 EVENT NUMBER : 2 LATITUDE : 47 56.00000 N ! (deg min) LONGITUDE : 129 10.20000 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 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). *HISTORY $TABLE: PROGRAMS ! Name Vers Date Time Recs In Recs Out ! -------- ------ ---------- -------- --------- --------- PADZEROS 1.0 1996/09/04 16:57:42 9 9 HDREDIT2 1.6 2003/07/02 14:35:27 ? ? CLEAN 4.3 2003/07/02 14:40:11 9 9 $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. $END !--1--- --2--- ---3--- ---4--- !Depth Temper Salinit Oxygen: ! ature: y: Dissolv ! Revers Bottle ed ! ing !------ ------ ------- ------- *END OF HEADER 925.0 3.62 34.367 0.469 1425.0 2.58 34.507 0.786 1925.0 1.95 34.593 1.620 2125.0 1.90 34.606 1.743 2175.0 1.86 34.610 1.769 2225.0 1.84 34.617 1.784 2275.0 1.83 34.621 1.858 2325.0 1.83 34.621 1.832 2375.0 1.82 34.619 1.880