*2003/07/02 14:40:11.53 *IOS HEADER VERSION 1.4 2002/12/04 2002/12/04 *FILE START TIME : UTC 1985/09/29 12:48:00.000 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 773 2223 2 Temperature:Reversing 'deg C (IPTS68)' 1.84 3.97 3 Salinity:Bottle PSS-78 34.263 34.612 4 Oxygen:Dissolved mL/L 0.393 1.735 $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: 8511H00548 0.80N129 1.80W85 9291248GMT 4 4DTSO 2223 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 : H005 EVENT NUMBER : 4 LATITUDE : 48 0.80000 N ! (deg min) LONGITUDE : 129 1.80000 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 16:57:44 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 773.0 3.97 34.263 0.393 1273.0 2.92 34.463 0.486 1773.0 2.13 34.561 1.206 1973.0 1.96 34.587 1.426 2023.0 1.93 34.593 1.482 2073.0 1.90 34.599 1.577 2123.0 1.87 34.605 1.621 2173.0 1.86 34.606 1.675 2223.0 1.84 34.612 1.735