*2024/12/03 09:08:57.48 *IOS HEADER VERSION 2.0 2016/04/28 2016/06/13 IVF16 *FILE START TIME : UTC 1985/06/15 17:42:00.000 NUMBER OF RECORDS : 10 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 0 172 2 Oxygen:Dissolved mL/L 1.57 5.964 $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 STDHYD85.DAT using SUStoIOS.BAS version 2.3 Sep 04/96 rmb Original HEADER: 854119 4823.60N12511.20W85 6151742GMT 69 4DTSO 172 100.0H $END *ADMINISTRATION MISSION : 1985-41 AGENCY : IOS, Tides & Currents, Sidney, B.C. COUNTRY : Canada PROJECT : Laperouse SCIENTIST : Crawford W. PLATFORM : Vector *LOCATION GEOGRAPHIC AREA : NE PACIFIC STATION : 19 EVENT NUMBER : 70 LATITUDE : 48 23.60000 N ! (deg min) LONGITUDE : 125 11.20000 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). References: Thomson,R.E., W.R. Crawford and W.S. Hugget. 1988. Water Property Observatio From The North Coast Oceanic Dynamics Experiment (NCODE): May 1983 to December 85 1980. Can. Data Rep. Hydrogr. Ocean Sci. 67: (Vol. 1 to 7). -------------------------------------------------------------------------- Some of the bottle samples from this cruise were originally archived as coming from cruise 1985-21, but they were actually collected during cruise 1985-41. Many of the dissolved oxygen samples were missing from the 1985-41 files, so the 2 sets were combined. In the course of the revision it was found that other bottle samples were missing from both sets, so those data were added which involved creating some new BOT files. For details on the revisions see file 1985-41-processing-revisions.doc. June 29, 2012 -------------------------------------------------------------------------- *HISTORY $TABLE: PROGRAMS ! Name Vers Date Time Recs In Recs Out ! -------- ------ ---------- -------- --------- --------- PADZEROS 1.0 1996/09/04 16:56:57 10 10 HDREDIT2 1.6 2003/07/02 17:25:33 ? ? CLEAN 4.3 2003/07/02 17:26:03 10 10 HDREDIT2 2.5.1 2012/06/29 17:37:19 ? ? HDREDIT2 3.2 2024/12/03 09:08:57 ? ? $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. -HEADER EDITS: 2012/06/29 17:37:19 Applied edit header: P:\Cruise_Data_Processing\1985\1985-41\DOC\1985-41-missing-bot2.txt -HEADER EDITS: 2024/12/03 09:08:57 Applied edit header: E:\Telework\1a-IOS_Tasks\Lu\1985-041\BOTTLE-old\1985-041-HDR.TXT $END !--1--- ---2--- !Depth Oxygen: ! Dissolv ! ed !------ ------- *END OF HEADER 0.0 5.964 10.0 3.858 20.0 3.394 30.0 3.077 50.0 2.405 75.0 1.931 100.0 1.863 125.0 1.719 150.0 1.670 172.0 1.570