*2003/06/30 13:23:27.57 *IOS HEADER VERSION 1.4 2002/12/04 2002/12/04 *FILE START TIME : UTC 1983/07/12 17:06:00.000 NUMBER OF RECORDS : 14 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 1987 2 Temperature:Reversing 'deg C (IPTS68)' 1.95 14.4 3 Salinity:Bottle PSS-78 31.724 34.591 4 Oxygen:Dissolved mL/L 0.296 6.675 $END $TABLE: CHANNEL DETAIL ! No Pad Start Width Format Type Decimal_Places ! -- ---- ----- ----- ------ ---- -------------- 1 -99 ' ' 6 F ' ' 0 2 -99 ' ' 7 F ' ' 2 3 -99 ' ' 8 F ' ' 3 4 -99 ' ' 8 F ' ' 3 $END $REMARKS This file converted from STDHYD file STDHYD83.DAT using SUStoIOS.BAS version 2.3 Sep 04/96 rmb Original HEADER: 8311QC7553 1.50N13324.00W83 71217 6GMT 45 4DTSO 1987 140.0H $END *ADMINISTRATION MISSION : 1983-11 AGENCY : IOS, Offshore Oceanography, Sidney, B.C. COUNTRY : Canada PROJECT : NCODE SCIENTIST : Thomson R.E. PLATFORM : ENDEAVOUR *LOCATION GEOGRAPHIC AREA : NE PACIFIC STATION : QC75 EVENT NUMBER : 45 LATITUDE : 53 1.50000 N ! (deg min) LONGITUDE : 133 24.00000 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 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). *HISTORY $TABLE: PROGRAMS ! Name Vers Date Time Recs In Recs Out ! -------- ------ ---------- -------- --------- --------- PADZEROS 1.0 1996/09/04 16:50:25 14 14 HDREDIT2 1.6 2003/06/30 13:23:19 ? ? CLEAN 4.3 2003/06/30 13:23:27 14 14 $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. 14.40 31.724 6.138 20. 13.04 31.899 6.362 30. 11.55 32.062 6.675 49. 9.63 32.295 6.314 99. 7.54 32.598 6.001 148. 7.66 33.415 3.881 197. 6.96 33.782 3.134 296. 5.70 33.983 2.475 494. 4.59 34.057 1.063 792. 3.73 34.255 0.351 991. 3.37 34.367 0.296 1190. 2.88 34.415 0.374 1489. 2.43 34.495 0.655 1987. 1.95 34.591 1.376