*2003/06/30 17:05:01.79 *IOS HEADER VERSION 1.4 2002/12/04 2002/12/04 *FILE START TIME : UTC 1984/04/25 06:06:00.000 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 0 350 2 Temperature:Reversing 'deg C (IPTS68)' 5.11 8.5 3 Salinity:Bottle PSS-78 31.957 33.982 4 Oxygen:Dissolved mL/L 1.874 6.995 $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 STDHYD84.DAT using SUStoIOS.BAS version 2.3 Sep 04/96 rmb Original HEADER: 8411J00152 0.00N13114.00W84 425 6 6GMT125 4DTSO 350 140.0H $END *ADMINISTRATION MISSION : 1984-11 AGENCY : IOS, Offshore Oceanography, Sidney, B.C. COUNTRY : Canada PROJECT : NCODE SCIENTIST : Huggett S. PLATFORM : Parizeau *LOCATION GEOGRAPHIC AREA : NE PACIFIC STATION : J001 EVENT NUMBER : 125 LATITUDE : 52 0.00000 N ! (deg min) LONGITUDE : 131 14.00000 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 16:51:57 14 14 HDREDIT2 1.6 2003/06/30 17:04:55 ? ? CLEAN 4.3 2003/06/30 17:05:01 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 0.0 8.50 31.960 6.906 10.0 8.50 31.957 6.995 20.0 8.20 32.004 6.835 30.0 8.14 32.022 6.895 51.0 8.11 32.029 6.795 76.0 8.09 32.040 6.746 101.0 8.06 32.161 6.632 125.0 7.88 32.477 6.050 150.0 7.56 33.015 4.863 175.0 7.18 33.384 3.904 199.0 6.35 33.670 3.030 249.0 5.88 33.826 2.600 299.0 5.54 33.915 2.106 350.0 5.11 33.982 1.874