*2003/06/30 16:57:42.60 *IOS HEADER VERSION 1.4 2002/12/04 2002/12/04 *FILE START TIME : UTC 1983/05/17 14:18:00.000 NUMBER OF RECORDS : 20 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 1447 2 Temperature:Reversing 'deg C (IPTS68)' 2.45 11.31 3 Salinity:Bottle PSS-78 31.619 34.498 4 Oxygen:Dissolved mL/L 0.359 6.772 $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 STDHYD83.DAT using SUStoIOS.BAS version 2.3 Sep 04/96 rmb Original HEADER: 8310H05 5038.00N131 8.30W83 5171418GMT165 4DTSO 1447 200.0H $END *ADMINISTRATION MISSION : 1983-10 AGENCY : IOS, Offshore Oceanography, Sidney, B.C. COUNTRY : Canada PROJECT : NCODE SCIENTIST : Huggett S. PLATFORM : Parizeau *LOCATION GEOGRAPHIC AREA : NE PACIFIC STATION : H05 EVENT NUMBER : 165 LATITUDE : 50 38.00000 N ! (deg min) LONGITUDE : 131 8.30000 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 16:50:04 20 20 HDREDIT2 1.6 2003/06/30 16:57:19 ? ? CLEAN 4.3 2003/06/30 16:57:42 20 20 $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 11.31 31.629 6.341 10.0 11.29 31.621 6.577 20.0 11.28 31.619 6.588 30.0 10.79 32.001 6.664 50.0 9.70 32.433 6.645 75.0 8.25 32.460 6.772 99.0 7.68 32.485 6.645 124.0 7.53 32.793 5.765 148.0 7.78 33.308 4.188 173.0 7.38 33.625 3.472 197.0 7.18 33.766 3.328 246.0 6.53 33.897 2.924 294.0 6.06 33.943 2.452 391.0 4.97 34.006 1.445 486.0 4.52 34.076 1.050 581.0 4.18 34.151 0.668 771.0 3.66 34.282 0.454 961.0 3.29 34.360 0.359 1153.0 2.90 34.431 0.470 1447.0 2.45 34.498 0.755