*2002/06/27 10:00:23.04 *IOS HEADER VERSION 1.3 1999/04/13 1999/12/09 *FILE START TIME : UTC 1982/01/20 09:00:00.000 NUMBER OF RECORDS : 6 DATA DESCRIPTION : Bottle:Wire FILE TYPE : ASCII DATA TYPE : REAL*4 PAD : -99 NUMBER OF CHANNELS : 3 $TABLE: CHANNELS ! No Name Units Minimum Maximum ! -- ----------------------- -------- -------------- -------------- 1 Depth metres 86 979 2 Temperature:Reversing 'deg C' 3.04 7.67 3 Salinity:Bottle ppt 32.456 34.38 $END $TABLE: CHANNEL DETAIL ! No Pad Start Width Format Type Decimal_Places ! -- ---- ----- ----- ------ ---- -------------- 1 ' ' ' ' 6 F ' ' 0 2 ' ' ' ' 7 F ' ' 2 3 ' ' ' ' 8 F ' ' 3 $END $REMARKS This file converted from STDHYD file STDHYD82.DAT using SUStoIOS.BAS version 2.3 Sep 04/96 rmb Original HEADER: 82 1P12 4856.00N13043.00W82 120 9 0GMT 16 3DTS 979 6 H $END *ADMINISTRATION MISSION : 1982-01 AGENCY : IOS, Offshore Oceanography, Sidney, B.C. COUNTRY : Canada PROJECT : Line P SCIENTIST : Tabata S. PLATFORM : Endeavour *LOCATION GEOGRAPHIC AREA : NE PACIFIC STATION : P12 EVENT NUMBER : 16 LATITUDE : 48 56.00000 N ! (deg min) LONGITUDE : 130 43.00000 W ! (deg min) *INSTRUMENT TYPE : Bottle MODEL : Niskin *COMMENTS Sample collection methods: -------------------------- Sea Water Temperature: - Reversing thermometers mounted on bottles. Salinity: - Collected in bottles. Dissolved Oxygen: - Collected in bottles. Reactive Nutrients (Phosphate, nitrate, silicate): - 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 300 m or greater. The accuracy of protected reversing thermometers is believed to be +-0.02C. Salinity determinations were made at sea with either a Guildline Autosal salinometer. Accuracy using duplicate determinations is estimated to be +-0.003 ppt. 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). Nutrient samples were frozen for analyzes ashore. Chlorophyll and nutrients were analyzed using methods from Bulletin 125 Fisheries Research Board of Canada 1960 "A manual of seawater analysis" J.D.H. Strickland and T.R. Parsons, and subsequent editions. References: 1. Carpenter, J.H. 1965. The Chesapeake Bay Institute Technique for the Winkler Dissolved Oxygen Method. Limmnol. & Oceanogr., 10: 141-143. 2. Strickland, J.D.H., and T.R. Parsons. 1968. A Practical Handbook of Seawater Analysis. Bullettin 167. Fisheries Research Board, Canada. 3. Strickland, J.D.H., and T.R. Parsons. 1972. A Practical Handbook of Seawater Analysis. Bullettin 167 (2nd edition). Fisheries Research Board, Canada. 4. S. Tabata and R. M. Brown. 1994. Hydrographic/CTD Observations Made During Ocean Climate Monitoring Study: 1981-1991 - A Summary of Operational Phase of Study. Canadian Data Report of Hydrography and Ocean Sciences, No. 136, 42 pp. *HISTORY $TABLE: PROGRAMS ! Name Vers Date Time Recs In Recs Out ! -------- ------ ---------- -------- --------- --------- PADZEROS 1.0 1996/09/04 16:47:38 6 6 CHGUNITS 1.3 2002/06/11 11:11:46 6 6 HDREDIT2 1.4 2002/06/11 11:14:26 ? ? CLEAN 3.8 2002/06/11 11:15:42 6 6 HDREDIT2 1.5 2002/06/27 10:00:23 ? ? $END $REMARKS CHANGE units: - No units changed CLEAN functions: - Reset #RECS, MIN & MAX values in header. - 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--- !Depth Temper Salinit ! ature: y: ! Revers Bottle ! ing !----- ------ ------- *END OF HEADER 86. 7.67 32.456 175. 6.29 33.724 354. 4.67 33.935 532. 4.11 34.063 711. 3.64 34.221 979. 3.04 34.380