*2002/07/23 13:27:25.10 *IOS HEADER VERSION 1.3 1999/04/13 1999/12/09 *FILE START TIME : UTC 1984/08/22 03:42:00.000 NUMBER OF RECORDS : 21 DATA DESCRIPTION : Bottle:Wire FILE TYPE : ASCII DATA TYPE : REAL*4 PAD : -99 NUMBER OF CHANNELS : 5 $TABLE: CHANNELS ! No Name Units Minimum Maximum ! -- ----------------------- --------- -------------- -------------- 1 Depth metres 0 1960 2 Temperature:Reversing 'deg C' 1.93 15.94 3 Salinity:Bottle PSS-78 31.465 34.592 4 Oxygen:Dissolved mL/L 0.419 6.431 5 Oxygen:Dissolved umol/kg 18.2 280.4 $END $TABLE: CHANNEL DETAIL ! No Pad Start Width Format Type Decimal_Places ! -- ---- ----- ----- ------ ---- -------------- 1 ' ' ' ' 6 F ' ' 0 2 ' ' ' ' 7 F ' ' 2 3 ' ' ' ' 8 F ' ' 3 4 ' ' ' ' 8 F ' ' 3 5 -99 ' ' 6 F ' ' 1 $END $REMARKS This file converted from STDHYD file STDHYD84.DAT using SUStoIOS.BAS version 2.3 Sep 04/96 rmb Original HEADER: 84 2P0064844.60N12740.00W84 822 342GMT 9 4DTSO 1960 210.0H $END *ADMINISTRATION MISSION : 1984-02 AGENCY : IOS, Ocean Physics Division, Sidney, B.C. COUNTRY : Canada PROJECT : Line P SCIENTIST : Bellegay R. PLATFORM : Endeavour *LOCATION GEOGRAPHIC AREA : NE PACIFIC STATION : P006 EVENT NUMBER : 9 LATITUDE : 48 44.60000 N ! (deg min) LONGITUDE : 127 40.00000 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. *HISTORY $TABLE: PROGRAMS ! Name Vers Date Time Recs In Recs Out ! -------- ------ ---------- -------- --------- --------- PADZEROS 1.0 1996/09/04 16:55:07 21 21 CHGUNITS 1.3 2002/06/13 11:15:56 21 21 HDREDIT2 1.5 2002/07/23 13:27:19 ? ? CLEAN 3.7 2002/07/23 13:27:25 21 21 $END $REMARKS CHANGE units: - Units changed from ml/l to umol/kg 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--- ---4--- --5-- !Depth Temper Salinit Oxygen: Oxyge ! ature: y: Dissolv n: ! Revers Bottle ed Disso ! ing lved !----- ------ ------- ------- ----- *END OF HEADER 0. 15.94 31.465 5.909 257.9 10. 13.61 31.756 6.431 280.4 19. 10.71 32.128 5.607 244.3 29. 9.55 32.398 6.013 261.9 48. 8.75 32.519 5.837 254.2 72. 8.45 33.040 4.576 199.2 96. 8.04 33.463 3.689 160.5 120. 7.55 33.712 3.674 159.8 144. 7.26 33.832 3.728 162.1 168. 6.91 33.884 3.391 147.5 192. 6.65 33.917 3.367 146.4 240. 6.23 33.963 2.772 120.5 289. 5.79 33.978 2.128 92.5 386. 5.19 33.998 1.512 65.7 484. 4.76 34.074 0.917 39.9 582. 4.30 34.148 0.758 32.9 779. 3.77 34.289 0.509 22.1 977. 3.33 34.372 0.419 18.2 1175. 2.97 34.434 0.447 19.4 1472. 2.44 34.514 0.584 25.4 1960. 1.93 34.592 1.217 52.9