*2003/06/30 17:22:09.54
*IOS HEADER VERSION 1.4  2002/12/04 2002/12/04

*FILE
    START TIME          : UTC 1984/06/24 22:12:00.000
    NUMBER OF RECORDS   : 9
    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           0              200
       2 Temperature:Reversing   'deg C (IPTS68)' 6.26           6.26
       3 Oxygen:Dissolved        mL/L             2.413          7.211
    $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
    $END
$REMARKS
       This file converted from STDHYD file STDHYD84.DAT
       using SUStoIOS.BAS version 2.3 Sep 04/96 rmb
  Original HEADER:
8412G00549 7.50N12655.20W84 6242212GMT 66             4DTSO         200    90.0H
$END

*ADMINISTRATION
    MISSION             : 1984-12
    AGENCY              : IOS, Offshore Oceanography, Sidney, B.C.
    COUNTRY             : Canada
    PROJECT             : CCEXP
    SCIENTIST           : Thomson R.E.
    PLATFORM            : Parizeau

*LOCATION
    GEOGRAPHIC AREA     : NE PACIFIC
    STATION             : G005
    EVENT NUMBER        : 66
    LATITUDE            :  49   7.50000 N  ! (deg min)
    LONGITUDE           : 126  55.20000 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 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., B.M. Hickey and P.H. LeBlond. 1986. Water Property Observation
    from the Vancouver Island Coastal Current Experiment: June, July and October
    1984. Can. Data Rep. Hydrogr. Ocean Sci. 46: 505p.

*HISTORY

    $TABLE: PROGRAMS
    !   Name     Vers   Date       Time     Recs In   Recs Out
    !   -------- ------ ---------- -------- --------- ---------
        PADZEROS 1.0    1996/09/04 16:52:51         9         9
        HDREDIT2 1.6    2003/06/30 17:22:00 ?         ?
        CLEAN    4.3    2003/06/30 17:22:09         9         9
    $END
    $REMARKS
        CLEAN functions:
         - Reset #RECS, MIN & MAX values in header.
         - Change Pad Value to -99 in All Channels.
         - Delete Empty Channels:   1 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 Oxygen:
!       ature: Dissolv
!       Revers ed     
!       ing           
!------ ------ -------
*END OF HEADER
    0.0 -99.00   7.211
   10.0 -99.00   7.167
   20.0 -99.00   6.632
   30.0 -99.00   6.431
   50.0 -99.00   5.399
   75.0 -99.00   4.694
  100.0 -99.00   3.580
  125.0 -99.00   3.366
  200.0   6.26   2.413