*2003/06/30 16:59:51.31
*IOS HEADER VERSION 1.4  2002/12/04 2002/12/04

*FILE
    START TIME          : UTC 1983/09/13 00:18:00.000
    NUMBER OF RECORDS   : 10
    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              1200
       2 Salinity:Bottle    PSS-78   31.798         34.427
       3 Oxygen:Dissolved   mL/L     0.366          6.1
    $END

    $TABLE: CHANNEL DETAIL
    ! No  Pad   Start  Width  Format  Type  Decimal_Places
    ! --  ----  -----  -----  ------  ----  --------------
       1  -99   ' '        7  F       ' '     1
       2  -99   ' '        8  F       ' '     3
       3  -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:
8312QC165240.30N13243.50W83 913 018GMT 52             4DTSO        1200   100.0H
$END

*ADMINISTRATION
    MISSION             : 1983-12
    AGENCY              : IOS, Offshore Oceanography, Sidney, B.C.
    COUNTRY             : Canada
    PROJECT             : NCODE
    SCIENTIST           : Huggett S.
    PLATFORM            : Parizeau

*LOCATION
    GEOGRAPHIC AREA     : NE PACIFIC
    STATION             : QC16
    EVENT NUMBER        : 52
    LATITUDE            :  52  40.30000 N  ! (deg min)
    LONGITUDE           : 132  43.50000 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 16:51:03        10        10
        HDREDIT2 1.6    2003/06/30 16:59:39 ?         ?
        CLEAN    4.3    2003/06/30 16:59:51        10        10
    $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  Salinit Oxygen:
!       y:      Dissolv
!       Bottle  ed     
!------ ------- -------
*END OF HEADER
    0.0  31.798   6.100
   10.0  31.947   6.045
   30.0  31.968   5.906
   50.0  32.287   5.536
  100.0  32.757   5.102
  200.0  33.798   3.512
  400.0  33.977   1.487
  600.0  34.130   0.613
  800.0  34.257   0.366
 1200.0  34.427   0.428