*2003/07/02 14:22:23.28
*IOS HEADER VERSION 1.4  2002/12/04 2002/12/04

*FILE
    START TIME          : UTC 1985/07/09 11:36:00.000
    NUMBER OF RECORDS   : 18
    DATA DESCRIPTION    : Bottle:Wire
    FILE TYPE           : ASCII
    DATA TYPE           : REAL*4
    PAD                 : -99
    NUMBER OF CHANNELS  : 2

    $TABLE: CHANNELS
    ! No Name               Units    Minimum        Maximum
    ! -- ------------------ -------- -------------- --------------
       1 Depth              metres   0              1000
       2 Oxygen:Dissolved   mL/L     0.367          7.044
    $END

    $TABLE: CHANNEL DETAIL
    ! No  Pad   Start  Width  Format  Type  Decimal_Places
    ! --  ----  -----  -----  ------  ----  --------------
       1  -99   ' '        7  F       ' '     1
       2  -99   ' '        8  F       ' '     3
    $END
$REMARKS
       This file converted from STDHYD file STDHYD85.DAT
       using SUStoIOS.BAS version 2.3 Sep 04/96 rmb
  Original HEADER:
8510LB1448 8.50N126 0.00W85 7 91136GMT102             4DTSO        1000   180.0H
$END

*ADMINISTRATION
    MISSION             : 1985-10
    AGENCY              : IOS, Ocean Physics Division, Sidney, B.C.
    COUNTRY             : Canada
    PROJECT             : NCODE
    SCIENTIST           : Huggett S.
    PLATFORM            : Parizeau

*LOCATION
    GEOGRAPHIC AREA     : NE PACIFIC
    STATION             : LB14
    EVENT NUMBER        : 102
    LATITUDE            :  48   8.50000 N  ! (deg min)
    LONGITUDE           : 126   0.00000 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 16:57:25        18        18
        HDREDIT2 1.6    2003/07/02 14:21:57 ?         ?
        CLEAN    4.3    2003/07/02 14:22:23        18        18
    $END
    $REMARKS
        CLEAN functions:
         - Reset #RECS, MIN & MAX values in header.
         - Change Pad Value to -99 in All Channels.
         - Delete Empty Channels:   2 deleted.
         - Set channel name post-colon letters to upper case.
         - Set last  4 characters of file name to event
    $END
!--1--- ---2---
!Depth  Oxygen:
!       Dissolv
!       ed     
!------ -------
*END OF HEADER
    0.0   6.095
   10.0   6.215
   20.0   6.867
   30.0   7.044
   50.0   6.338
   75.0   5.426
  100.0   4.228
  125.0   3.557
  150.0   3.125
  175.0   3.047
  200.0   2.833
  250.0   2.459
  300.0   2.057
  400.0   1.207
  500.0   0.809
  600.0   0.591
  800.0   0.371
 1000.0   0.367