*2011/01/06 16:25:53.76
*IOS HEADER VERSION 1.8  2007/05/25 2007/05/25

*FILE
    START TIME          : UTC 1987/01/14 15:41:00.000
    NUMBER OF RECORDS   : 18
    DATA DESCRIPTION    : Bottle:Wire
    FILE TYPE           : ASCII
    NUMBER OF CHANNELS  : 5

    $TABLE: CHANNELS
    ! No Name                         Units     Minimum        Maximum
    !--- ---------------------------- --------- -------------- --------------
       1 Depth                        metres    0              1000
       2 Carbon:Dissolved:Inorganic   umol/kg   1986           2376
       3 Temperature:Reversing        'deg C'   3.59           9.83
       4 Salinity:Bottle              PSS-78    32.381         34.383
       5 Oxygen:Dissolved             umol/kg   18.3           291.1
    $END

    $TABLE: CHANNEL DETAIL
    ! No  Pad   Start  Width  Format  Type  Decimal_Places
    !---  ----  -----  -----  ------  ----  --------------
       1  -99   ' '    ' '    F7.1    R4    ' '
       2  -99   ' '    ' '    F7.1    R4    ' '
       3  -99   ' '    ' '    F7.2    R4    ' '
       4  -99   ' '    ' '    F8.3    R4    ' '
       5  -99   ' '    ' '    F7.2    R4    ' '
    $END

*ADMINISTRATION
    MISSION             : 1987-91
    AGENCY              : IOS, Ocean Physics Division, Sidney, B.C.
    COUNTRY             : Canada
    PROJECT             : Line P
    SCIENTIST           : Bellegay R.
    PLATFORM            : Endeavour

*LOCATION
    STATION             : MP03
    EVENT NUMBER        : 1
    LATITUDE            :  48  37.50000 N  ! (deg min)
    LONGITUDE           : 126  20.00000 W  ! (deg min)

*HISTORY

    $TABLE: PROGRAMS
    !   Name     Vers   Date       Time     Recs In   Recs Out
    !   -------- ------ ---------- -------- --------- ---------
        SPRD2IS  4.5    2011/01/06 16:24:00        18        18
        HDREDIT2 2.5.1  2011/01/06 16:25:53 ?         ?
    $END
    $REMARKS
        -HEADER EDITS: 2011/01/06 16:25:53
         Applied edit header: O:\Data Processing\Header Comments\Work\1987-91.TXT
    $END

*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 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 analyzed aboard ship by the use of a Technicon
        AutoAnalyzer using methods described in Barwell-Clarke and Whitney, 1996.

        Chlorophyll concentration was estimated from fluorescence of aqueous acetone
        extracts from filtered samples. Analysis methods generally followed those
        described in Parsons et al. 1972, however there have been various
        modifications of filtering and extraction protocols. Contact data
        originator(s) for details specific to individual time periods.

        For Productivity, POC and PON methods see file in directory
        \\OSD_Data_Archive\Cruise_Data\Documents\ProdChemistryMethods\

        Dissolved inorganic carbon (DIC) was determined using coulometric analysis.

        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. 1972. A Practical Handbook of
        Seawater Analysis. Bullettin 167 (2nd edition). Fisheries Research
        Board, Canada.
        3. J. Barwell-Clarke and F. Whitney. 1996. Institute of Ocean Sciences
        Nutrient Methods and Analysis. Canadian Technical Report of Hydrography
        and Ocean Sciences, No. 182, 43 pp.
!--1--- --2--- --3--- ---4--- --5---
!Depth  Carbon Temper Salinit Oxygen
!       :Disso ature: y:      :     
!       lved:  Revers Bottle  Dissol
!       Inorga ing            ved   
!       nic                         
!------ ------ ------ ------- ------
*END OF HEADER
    0.0 1990.0   9.76  32.381 287.90
   10.0 1986.0   9.79  32.384 288.80
   20.0 1986.0   9.78  32.381 288.80
   30.0 1988.0   9.80  32.395 291.10
   50.0 2054.0   9.83  32.825 233.50
   75.0 2093.0   9.72  33.126 205.40
  100.0 2123.0   9.36  33.384 184.80
  150.0 2166.0   8.86  33.722 149.60
  200.0 2199.0   8.38  33.870 111.20
  250.0 2194.0   7.87  33.948 110.70
  300.0 2223.0   7.06  33.986  96.40
  400.0 2262.0   6.02  34.046  69.60
  500.0 2294.0   5.30  34.078  43.30
  600.0 2319.0   4.74  34.162  26.80
  700.0 2326.0   4.39  34.229  21.40
  800.0 2363.0   4.03  34.281  18.30
  900.0 2370.0   3.78  34.340  25.00
 1000.0 2376.0   3.59  34.383  18.30