| 3-month halosteric sea level anomaly from 2005 to present |
|
| - Atlantic: |
0 - 700,
0 - 2000 meters (Jan-Mar)
0 - 700,
0 - 2000 meters (Apr-Jun)
0 - 700,
0 - 2000 meters (Jul-Sep)
0 - 700,
0 - 2000 meters (Oct-Dec)
|
| - Indian: |
0 - 700,
0 - 2000 meters (Jan-Mar)
0 - 700,
0 - 2000 meters (Apr-Jun)
0 - 700,
0 - 2000 meters (Jul-Sep)
0 - 700,
0 - 2000 meters (Oct-Dec)
|
| - Pacific: |
0 - 700,
0 - 2000 meters (Jan-Mar)
0 - 700,
0 - 2000 meters (Apr-Jun)
0 - 700,
0 - 2000 meters (Jul-Sep)
0 - 700,
0 - 2000 meters (Oct-Dec)
|
| - World: |
0 - 700,
0 - 2000 meters (Jan-Mar)
0 - 700,
0 - 2000 meters (Apr-Jun)
0 - 700,
0 - 2000 meters (Jul-Sep)
0 - 700,
0 - 2000 meters (Oct-Dec)
0 - 700,
0 - 2000
all months
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FILE NAMING CONVENTIONS:
b-mm-[Y]0-[Z]m[X1-X2].dat
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| | | | | | the filename extension
| | | | | the 3-month period, where: '1-3' for Jan-Mar, '4-6' for Apr-Jun,
| | | | | '7-9' for Jul-Sep, '10-12' for Oct-Dec
| | | | the label refering to depth in meters
| | | the lower depth of integration ('700')
| | the upper depth of integration ('0' stands for the sea surface)
| ocean basins: w - World, p - Pacific, a - Atlantic, i - Indian
the label for sea level
For example, file 'b-w0-700m1-3.dat' contains the time series of ocean 3-month (Jan-Mar)
heat content of the 0-700 m layer for the World Ocean
|
HALOSTERIC SEA LEVEL ANOMALY (HSLA) UNITS: mm
DATA FORMAT:
Data in each file is organized in column form:
each column corresponds to the time series for ocean basins as outlined below.
1st column - year+0.5 (for the yearly heat content) ;
2nd column - time series of HSLA of OB;
3rd column - time series of the standard error of HSLA of OB;
4th column - time series of HSLA of NHPB;
5th column - time series of the standard error of HSLA of NHPB;
6th column - time series of HSLA of SHPB;
7th column - time series of the standard error of HSLA of SHPB.
The first line of file contains the labels for each of 7 columns.
Read the second line through the last line using an equivalent of the FORTRAN FORMAT
(F8.1, 6F8.3) statement.
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