served from IRI/LDEO Climate Data Library
∂T ∫dX [ KAPLAN EXTENDED ssta ] : ∂T SST anomaly data
EXTENDED ssta int_dX int_dX ∂T SST anomaly from KAPLAN: Various datasets by Kaplan et. al.Independent Variables (Grids)
- Time
- grid: /T (months since 1960-01-01) ordered (16 Jan 1856 - 15 Feb 1856) to (16 Feb 2003 - 15 Mar 2003) by 1.0 N= 1766 pts :grid
- Longitude
- grid: /X (degree_east) ordered (27.5E) to (22.5E) by 5.0 N= 72 pts :grid
- Latitude
- grid: /Y (degree_north) ordered (87.5S) to (87.5N) by 5.0 N= 36 pts :grid
Other Info
- datatype
- realarraytype
- file_missing_value
- 1.00000002E30
- missing_value
- NaN
- units
- 0.20943951023932 degree_Kelvin radian east year-1
- history
- OS extended by NCEP
Last updated: Thu, 04 Nov 2021 17:46:15 GMT
Data Views
Views
data as colors
data as contours
colors with land
contours with land
colors with coasts| T | X | Y | |
 $partialdiff sub T$ $integral dX$ [ KAPLAN EXTENDED ssta ] [ X Y | T] | M | M | M |
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Filters
Here are some filters that are useful for manipulating data. There are actually many more available, but they have to be entered manually. See Ingrid Function Documentation for more information.- Monthly Climatology calculates a monthly climatology by averaging over all years.
- anomalies calculates the difference between the (above) monthly climatology and the original data.
- Integrate along X Y T
- Differentiate along X Y T
- Take differences along X Y T
RMS (root mean square with mean *not* removed) over X Y T | X Y X T Y T | X Y T |
RMSA (root mean square with mean removed) over X Y T | X Y X T Y T | X Y T |
Maximum over X Y T | X Y X T Y T | X Y T |
Minimum over X Y T | X Y X T Y T | X Y T |
Detrend (best-fit-line) over X Y T | X Y X T Y T | X Y T |
Note on units