served from IRI/LDEO Climate Data Library
NOAA NCDC ERSST version2 SST anomalies climatology: Sea Surface Temperature data
SST SST SST Sea Surface Temperature from NOAA NCDC ERSST version2: Improved extended reconstructed global sea surface temperature data based on COADS data.Independent Variables (Grids)
- Time (time)
- grid: /T (months since 01-Jan) periodic (16 Jan - 15 Feb) to (16 Dec - 15 Jan) by 1.0 N= 12 pts :grid
- Longitude (longitude)
- grid: /X (degree_east) periodic (0) to (2W) by 2.0 N= 180 pts :grid
- Latitude (latitude)
- grid: /Y (degree_north) ordered (88S) to (88N) by 2.0 N= 89 pts :grid
Other Info
- CE
- null
- CS
- null
- datatype
- realarraytype
- file_missing_value
- -9999
- missing_value
- NaN
- pointwidth
- 0
- units
- degree_Celsius
- standard units*
- degree_Kelvin
- history
- NOAA NCDC ERSST version2 SST anomalies climatology
- Averaged over T2[16 Jan 1854 - 15 Jan 1855, 16 Jan 2008 - 15 Jan 2009] minimum 0.0% data present
Averaged over T2[16 Jan 1854 - 15 Jan 1855, 16 Jan 2008 - 15 Jan 2009] minimum 0.0% data present
- Averaged over T2[16 Jan 1854 - 15 Jan 1855, 16 Jan 2008 - 15 Jan 2009] minimum 0.0% data present
References
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Data Views
Views
data as colors
data as contours
colors with land
contours with land
colors with coasts| T | X | Y | |
 NOAA NCDC ERSST version2 SST anomalies climatology[ Y X T |] | M | M | M |
|---|
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 Y X T
- Differentiate along Y X T
- Take differences along Y X T
RMS (root mean square with mean *not* removed) over Y X T | Y X Y T X T | Y X T |
RMSA (root mean square with mean removed) over Y X T | Y X Y T X T | Y X T |
Maximum over Y X T | Y X Y T X T | Y X T |
Minimum over Y X T | Y X Y T X T | Y X T |
Detrend (best-fit-line) over Y X T | Y X Y T X T | Y X T |
Note on units