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NOAA NCDC ERSST version3b sst: Extended reconstructed sea surface temperature data
Extended reconstructed sea surface temperature from NOAA NCDC ERSST version3b: ERSST.v3b: Extended Reconstructed Sea Surface Temperature Dataset, Verson 3b.Independent Variables (Grids)
- Time (time)
- grid: /T (months since 1960-01-01) ordered (Jan 1854) to (Oct 2017) by 1.0 N= 1966 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
- zlev
- grid: /zlev (meters) ordered [ (0.0)] :grid
Other Info
- datatype
- shortarraytype
- iridl:hasSemantics
- iridl:SeaSurfaceTemperature
- missing_value
- -999
- pointwidth
- 1.0
- scale_factor
- 0.01
- units
- degree_Celsius
- valid_max
- 4500
- valid_min
- -300
- standard units*
- degree_Kelvin
- history
- Version 3b
References
Smith_etal2008Xue_etal2003
Last updated: Wed, 20 Mar 2019 09:34:10 GMT
Expires: Tue, 02 Oct 2018 00:00:00 GMT
Data Views
Views
data as colors
data as contours
colors with land
contours with land
colors with coasts| T | X | Y | zlev | |
 NOAA NCDC ERSST version3b[sst
err
anom
] | ||||
| NOAA NCDC ERSST version3b anom 0.0 meters[ X Y zlev | T] | M | M | M | M |
|---|---|---|---|---|
 NOAA NCDC ERSST version3b sst 0.0 meters[ X Y zlev | T] | M | 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 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