data: $partialdiff sub Y$ $partialdiff sub T$ [ NOAA NCDC ERSST version3b sst ]

∂_Y ∂_T [ NOAA NCDC ERSST version3b sst ] : ∂_Y ∂_T Extended reconstructed sea surface temperature data

sst partial_T partial_Y ∂_Y ∂_T 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 (Feb 1854) to (Oct 2025) by 1.0 N= 2061 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 (87S) to (87N) by 2.0 N= 88 pts :grid
zlev: grid: /zlev (meters) ordered [ (0.0)] :grid

Other Info

datatype: realarraytype
iridl:hasSemantics: iridl:SeaSurfaceTemperature
missing_value: NaN
pointwidth: 1.0
units: 687.549354156988 degree_Kelvin radian^-1 north year^-1
history: Version 3b

References

Smith_etal2008

Xue_etal2003

Last updated: Tue, 13 Aug 2024 08:17:43 GMT
Expires: Mon, 02 Sep 2024 00:00:00 GMT

Data Views

	T	X	Y	zlev
$partialdiff sub Y$ $partialdiff sub T$ [ 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