data: $partialdiff sub T$ $partialdiff sub X$ [ NOAA NCDC ERSST version4 sst ]

served from IRI/LDEO Climate Data Library

∂_T ∂_X [ NOAA NCDC ERSST version4 sst ] : ∂_T ∂_X Extended reconstructed sea surface temperature data

sst partial_X partial_T ∂_T ∂_X Extended reconstructed sea surface temperature from NOAA NCDC ERSST version4: In situ data: ICOADS2.5 before 2007, NCEP in situ data from 2008 to present. Ice data: HadISST ice before 2015 and NCEP ice after 2015..

Independent Variables (Grids)

Time (time): grid: /T (months since 1960-01-01) ordered (Feb 1854) to (Jan 2020) by 1.0 N= 1992 pts :grid
Longitude (longitude): grid: /X (degree_east) periodic (1W) to (3W) 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: realarraytype
file_missing_value: -999.0
iridl:hasSemantics: iridl:SeaSurfaceTemperature
missing_value: NaN
pointwidth: 1.0
standard_name: sea_surface_temperature
units: 687.549354156988 degree_Kelvin radian^-1 east year^-1

References

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Liu_etal2015

Last updated: Tue, 26 May 2020 18:41:27 GMT

Data Views

	T	X	Y	zlev
$partialdiff sub T$ $partialdiff sub X$ [ NOAA NCDC ERSST version4 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