data: $integral dT$ $partialdiff sub X$ $integral dT$ $partialdiff sub Y$ [ IGOSS nmc Reyn

served from IRI/LDEO Climate Data Library

∫dT ∂_X ∫dT ∂_Y [ IGOSS nmc Reyn_SmithOIv2 monthly ssta ] : ∂_X ∂_Y Sea Surface Temperature Anomaly data

monthly ssta partial_Y int_dT partial_X ∂_X ∂_Y Sea Surface Temperature Anomaly from IGOSS nmc Reyn_SmithOIv2: SST fields updated from version 1 with more COADS data, new sea-ice to SST conversion algorithm, and 1971-2000 climatology.

Independent Variables (Grids)

Time (time): grid: /T (months since 1960-01-01) ordered (0000 16 Oct 1981) to (0000 16 Feb 2023) by 1.0 N= 497 pts :grid
Longitude (longitude): grid: /X (degree_east) periodic (0) to (1W) by 1.0 N= 360 pts :grid
Latitude (latitude): grid: /Y (degree_north) ordered (89S) to (89N) by 1.0 N= 179 pts :grid

Other Info

bufferwordsize: 8
CE: null
colorscalename: sstacolorscale
CS: null
datatype: doublearraytype
maxncolor: 254
missing_value: NaN
pointwidth: 1.0
standard_name: sea_surface_temperature
units: 22.797266319526 degree_Kelvin radian^-2 north year²

References

Reynolds_etal2002

Last updated: Wed, 22 Mar 2023 18:04:31 GMT

Data Views

	T	X	Y
$integral dT$ $partialdiff sub X$ $integral dT$ $partialdiff sub Y$ [ IGOSS nmc Reyn_SmithOIv2 monthly ssta ] [ X Y \| 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 X Y T
Differentiate along X Y T
Take differences along X Y T