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

served from IRI/LDEO Climate Data Library

∂_X ∫dT [ IGOSS nmc Reyn_SmithOIv2 climatology c6190 sst ] : ∂_X Sea Surface Temperature data

climatology c6190 sst int_dT ∂_X Sea Surface Temperature 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 1 Jan 1960) to (0000 1 Jan 1961) by 1.0 N= 13 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 (89.5S) to (89.5N) by 1.0 N= 180 pts :grid

Other Info

CE: null
colorscalename: sstcolorscale
CS: null
datatype: realarraytype
file_missing_value: -999.90002
missing_value: NaN
units: 4.77464829275686 degree_Kelvin radian^-1 east year

References

Reynolds, R.W., N.A. Rayner, T.M. Smith, D.C. Stokes, and W. Wang, 2002: An Improved In Situ and Satellite SST Analysis for Climate. J. Climate, 15, 1609-1625.

Last updated: Thu, 14 Oct 2021 07:04:12 GMT

Data Views

	T	X	Y
$partialdiff sub X$ $integral dT$ [ IGOSS nmc Reyn_SmithOIv2 climatology c6190 sst ] [ 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