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

served from IRI/LDEO Climate Data Library

∫dT ∫dX ∂_T ∂_X [ IGOSS nmc Reyn_SmithOIv2 weekly sst ] : ∂_T ∂_X Sea Surface Temperature data

weekly sst partial_X partial_T int_dX int_dX ∂_T ∂_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 (julian_day) ordered [ (1200 8 Nov 1981 - 1200 15 Nov 1981) (1200 15 Nov 1981 - 1200 22 Nov 1981) (1200 22 Nov 1981 - 1200 29 Nov 1981) ... (1200 25 Jan 2023 - 1200 1 Feb 2023)] N= 2152 pts :grid
Longitude (longitude): grid: /X (degree_east) ordered (0.5W) to (0.5W) by 1.0 N= 361 pts :grid
Latitude (latitude): grid: /Y (degree_north) ordered (89.5S) to (89.5N) by 1.0 N= 180 pts :grid

Other Info

bufferwordsize: 8
CE: null
colorscalename: sstcolorscale
CS: null
datatype: doublearraytype
units: degree_Celsius
standard units*: degree_Kelvin

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

Data Views

	T	X	Y
$integral dT$ $integral dX$ $partialdiff sub T$ $partialdiff sub X$ [ IGOSS nmc Reyn_SmithOIv2 weekly 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