data: $integral dX$ $partialdiff sub T$ [ NOAA NCEP EMC CMB GLOBAL Reyn

∫dX ∂_T [ NOAA NCEP EMC CMB GLOBAL Reyn_SmithOIv2 pentad-climatology sst ] : ∂_T Sea Surface Temperature data

pentad-climatology sst partial_T ∂_T Sea Surface Temperature from NOAA NCEP EMC CMB GLOBAL 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: grid: /T (pentads since 1960-01-01) periodic (1200 29 Dec - 1200 3 Jan) to (1200 24 Dec - 1200 29 Dec) by 1.0 N= 73 pts :grid
Longitude (longitude): grid: /X (degree_east) ordered (0) to (0) 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: 35
colorscalename: sstcolorscale
CS: -2
datatype: doublearraytype
file_missing_value: -999.90002
missing_value: NaN
units: 1.27409035395586 degree_Kelvin radian east year^-1
history: Averaged over T[Jan, Dec] minimum 0.0% data present
colorscale

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: Tue, 09 Jan 2018 17:35:48 GMT

Data Views

	T	X	Y
NOAA NCEP EMC CMB GLOBAL Reyn_SmithOIv2 pentad-climatology[sst ]
$integral dX$ $partialdiff sub T$ [ NOAA NCEP EMC CMB GLOBAL Reyn_SmithOIv2 pentad-climatology 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