data: $partialdiff sub X$ [ $partialdiff sub X$ ( NOAA NCEP EMC CMB GLOBAL Reyn

∂_X [ ∂_X ( NOAA NCEP EMC CMB GLOBAL Reyn_SmithOIv2 monthly sst ) climatology ]: ∂_X ∂_X Sea Surface Temperature data

monthly sst partial_X partial_X ∂_X ∂_X 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 (time): grid: /T (months since 01-Jan) periodic (Nov) to (Oct) by 1.0 N= 12 pts :grid
Longitude (longitude): grid: /X (degree_east) periodic (0.5W) to (1.5W) 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: 3282.80635001174 degree_Kelvin radian^-2 east
history: Averaged over T2[Nov 1981 - Oct 1982, Nov 2009 - Oct 2010] minimum 0.0% data present

References

Reynolds_etal2002

Last updated: Tue, 15 Aug 2017 14:04:01 GMT
Expires: Mon, 07 Feb 2011 00:00:00 GMT

Data Views

	T	X	Y
$partialdiff sub X$ [ $partialdiff sub X$ ( NOAA NCEP EMC CMB GLOBAL Reyn_SmithOIv2 monthly sst ) climatology ][ 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