data: max $partialdiff sub T$ $partialdiff sub X$ [ NOAA NCDC ERSST version3b sst climatology ]

max ∂_T ∂_X [ NOAA NCDC ERSST version3b sst climatology ] : ∂_T ∂_X Extended reconstructed sea surface temperature data

sst sst partial_X partial_T ∂_T ∂_X Extended reconstructed sea surface temperature from NOAA NCDC ERSST version3b: ERSST.v3b: Extended Reconstructed Sea Surface Temperature Dataset, Verson 3b.

Independent Variables (Grids)

Longitude (longitude): grid: /X (degree_east) periodic (1W) to (3W) by 2.0 N= 180 pts :grid
zlev: grid: /zlev (meters) ordered [ (0.0)] :grid

Other Info

CE

null

CS

null

datatype

realarraytype

iridl:hasSemantics

iridl:SeaSurfaceTemperature

missing_value

NaN

pointwidth

1.0

units

687.549354156988 degree_Kelvin radian^-1 east year^-1

history

$partialdiff sub T$ $partialdiff sub X$ [ NOAA NCDC ERSST version3b sst climatology ]

Version 3b
Averaged over T2[1854, 2024] minimum 0.0% data present

max $partialdiff sub T$ $partialdiff sub X$ [ NOAA NCDC ERSST version3b sst climatology ]

max over Y[88S, 88N] T[16 Dec - 15 Jan, 16 Nov - 15 Dec]

References

Smith_etal2008

Xue_etal2003

Last updated: Tue, 13 Aug 2024 08:17:43 GMT
Expires: Mon, 02 Sep 2024 00:00:00 GMT

Data Views

	X	zlev
max $partialdiff sub T$ $partialdiff sub X$ [ NOAA NCDC ERSST version3b sst climatology ] 0.0 meters[ X zlev \|]	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
Differentiate along X
Take differences along X