data: $partialdiff sub Y$ [ $integral dT$ $partialdiff sub X$ ( UEA CRU TS3p21 monthly st0 dtr ) climatology ]

served from 213.55.84.78

∂_Y [ ∫dT ∂_X ( UEA CRU TS3p21 monthly st0 dtr ) climatology ]: ∂_Y ∂_X in-cell station count for dtr data

∂_Y [ ∫dT ∂_X ( UEA CRU TS3p21 monthly st0 dtr ) climatology ].

Independent Variables (Grids)

Time (time): grid: /T (months since 01-Jan) periodic (0000 1 Jan) to (0000 1 Dec) by 1.0 N= 12 pts :grid
Longitude (longitude): grid: /X (degree_east) periodic (180W) to (179.5E) by 0.5 N= 720 pts :grid
Latitude (latitude): grid: /Y (degree_north) ordered (89.5S) to (89.5N) by 0.5 N= 359 pts :grid

Other Info

CE

null

CS

null

datatype

realarraytype

file_missing_value

9.96920997E36

missing_value

NaN

pointwidth

units

number /degree_east months /degree_north

history

$partialdiff sub Y$ [ $integral dT$ $partialdiff sub X$ ( UEA CRU TS3p21 monthly st0 dtr ) climatology ]

Wed 10 Jul 2013 18:28:10 BST : User ianharris : Program makegridsauto.for called by update.for
Averaged over T2[16 Dec 1900 - 15 Dec 1901, 16 Dec 2011 - 15 Dec 2012] minimum 0.0% data present

References

Harris_etal2013

Last updated: Wed, 01 Feb 2023 14:07:40 GMT

Data Views

	T	X	Y
$partialdiff sub Y$ [ $integral dT$ $partialdiff sub X$ ( UEA CRU TS3p21 monthly st0 dtr ) 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