data: detrended-bfl detrended-bfl $integral dT$ $partialdiff sub Y$ [ UEA CRU TS3p21 monthly tmx ]

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detrended-bfl detrended-bfl ∫dT ∂_Y [ UEA CRU TS3p21 monthly tmx ] : ∂_Y near-surface temperature maximum data

detrended-bfl detrended-bfl ∫dT ∂_Y [ UEA CRU TS3p21 monthly tmx ] .

Independent Variables (Grids)

Time (time): grid: /T (months since 1960-01-01) ordered (0000 1 Jan 1901) to (0000 1 Jan 2013) by 1.0 N= 1345 pts :grid
Longitude (longitude): grid: /X (degree_east) periodic (179.75W) to (179.75E) 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

bufferwordsize: 8
CE: null
correlation_decay_distance: 1200.0
CS: null
datatype: doublearraytype
file_missing_value: 9.96920997E36
missing_value: NaN
pointwidth: 1
standard_name: air_temperature
units: 4.77464829275686 degree_Kelvin radian^-1 north year
history: Wed 10 Jul 2013 18:28:10 BST : User ianharris : Program makegridsauto.for called by update.for

References

Harris_etal2013

Last updated: Fri, 26 Jul 2024 12:21:16 GMT

Data Views

	T	X	Y
detrended-bfl detrended-bfl $integral dT$ $partialdiff sub Y$ [ UEA CRU TS3p21 monthly tmx ] [ 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