data: detrended-bfl root mean sq anom $integral dT$ $integral dX$ [ UEA CRU TS3p21 monthly tmx ]

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detrended-bfl root mean sq anom ∫dT ∫dX [ UEA CRU TS3p21 monthly tmx ] : near-surface temperature maximum data

detrended-bfl root mean sq anom ∫dT ∫dX [ UEA CRU TS3p21 monthly tmx ] .

Independent Variables (Grids)

Longitude (longitude): grid: /X (degree_east) ordered (180W) to (180) by 0.5 N= 721 pts :grid
Latitude (latitude): grid: /Y (degree_north) ordered (89.75S) to (89.75N) by 0.5 N= 360 pts :grid

Other Info

bufferwordsize

CE

null

correlation_decay_distance

1200.0

CS

null

datatype

doublearraytype

file_missing_value

9.96920997E36

missing_value

NaN

pointwidth

standard_name

air_temperature

units

0.00145444104332861 ( degree_Kelvin above 273.15 ) radian east year

history

detrended-bfl root mean sq anom $integral dT$ $integral dX$ [ UEA CRU TS3p21 monthly tmx ]

Wed 10 Jul 2013 18:28:10 BST : User ianharris : Program makegridsauto.for called by update.for
Averaged over T[0000 1 Jan 1901, 0000 1 Jan 2013] minimum 0.0% data present

References

Harris_etal2013

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

Data Views

	X	Y
detrended-bfl root mean sq anom $integral dT$ $integral dX$ [ UEA CRU TS3p21 monthly tmx ] [ X Y \|]	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
Differentiate along X Y
Take differences along X Y

Average over X Y | X Y |
RMS (root mean square with mean *not* removed) over X Y | X Y |
RMSA (root mean square with mean removed) over X Y | X Y |
Maximum over X Y | X Y |
Minimum over X Y | X Y |
Detrend (best-fit-line) over X Y | X Y |

Note on units