data: $integral dX$ [ UEA CRU Jones CRUTEM4p2p0p0 station

served from IRI/LDEO Climate Data Library

∫dX [ UEA CRU Jones CRUTEM4p2p0p0 station_error ]: Station Error data

station_error Station Error from UEA CRU Jones CRUTEM4p2p0p0: Land air temperature anomalies.

Independent Variables (Grids)

Time (time): grid: /T (months since 1960-01-01) ordered (Jan 1850) to (Jul 2014) by 1.0 N= 1975 pts :grid
Longitude (longitude): grid: /X (degree_east) ordered (180W) to (180) by 5.0 N= 73 pts :grid
latitude (latitude): grid: /Y (degree_north) ordered (87.5S) to (87.5N) by 5.0 N= 36 pts :grid

Other Info

bufferwordsize: 8
datatype: doublearraytype
file_missing_value: -1.00000002E30
missing_value: NaN
reference_period: [ 1961 1990 ]
units: 0.0174532925199433 ( degree_Kelvin above 0 ) radian east

References

Jones, P. D., D. H. Lister, T. J. Osborn, C. Harpham, M. Salmon, and C. P. Morice (2012), Hemispheric and large-scale land-surface air temperature variations: An extensive revision and an update to 2010, J. Geophys. Res., 117, D05127, doi:10.1029/2011JD017139.

Brohan, P., J. J. Kennedy, I. Harris, S. F. B. Tett, and P. D. Jones (2006), Uncertainty estimates in regional and global observed temperature changes: A new data set from 1850, J. Geophys. Res., 111, D12106, doi:10.1029/2005JD006548.

Last updated: Wed, 13 Feb 2019 20:27:28 GMT

Data Views

	T	X	Y
$integral dX$ [ UEA CRU Jones CRUTEM4p2p0p0 station_error ][ 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