data: detrended-bfl [ UEA CRU TS2p1 monthly mean temp ]

detrended-bfl [ UEA CRU TS2p1 monthly mean temp ]: temperature data

monthly mean temp temperature from UEA CRU TS2p1: Mean surface climate data over global land areas, including tercile and percentile data.

Independent Variables (Grids)

Time (time): grid: /T (months since 1960-01-01) ordered (Jan 1901) to (Dec 2002) by 1.0 N= 1224 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 (89.75S) to (89.75N) by 0.5 N= 360 pts :grid

Other Info

bufferwordsize: 8
CE: null
CS: null
datatype: doublearraytype
missing_value: NaN
units: degree_Celsius
standard units*: degree_Kelvin

References

Mitchell, T. D., P. D. Jones. An improved method of constructing a database of monthly climate observations and associated high-resolution grids. Int. J. Climatol. 25, 2005

Last updated: Tue, 15 Aug 2017 14:04:01 GMT

Data Views

	T	X	Y
UEA CRU TS2p1 monthly[maximum vap elev prcp mean minimum ]
grid: /X (degree_east) periodic (179.75W) to (179.75E) by 0.5 N= 720 pts :grid		M
grid: /Y (degree_north) ordered (89.75S) to (89.75N) by 0.5 N= 360 pts :grid			M
grid: /T (months since 1960-01-01) ordered (Jan 1901) to (Dec 2002) by 1.0 N= 1224 pts :grid	M
detrended-bfl [ UEA CRU TS2p1 monthly mean temp ][ 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