data: detrended-bfl $integral dX$ [ CMC FCLIMDEX R50 ]

served from 129.236.110.25

detrended-bfl ∫dX [ CMC FCLIMDEX R50 ] : FCLIMDEX R50 data

detrended-bfl ∫dX [ CMC FCLIMDEX R50 ] .

Independent Variables (Grids)

Time (time): grid: /T (months since 1960-01-01) periodic (Jul 1947 - Jun 1948) to (Jul 2005 - Jun 2006) by 12.0 N= 59 pts :grid
Longitude (longitude): grid: /X (degree_east) ordered (74.48438W) to (58.01562W) by 0.96875 N= 18 pts :grid
Latitude (latitude): grid: /Y (degree_north) ordered (13.5N) to (0.5N) by 1.0 N= 14 pts :grid

Other Info

CE: null
CS: null
datatype: realarraytype
units: degree_east
standard units*: 0.0174532925199433 radian east

Last updated: Tue, 10 Apr 2018 00:04:26 GMT

Data Views

	T	X	Y
CMC FCLIMDEX[R95p R99p tx90p PRCPT R10 tn10p R20 R50 tn90p tx10p ]
grid: /X (degree_east) ordered (74W) to (58.5W) by 0.96875 N= 17 pts :grid		O=-0.484375
grid: /Y (degree_north) ordered (14N) to (0) by 1.0 N= 15 pts :grid			O=-0.5
grid: /T (months since 1960-01-01) periodic (Jul 1947 - Jun 1948) to (Jul 2005 - Jun 2006) by 12.0 N= 59 pts :grid	M
detrended-bfl $integral dX$ [ CMC FCLIMDEX R50 ] [ 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