data: $integral dT$ $integral dY$ $integral dX$ [ CMC FCLIMDEX R50 ]

served from 129.236.110.25

∫dT ∫dY ∫dX [ CMC FCLIMDEX R50 ] : FCLIMDEX R50 data

∫dT ∫dY ∫dX [ CMC FCLIMDEX R50 ] .

Independent Variables (Grids)

Time (time): grid: /T (months since 0000-01-01) ordered (0000 1 Jul 0014BC) to (0000 1 Jul 0046) by 12.0 N= 60 pts :grid
Longitude (longitude): grid: /X (degree_east) ordered (74W) to (58.5W) by 0.96875 N= 17 pts :grid
Latitude (latitude): grid: /Y (degree_north) ordered (14.5N) to (0.5S) by 1.0 N= 16 pts :grid

Other Info

bufferwordsize: 8
CE: null
Conventions: COARDS
CS: null
datatype: doublearraytype
units: 2.53847849822257×10^-05 radian² north year

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		M
grid: /Y (degree_north) ordered (14N) to (0) by 1.0 N= 15 pts :grid			O=0.5
grid: /T (months since 0000-01-01) periodic (Jul 0014BC - Jun 0013BC) to (Jul 0045 - Jun 0046) by 12.0 N= 59 pts :grid	O=-6.0
$integral dT$ $integral dY$ $integral dX$ [ 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