data: $integral dY$ max detrended-bfl [ OLE2 CAM3p1 HINDCAST OBS PRECT ]

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∫dY max detrended-bfl [ OLE2 CAM3p1 HINDCAST OBS PRECT ] : Total (convective and large-scale) precipitation rate data

∫dY max detrended-bfl [ OLE2 CAM3p1 HINDCAST OBS PRECT ] .

Independent Variables (Grids)

member: grid: /M (unitless) ordered (1.0) to (9.0) by 1.0 N= 9 pts :grid
Time (time): grid: /T (months since 1960-01-01) ordered (Jan 1971) to (Dec 2010) by 1.0 N= 480 pts :grid
Latitude (latitude): grid: /Y (degree_north) ordered (89.25765S) to (89.25765N) by 2.789302 N= 65 pts :grid

Other Info

bufferwordsize: 8
CE: null
CS: null
datatype: doublearraytype
pointwidth: 1.0
units: 2.02005700462307×10^-10 meter radian north second^-1
history: max over X[0, 2.8125W]

Last updated: Fri, 17 Jun 2016 14:57:32 GMT

Data Views

	M	T	Y
grid: /X (degree_east) periodic (0) to (2.8125W) by 2.8125 N= 128 pts :grid
grid: /Y (degree_north) ordered (87.863S) to (87.863N) by 2.789302 N= 64 pts :grid			O=-1.394648
grid: /M (unitless) ordered (1.0) to (9.0) by 1.0 N= 9 pts :grid	M
grid: /T (months since 1960-01-01) ordered (Jan 1971) to (Dec 2010) by 1.0 N= 480 pts :grid		M
$integral dY$ max detrended-bfl [ OLE2 CAM3p1 HINDCAST OBS PRECT ] [ Y \| M 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 Y M T
Differentiate along Y M T
Take differences along Y M T