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∫dY [ MGAP CPT CrossValHind ]: cross-validated hindcasts data
MGAP CPT CrossValHind int_dY int_dY int_dY int_dY cross-validated hindcasts from SOURCES: datos de MGAP SNIA prueba.Independent Variables (Grids)
- L
- grid: /L (months) ordered (3.0 months) to (4.0 months) N= 2 pts :grid
- Time (time)
- grid: /T (days since 1960-01-01) ordered [ (16 Sep 1960 - 15 Oct 1960) (16 Oct 1960 - 15 Nov 1960)] :grid
- Training period
- grid: /T2 (months since 1960-01-01) ordered (1980) to (2011) by 12.0 N= 32 pts :grid
- Longitude (longitude)
- grid: /X (degree_east) ordered (59.75W) to (52.25W) by 0.5 N= 16 pts :grid
- Latitude (latitude)
- grid: /Y (degree_north) ordered (29.25S) to (35.75S) by 0.5 N= 14 pts :grid
Other Info
- CE
- null
- CS
- null
- datatype
- realarraytype
- file_missing_value
- -999.0
- missing_value
- NaN
- pointwidth
- 3.0
- units
- 0.00020943951023932 meter radian north year-1
- history
- Output from CPT for 12 3-month running seasons for 1960-2009 between ECHAM4p5 GCM and CRU dataset, CPT recompiled on Mac 9.04 version
Last updated: Thu, 04 Feb 2016 15:18:08 GMT
Data Views
Views
data as colors
data as contours
colors with land
contours with land
colors with coasts| L | T | T2 | X | Y | |
 $integral dY$ [ MGAP CPT CrossValHind ][ X Y T2 | T L] | M | M | 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 T2 T L
- Differentiate along X Y T2 T L
- Take differences along X Y T2 T L
RMS (root mean square with mean *not* removed) over X Y T2 T L | X Y X T2 X T X L Y T2 Y T Y L T2 T T2 L T L | X Y T2 X Y T X Y L X T2 T X T2 L X T L Y T2 T Y T2 L Y T L T2 T L | X Y T2 T X Y T2 L X Y T L X T2 T L Y T2 T L | X Y T2 T L |
RMSA (root mean square with mean removed) over X Y T2 T L | X Y X T2 X T X L Y T2 Y T Y L T2 T T2 L T L | X Y T2 X Y T X Y L X T2 T X T2 L X T L Y T2 T Y T2 L Y T L T2 T L | X Y T2 T X Y T2 L X Y T L X T2 T L Y T2 T L | X Y T2 T L |
Maximum over X Y T2 T L | X Y X T2 X T X L Y T2 Y T Y L T2 T T2 L T L | X Y T2 X Y T X Y L X T2 T X T2 L X T L Y T2 T Y T2 L Y T L T2 T L | X Y T2 T X Y T2 L X Y T L X T2 T L Y T2 T L | X Y T2 T L |
Minimum over X Y T2 T L | X Y X T2 X T X L Y T2 Y T Y L T2 T T2 L T L | X Y T2 X Y T X Y L X T2 T X T2 L X T L Y T2 T Y T2 L Y T L T2 T L | X Y T2 T X Y T2 L X Y T L X T2 T L Y T2 T L | X Y T2 T L |
Detrend (best-fit-line) over X Y T2 T L | X Y X T2 X T X L Y T2 Y T Y L T2 T T2 L T L | X Y T2 X Y T X Y L X T2 T X T2 L X T L Y T2 T Y T2 L Y T L T2 T L | X Y T2 T X Y T2 L X Y T L X T2 T L Y T2 T L | X Y T2 T L |
Note on units