served from dlibrary.snia.gub.uy
∂T2 ∫dL ∂L [ MGAP CPT InputObs ] : ∂T2 ∂L input observations data
MGAP CPT InputObs partial_L partial_L int_dL int_dL partial_T2 partial_T2 ∂T2 ∂L input observations 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 (months since 1960-01-01) ordered (16 Sep 1960 - 15 Oct 1960) to (16 Oct 1960 - 15 Nov 1960) N= 2 pts :grid
- T2
- grid: /T2 (months since 1960-01-01) ordered (1981) to (2010) by 12.0 N= 30 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 (29.5S) to (35.5S) by 0.5 N= 13 pts :grid
Other Info
- CE
- null
- CS
- null
- datatype
- realarraytype
- file_missing_value
- -999.0
- missing_value
- NaN
- pointwidth
- 3.0
- units
- 0.144 meter year-2
- 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 | |
 $partialdiff sub T2$ $integral dL$ $partialdiff sub L$ [ MGAP CPT InputObs ] [ 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