served from dlibrary.snia.gub.uy
max [ T2 , max ( T , max { MGAP CPT InputObs } ) ]: T2, Time, input observations data
max [ T2 , max ( T , max { MGAP CPT InputObs } ) ].Independent Variables (Grids)
- Time (time)
- grid: /T (months since 01-Jan) ordered (Sep) to (Nov) by 1.0 N= 3 pts :grid
- T2
- grid: /T2 (months since 1960-01-01) ordered (Jul 1980 - Jun 1981) to (Jul 2010 - Jun 2011) by 12.0 N= 31 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
- calendar
- 360
- datatype
- realarraytype
- fnname
- max
- gridid
- 184886336
- missing_value
- NaN
- scale_max
- null
- scale_min
- null
- units
- months since 1960-01-01
- standard units*
- 0.0833333333333333 ( years since 1960-01-01 00:00.000000000 )
- history
- max [ MGAP CPT InputObs ]
- 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
max over L[2.5 months, 4.5 months]
- 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| T | T2 | X | Y | |
 MGAP CPT[PredErrorVars
Forecast
hindcast_date
InputObs
target_date
CrossValHind
PearsonR
CFSv2_AtlPac_sst
] | ||||
| grid: /X (degree_east) ordered (59.75W) to (52.25W) by 0.5 N= 16 pts :grid | M | |||
|---|---|---|---|---|
| grid: /Y (degree_north) ordered (29.5S) to (35.5S) by 0.5 N= 13 pts :grid | M | |||
 max [ T2 , max ( T , max { MGAP CPT InputObs } ) ][ | T2 T X Y] | 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 T2 T X Y
- Differentiate along T2 T X Y
- Take differences along T2 T X Y
RMS (root mean square with mean *not* removed) over T2 T X Y | T2 T T2 X T2 Y T X T Y X Y | T2 T X T2 T Y T2 X Y T X Y | T2 T X Y |
RMSA (root mean square with mean removed) over T2 T X Y | T2 T T2 X T2 Y T X T Y X Y | T2 T X T2 T Y T2 X Y T X Y | T2 T X Y |
Maximum over T2 T X Y | T2 T T2 X T2 Y T X T Y X Y | T2 T X T2 T Y T2 X Y T X Y | T2 T X Y |
Minimum over T2 T X Y | T2 T T2 X T2 Y T X T Y X Y | T2 T X T2 T Y T2 X Y T X Y | T2 T X Y |
Detrend (best-fit-line) over T2 T X Y | T2 T T2 X T2 Y T X T Y X Y | T2 T X T2 T Y T2 X Y T X Y | T2 T X Y |
Note on units