served from IRI/LDEO Climate Data Library
IRI FD CPT Monsoon_Asia temperature maximum InputObs: input observations data
Monsoon_Asia temperature maximum input observations from IRI FD CPT: Climate Prediction Tool.Independent Variables (Grids)
- Forecast Lead Time in Months
- grid: /L (months) ordered (2.5 months) to (5.5 months) by 1.0 N= 4 pts :grid
- Time (time)
- grid: /T (months since 01-Jan) periodic (Jan) to (Dec) by 1.0 N= 12 pts :grid
- Training period
- grid: /T2 (months since 1960-01-01) ordered (1979) to (2008) by 12.0 N= 30 pts :grid
- Longitude (longitude)
- grid: /X (degree_east) ordered (70.25E) to (99.75E) by 0.5 N= 60 pts :grid
- Latitude (latitude)
- grid: /Y (degree_north) ordered (20.25N) to (35.75N) by 0.5 N= 32 pts :grid
Other Info
- bufferwordsize
- 4
- datatype
- realarraytype
- missing_value
- -999.0
- pointwidth
- 1.0
- units
- Celsius_scale
- standard units*
- degree_Kelvin above 273.15
- history
- Output from CPT for 12 3-month running seasons for 1979-2008 with UEA CRU TS3p1 monthly dataset, CPT v10
Last updated: Fri, 11 Jun 2021 17:23:22 GMT
Data Views
Views
data as colors
data as contours
colors with land
contours with land
colors with coasts| L | T | T2 | X | Y | |
 IRI FD CPT Monsoon_Asia temperature maximum InputObs[ X Y T2 | T L] | M | M | M | M | M |
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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