served from IRI/LDEO Climate Data Library
∂X [ IRI Analyses ENSO-RP ver1950-2002 2p5deg prob ]: ∂X probability data
2p5deg prob partial_X ∂X probability from IRI Analyses ENSO-RP ver1950-2002: Probabilistic precipitation anomalies associated with ENSO (1950-2002).Independent Variables (Grids)
- ENSO
- grid: /ENSO (ids) unordered [ (nino) (nina)] :grid
- prcp
- grid: /prcp (ids) unordered [ (wet) (normal) (dry)] :grid
- Time (time)
- grid: /T (months since 01-Jan) periodic (16 Jan - 15 Feb) to (16 Dec - 15 Jan) by 1.0 N= 12 pts :grid
- Longitude (longitude)
- grid: /X (degree_east) periodic (0) to (2.5W) by 2.5 N= 144 pts :grid
- Latitude (latitude)
- grid: /Y (degree_north) ordered (88.75N) to (88.75S) by 2.5 N= 72 pts :grid
Other Info
- CE
- 1
- colorscalename
- tercileclassesscale
- CS
- 0
- datatype
- realarraytype
- file_missing_value
- -9999.0
- maxncolor
- 254
- missing_value
- NaN
- units
- 57.2957795130823 radian-1 east
- colorscale
References
Mason_Goddard2001Lenssen, N. J. L., Goddard, L., Mason, S. (2020). Seasonal Forecast Skill of ENSO Teleconnection Maps, Weather and Forecasting, 35(6), 2387-2406.
Last updated: Fri, 11 Jun 2021 17:23:01 GMT
Data Views
Views
data as colors
data as contours
colors with land
contours with land
colors with coasts| ENSO | prcp | T | X | Y | |
 $partialdiff sub X$ [ IRI Analyses ENSO-RP ver1950-2002 2p5deg prob ][ X Y | prcp ENSO T] | 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 prcp ENSO T
- Differentiate along X Y prcp ENSO T
- Take differences along X Y prcp ENSO T
RMS (root mean square with mean *not* removed) over X Y prcp ENSO T | X Y X prcp X ENSO X T Y prcp Y ENSO Y T prcp ENSO prcp T ENSO T | X Y prcp X Y ENSO X Y T X prcp ENSO X prcp T X ENSO T Y prcp ENSO Y prcp T Y ENSO T prcp ENSO T | X Y prcp ENSO X Y prcp T X Y ENSO T X prcp ENSO T Y prcp ENSO T | X Y prcp ENSO T |
RMSA (root mean square with mean removed) over X Y prcp ENSO T | X Y X prcp X ENSO X T Y prcp Y ENSO Y T prcp ENSO prcp T ENSO T | X Y prcp X Y ENSO X Y T X prcp ENSO X prcp T X ENSO T Y prcp ENSO Y prcp T Y ENSO T prcp ENSO T | X Y prcp ENSO X Y prcp T X Y ENSO T X prcp ENSO T Y prcp ENSO T | X Y prcp ENSO T |
Maximum over X Y prcp ENSO T | X Y X prcp X ENSO X T Y prcp Y ENSO Y T prcp ENSO prcp T ENSO T | X Y prcp X Y ENSO X Y T X prcp ENSO X prcp T X ENSO T Y prcp ENSO Y prcp T Y ENSO T prcp ENSO T | X Y prcp ENSO X Y prcp T X Y ENSO T X prcp ENSO T Y prcp ENSO T | X Y prcp ENSO T |
Minimum over X Y prcp ENSO T | X Y X prcp X ENSO X T Y prcp Y ENSO Y T prcp ENSO prcp T ENSO T | X Y prcp X Y ENSO X Y T X prcp ENSO X prcp T X ENSO T Y prcp ENSO Y prcp T Y ENSO T prcp ENSO T | X Y prcp ENSO X Y prcp T X Y ENSO T X prcp ENSO T Y prcp ENSO T | X Y prcp ENSO T |
Detrend (best-fit-line) over X Y prcp ENSO T | X Y X prcp X ENSO X T Y prcp Y ENSO Y T prcp ENSO prcp T ENSO T | X Y prcp X Y ENSO X Y T X prcp ENSO X prcp T X ENSO T Y prcp ENSO Y prcp T Y ENSO T prcp ENSO T | X Y prcp ENSO X Y prcp T X Y ENSO T X prcp ENSO T Y prcp ENSO T | X Y prcp ENSO T |
Note on units