served from IRI/LDEO Climate Data Library
detrended-bfl ∫dY [ IRI Analyses ENSO-RP ver1950-2002 2p5deg prob ] : probability data
2p5deg prob int_dY int_dY 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 (Dec - Feb) to (Nov - Jan) by 1.0 N= 12 pts :grid
- Longitude (longitude)
- grid: /X (degree_east) periodic (2.5E) to (0) by 2.5 N= 144 pts :grid
- Latitude (latitude)
- grid: /Y (degree_north) ordered (90N) to (90S) by 2.5 N= 73 pts :grid
Other Info
- bufferwordsize
- 8
- CE
- null
- colorscalename
- tercileclassesscale
- CS
- null
- datatype
- doublearraytype
- file_missing_value
- -9999.0
- maxncolor
- 254
- missing_value
- NaN
- units
- degree_north
- standard units*
- 0.0174532925199433 radian north
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 | |
 detrended-bfl $integral dY$ [ IRI Analyses ENSO-RP ver1950-2002 2p5deg prob ] [ X Y | ENSO prcp 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 ENSO prcp T
- Differentiate along X Y ENSO prcp T
- Take differences along X Y ENSO prcp T
RMS (root mean square with mean *not* removed) over X Y ENSO prcp T | X Y X ENSO X prcp X T Y ENSO Y prcp Y T ENSO prcp ENSO T prcp T | X Y ENSO X Y prcp X Y T X ENSO prcp X ENSO T X prcp T Y ENSO prcp Y ENSO T Y prcp T ENSO prcp T | X Y ENSO prcp X Y ENSO T X Y prcp T X ENSO prcp T Y ENSO prcp T | X Y ENSO prcp T |
RMSA (root mean square with mean removed) over X Y ENSO prcp T | X Y X ENSO X prcp X T Y ENSO Y prcp Y T ENSO prcp ENSO T prcp T | X Y ENSO X Y prcp X Y T X ENSO prcp X ENSO T X prcp T Y ENSO prcp Y ENSO T Y prcp T ENSO prcp T | X Y ENSO prcp X Y ENSO T X Y prcp T X ENSO prcp T Y ENSO prcp T | X Y ENSO prcp T |
Maximum over X Y ENSO prcp T | X Y X ENSO X prcp X T Y ENSO Y prcp Y T ENSO prcp ENSO T prcp T | X Y ENSO X Y prcp X Y T X ENSO prcp X ENSO T X prcp T Y ENSO prcp Y ENSO T Y prcp T ENSO prcp T | X Y ENSO prcp X Y ENSO T X Y prcp T X ENSO prcp T Y ENSO prcp T | X Y ENSO prcp T |
Minimum over X Y ENSO prcp T | X Y X ENSO X prcp X T Y ENSO Y prcp Y T ENSO prcp ENSO T prcp T | X Y ENSO X Y prcp X Y T X ENSO prcp X ENSO T X prcp T Y ENSO prcp Y ENSO T Y prcp T ENSO prcp T | X Y ENSO prcp X Y ENSO T X Y prcp T X ENSO prcp T Y ENSO prcp T | X Y ENSO prcp T |
Detrend (best-fit-line) over X Y ENSO prcp T | X Y X ENSO X prcp X T Y ENSO Y prcp Y T ENSO prcp ENSO T prcp T | X Y ENSO X Y prcp X Y T X ENSO prcp X ENSO T X prcp T Y ENSO prcp Y ENSO T Y prcp T ENSO prcp T | X Y ENSO prcp X Y ENSO T X Y prcp T X ENSO prcp T Y ENSO prcp T | X Y ENSO prcp T |
Note on units