served from IRI/LDEO Climate Data Library
∂T [ LDEO TRL MADA pdsi ]: ∂T data
pdsi pdsi ∂T from LDEO TRL MADA: Reconstruction of Palmer Drought Severity Index for Monsoon Asia based on tree ring data.Independent Variables (Grids)
- Time
- grid: /T (months since 1960-01-01) ordered (Jul 1300 - Jun 1301) to (Jul 2004 - Jun 2005) by 12.0 N= 705 pts :grid
- Longitude
- grid: /X (degree_east) ordered (62.5E) to (142.5E) by 2.5 N= 33 pts :grid
- Latitude
- grid: /Y (degree_north) ordered (8.75S) to (56.25N) by 2.5 N= 27 pts :grid
Other Info
- datatype
- realarraytype
- file_missing_value
- -99.999001
- iridl:hasSemantics
- iridl:PalmerDroughtSeverityIndex
- missing_value
- NaN
- units
- 12 year-1
References
Cook, E.R., K.J. Anchukaitis, B.M. Buckley, R.D. D'Arrigo, G.C. Jacoby, W.E. Wright, Asian monsoon failure and megadrought during the last millennium, Science, 328(5977), doi:10.1126/science.1185188, 2010
Last updated: Mon, 12 Sep 2016 21:11:48 GMT
Data Views
Views
data as colors
data as contours
colors with land
contours with land
colors with coasts| T | X | Y | |
 $partialdiff sub T$ [ LDEO TRL MADA pdsi ][ T Y | X] | 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 T Y X
- Differentiate along T Y X
- Take differences along T Y X
RMS (root mean square with mean *not* removed) over T Y X | T Y T X Y X | T Y X |
RMSA (root mean square with mean removed) over T Y X | T Y T X Y X | T Y X |
Maximum over T Y X | T Y T X Y X | T Y X |
Minimum over T Y X | T Y T X Y X | T Y X |
Detrend (best-fit-line) over T Y X | T Y T X Y X | T Y X |
Note on units