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U.S. Gridded Palmer Drought Severity Index (PDSI) from gridMET

Associated Agencies

University of California, Merced

This new experimental implementation of the Palmer Drought Severity Index (PDSI) updates every 5 days using the high-resolution gridMET gridded research dataset and USDA STATSGO soils data. The PDSI is a standardized index based on a simplified soil water balance and estimates relative soil moisture conditions. The magnitude of PDSI indicates the severity of the departure from normal conditions. A PDSI value >4 represents very wet conditions, while a PDSI <-4 represents an extreme drought. 

This PDSI uses a new methodology for sub-monthly PDSI, outlined in the Documentation section below.

 

Interactive Map: Gridded Palmer Drought Severity Index
Map

Dry Conditions (Relative)
Range Map Hex Color
- -5 #730000
-5 - -4 #e60000
-4 - -3 #ffaa00
-3 - -2 #fcd37f
-2 - -1 #ffff00
Wet Conditions (Relative)
Range Map Hex Color
1 - 2 #aaff55
2 - 3 #01ffff
3 - 4 #00aaff
4 - 5 #00f
5 - #00a

Experimental

Access

Climate Engine: View this sub-monthly PDSI with the Climate Engine tool.

THREDDS: Access this sub-monthly PDSI data with THREDDS, including service access using OPeNDAP, Web Map Service (WMS) and the NetCDF Subset tool.  Data downloads are available in NetCDF for grids or CSV/XML/JSON for single grid cell subsets.

Documentation

This PDSI uses a new methodology for sub-monthly PDSI, based on the methodology outlined in Rhee, J., and G. J. Carbone. 2007. "A Comparison of Weekly Monitoring Methods of the Palmer Drought Index." Journal of Climate, 20(24): 6033-6044. 

PDSI and Z are calculated using a modified version of the Palmer formula, which uses reference evapotranspiration and precipitation from gridMET, and a static soil water holding capacity layer (top 1500mm) from STATSGO. The Z-index is calculated using non-overlapping 6-pentad (30-day) blocks of precipitation and potential ET. To compute the pentad PDSI, the authors apply modifications to the standard PDSI equations similar to Rhee et al. 2007. First, the Z-index is divided by 6 given the differences between a ~30-day month and a 5-day pentad. Second, the coefficient of the drought severity equation is modified as X(i)=0.9828*X(i-1)+Z/3; and modified effective wetness/dryness accordingly to scale for differences between the timescales. The baseline period for PDSI and Z calculations is 1979-2018. Given the non-standard nature of the calculations, the pentad PDSI and Z-index are experimental.