Index
- Alaska Climate Divisions FAQs
- Anomalies vs. Temperature
- Arctic Sea Ice Measurements
- Billion-Dollar Disasters: Calculating the Costs
- Binomial Filter
- Climate Division Dataset Transition
- Climate Extremes Index
- CLIMAT Messages
- Climatological Rankings
- Coral Reef Bleaching
- Dead Fuel Moisture
- Definition of Drought
- Drought Indicators
- Drought in the Colorado River Basin
- Drought vs. Aridity
- El Niño: A Historical Perspective
- Explanation of the 500 mb Flow
- Future Drought
- Global Precipitation Percentile Maps
- Global Regions Definitions
- Global Temperature Anomaly Percentile Maps
- Global Temperature Uncertainty
- Groundwater Drought Indicators
- Hawaiʻi Climate Divisions FAQs
- LOESS
- Measuring Drought
- Monthly Releases
- Monthly Report RSS Feed
- nClimDiv Maximum and Minimum Temperatures
- Palmer Drought Index
- Potential Evapotranspiration
- Reforestation of Bastrop Lost Pines
- Regional Climate Centers
- Regional Snowfall Index (RSI)
- Satellite-Based Drought Indicators
- Soil Moisture Water Balance Models
- Southern Hemisphere Snow Cover Extent
- Standardized Precipitation Index
- Streamflow Drought Indicators
- Subtropical Highs
- Tornado Count
- U.S. Climate Divisions
- U.S. Climate Normals
- U.S. Drought Monitor Scale
- USHCN Version 2.5 Transition
- Water Supply vs. Water Demand
Palmer Drought Index
In 1965, Wayne Palmer developed a drought index which built upon decades of earlier attempts to define and monitor drought. Palmer's index was revolutionary because, for the first time, it expressed drought and wet spells as a standardized index reflecting the imbalance between water supply and water demand. Many new drought indices have been developed since then, with some utilizing satellite observations and more sophisticated computer models among other things. The U.S. Drought Monitor incorporates information from all of these indices as well as drought impacts in depicting drought.