Drought conditions are assessed using precipitation amounts, stream flows, lake and reservoir levels, and soil moisture. In the 1960's, Wayne Palmer developed the Palmer Drought Severity Index (PDSI) based on temperature and rainfall. It is most effective over a period of several months, enabling it to measure meteorological and hydrological drought.
Palmer also developed the Crop Moisture Index (CMI) for use from week to week, instead of months. It is more efficient at measuring short term dryness or wetness, which will more easily influence agriculture.
In recent years, a new tool has been developed by the National Drought Mitigation Center, located at the University of Nebraska, Tracking drought blends science and art. No single definition of drought works for all circumstances, so people rely on drought indices to detect and measure droughts. But no single index works under all circumstances, either. That's why the Drought Monitor was developed, a synthesis of multiple indices, outlooks and news accounts, that represents a consensus of federal and academic scientists. The product will be refined over time as ways are found to make it better reflect the needs of decision-makers and others who use the information. Click
here to view the latest U.S. Drought Monitor.