Tc. Piechota et Ja. Dracup, DROUGHT AND REGIONAL HYDROLOGIC VARIATION IN THE UNITED-STATES - ASSOCIATIONS WITH THE EL-NINO SOUTHERN OSCILLATION, Water resources research, 32(5), 1996, pp. 1359-1373
Using 94 years of monthly Palmer Drought Severity Index (PDSI) data fo
r 344 climate divisions, this study investigates the hydroclimatic res
ponse in the United States to the extreme phases of the Southern Oscil
lation (El Nino and La Nina). Several regions of coherent response to
El Nino-Southern Oscillation (ENSO) are identified. The strongest rela
tionship between El Nino and extreme drought years is found in the Pac
ific Northwest. A strong relationship is also noticed in the southern
United States, where dry conditions occur consistently during La Nina
events. Next, the conditional response in PDSI is evaluated based on t
he extreme phases of the Southern Oscillation. The PDSI results were c
ompared to similar analyses on 41 years of station temperature, precip
itation, and streamflow data. A consistent response is seen in the oth
er hydroclimatic variables, though the most filtered response is seen
in PDSI data and streamflow data. The major contribution to the unders
tanding of the ENSO-United States climate relationship is the evaluati
on of the general form of drought and comparison of these results to t
he fundamental hydrologic processes (precipitation, temperature, and s
treamflow).