| Thomas L. Thurow and Charles A. Taylor, Jr. |
| Authors are professor and head, Renewable Resources Department, University of Wyoming, Laramie, Wyo. 82071 and professor, Texas Agricultural Experiment Station, P.O. Box 918, Sonora, Tex. 76950. |
Abstract |
| Drought is an ambiguous term, subject to expectation and the weight of emphasis on meteorological, agricultural, hydrological and socio-economic dimensions. Uncertainty associated with the identification of drought often results in a lagged response in reducing stocking rates. This delay reduces vegetation cover, increasing the potential for accelerated erosion following the drought. The long-term consequences of accelerated erosion are a reduction of soil depth, a decline in soil structure and a decrease in infiltration rate and water storage capacity. Less water stored on a site hastens the onset of plant stress, effectively increasing the perceived frequency and consequences of drought. Management and policy tools must improve the integration of economic and ecological aspects of drought-induced de-stocking decisions, especially by incorporating the long-term irreversible costs of erosion. |
| Key Words: climate, desertification, erosion, grazing management, hydrologic cycle |