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 con' sequences 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
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 con' sequences 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
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