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Title: Hydrologic effects of climate change in the Delaware River basin

Journal Article · · Water Resources Bulletin; (United States)
OSTI ID:6059767
;  [1]
  1. Geological Survey, West Trenton, NJ (United States)

The Thornthwaite water balance and combinations of temperature and precipitation changes representing climate change were used to estimate changes in seasonal soil-moisture and runoff in the Delaware River basin. Winter warming may cause a greater proportion of precipitation in the northern part of the basin to fall as rain, which may increase winter runoff and decrease spring and summer runoff. Estimates of total annual runoff indicate that a 5 percent increase in precipitation would be needed to counteract runoff decreases resulting from a warming of 2C; a 15 percent increase for a warming of 4C. A warming of 2 to 4C, without precipitation increases, may cause a 9 to 25 percent decrease in runoff. The general circulation model derived changes in annual runoff ranged from {minus}39 to +9 percent. Results generally agree with those obtained in studies elsewhere. The changes in runoff agree in direction but differ in magnitude. In this humid temperate climate, where precipitation is evenly distributed over the year, decreases in snow accumulation in the northern part of the basin and increases in evapotranspiration throughout the basin could change the timing of runoff and significantly reduce total annual water availability unless precipitation were to increase concurrently.

OSTI ID:
6059767
Journal Information:
Water Resources Bulletin; (United States), Vol. 25:6; ISSN 0043-1370
Country of Publication:
United States
Language:
English