Relating low-flow characteristics to the base flow recession time constant at partial record stream gauges

被引:42
|
作者
Eng, Ken
Milly, P. C. D.
机构
[1] US Geol Survey, Reston, VA USA
[2] NOAA, Geophys Fluid Dynam Lab, Princeton, NJ USA
[3] US Geol Survey, Princeton, NJ 08542 USA
关键词
D O I
10.1029/2006WR005293
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Base flow recession information is helpful for regional estimation of low-flow characteristics. However, analyses that exploit such information generally require a continuous record of streamflow at the estimation site to characterize base flow recession. Here we propose a simple method for characterizing base flow recession at low-flow partial record stream gauges (i.e., sites with very few streamflow measurements under low-streamflow conditions), and we use that characterization as the basis for a practical new approach to low-flow regression. In a case study the introduction of a base flow recession time constant, estimated from a single pair of strategically timed streamflow measurements, approximately halves the root-mean-square estimation error relative to that of a conventional drainage area regression. Additional streamflow measurements can be used to reduce the error further.
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页数:8
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