Physical and temporal isolation of mountain headwater streams in the western mojave desert, southern california
Streams draining mountain headwater areas of the western Mojave Desert are commonly physically isolated from downstream hydrologic systems such as springs, playa lakes, wetlands, or larger streams and rivers by stream reaches that are dry much of the time. The physical isolation of surface flow in t...
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Veröffentlicht in: | Journal of the American Water Resources Association 2007-02, Vol.43 (1), p.26-40 |
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Format: | Artikel |
Sprache: | eng |
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