Spatiotemporal processes that contribute to hydrologic exchange between hillslopes, valley bottoms, and streams

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Spatiotemporal processes that contribute to hydrologic exchange between hillslopes, valley bottoms, and streams

Quantifying how watershed structure influences the exchanges of water among component parts of a watershed, particularly the connection between uplands, valley bottoms, and in-stream hydrologic exchange, remains a challenge. However, this understanding is critical for ascertaining the source areas and temporal contributions of water and associated biogeochemical constituents in streams. We used...

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9 Hydrologic Processes

A catchment is a basic unit of landscape particularly for investigations of hydrologic processes. Typically, the topographic boundary of a catchment coincides with the hydrologic boundary causing any precipitation falling on to the catchment to be routed to a stream where it is transported out of the catchment. Fundamental components of the hydrologic cycle, such as precipitation, runoff and ev...

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Variability in isotopic composition of base flow in two headwater streams of the southern Appalachians

We investigated the influence of hillslope scale topographic characteristics and the relative position of hillslopes along streams (i.e., internal catchment structure) on the isotopic composition of base flow in first-order, forested headwater streams at Coweeta Hydrologic Laboratory. The study focused on two adjacent forested catchments with different topographic characteristics. We used stabl...

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ژورنال

عنوان ژورنال: Water Resources Research

سال: 2016

ISSN: 0043-1397

DOI: 10.1002/2015wr017972