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Sarah E. Godsey

Researcher at Idaho State University

Publications -  59
Citations -  3107

Sarah E. Godsey is an academic researcher from Idaho State University. The author has contributed to research in topics: Streamflow & Permafrost. The author has an hindex of 22, co-authored 51 publications receiving 2163 citations. Previous affiliations of Sarah E. Godsey include University of California, Berkeley & University of Cincinnati.

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Concentration–discharge relationships reflect chemostatic characteristics of US catchments

TL;DR: In this paper, the authors examined concentration-discharge relationships for solutes produced primarily by mineral weathering in 59 geochemically diverse US catchments and found that these catchments exhibit nearly chemostatic behaviour; their stream concentrations of weathering products such as Ca, Mg, Na, and Si typically vary by factors of only 3 to 20 while discharge varies by several orders of magnitude.
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Dynamic, discontinuous stream networks: hydrologically driven variations in active drainage density, flowing channels and stream order

TL;DR: In this paper, the authors present field surveys of the active drainage networks of four California headwater streams (4 −27 km2) spanning diverse topographic, geologic and climatic settings.
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Hydrological Partitioning in the Critical Zone: Recent Advances and Opportunities for Developing Transferable Understanding of Water Cycle Dynamics

TL;DR: In this article, the authors present a review of recent work in catchment hydrology and hydrochemistry, hydrogeology, and ecohydrology that highlights a common knowledge gap in how precipitation is partitioned in the critical zone: how is the amount, routing, and residence time of water in the subsurface related to the biogeophysical structure of the CZ?
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Patterns and persistence of hydrologic carbon and nutrient export from collapsing upland permafrost

TL;DR: In this paper, the authors studied the effect of permafrost collapse on aquatic biogeochemical cycles and found that thermokarst caused substantial increases in dissolved organic carbon and other solute concentrations with a particularly large impact on inorganic nitrogen.