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Troy R. Brosten

Researcher at Boise State University

Publications -  14
Citations -  513

Troy R. Brosten is an academic researcher from Boise State University. The author has contributed to research in topics: Hyporheic zone & Permafrost. The author has an hindex of 7, co-authored 14 publications receiving 468 citations. Previous affiliations of Troy R. Brosten include United States Geological Survey.

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Application of time-lapse ERT imaging to watershed characterization

TL;DR: In this article, the authors assess various approaches for inverting and interpreting time-lapse electrical resistivity tomography (ERT) data and determine that the first approach is useful to proceed beyond straightforward inversion of data differences and take advantage of thetime-lapsenature-of-differentata.
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Transient storage as a function of geomorphology, discharge, and permafrost active layer conditions in Arctic tundra streams

TL;DR: In this paper, the effects of discharge, channel morphology, and potential size of the hyporheic zone on transient storage were investigated using stream tracer experiments in five morphologically diverse tundra streams in Arctic Alaska during the thaw season of 2004.
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Profiles of temporal thaw depths beneath two arctic stream types using ground‐penetrating radar

TL;DR: In this paper, a series of ground-penetrating radar (GPR) profiles at five sites from May-September, using 100, 200 and 400 MHz antennas, were acquired to investigate thaw progression over the 2004 summer season.
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Influence of Morphology and Permafrost Dynamics on Hyporheic Exchange in Arctic Headwater Streams under Warming Climate Conditions

TL;DR: In this paper, the authors investigated surface-subsurface (hyporheic) exchange in two morphologically distinct arctic headwater streams experiencing warming (thawing) sub-channel conditions.
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Estimating 3D variation in active-layer thickness beneath arctic streams using ground-penetrating radar

TL;DR: In this article, the authors acquired 3D ground-penetrating radar (GPR) data across three stream sites on the North Slope, AK, in August 2005, to investigate the dependence of thaw depth on channel morphology.