M
Michael N. Gooseff
Researcher at University of Colorado Boulder
Publications - 176
Citations - 8903
Michael N. Gooseff is an academic researcher from University of Colorado Boulder. The author has contributed to research in topics: Hyporheic zone & Soil water. The author has an hindex of 50, co-authored 162 publications receiving 7636 citations. Previous affiliations of Michael N. Gooseff include Colorado State University & Colorado School of Mines.
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Journal ArticleDOI
Hydrologic connectivity between landscapes and streams: Transferring reach- and plot-scale understanding to the catchment scale
Kelsey Jencso,Brian L. McGlynn,Michael N. Gooseff,Steven M. Wondzell,Kenneth E. Bencala,Lucy Marshall +5 more
TL;DR: In this article, the authors quantified water table connectivity based on 84 recording wells distributed across 24 HRS transects within the Tenderfoot Creek Experimental Forest (U.S. Forest Service), northern Rocky Mountains, Montana.
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The polar regions in a 2°C warmer world
Eric Post,Richard B. Alley,Torben R. Christensen,Marc Macias-Fauria,Bruce C. Forbes,Michael N. Gooseff,Amy M. Iler,Jeffrey T. Kerby,Jeffrey T. Kerby,Kristin L. Laidre,Michael E. Mann,Johan Olofsson,Julienne Stroeve,Fran Ulmer,Ross A. Virginia,Muyin Wang,Muyin Wang +16 more
TL;DR: Expected consequences of increased Arctic warming include ongoing loss of land and sea ice, threats to wildlife and traditional human livelihoods, increased methane emissions, and extreme weather at lower latitudes.
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River corridor science: Hydrologic exchange and ecological consequences from bedforms to basins
TL;DR: In this article, the authors propose river corridor science as a concept that integrates downstream transport with lateral and vertical exchange across interfaces, and include the main channel exchange with recirculating marginal waters, hyporheic exchange, bank storage, and overbank flow onto floodplains under a broad continuum of interactions known as hydrologic exchange flows.
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Changes in the character of stream water dissolved organic carbon during flushing in three small watersheds, Oregon
TL;DR: In this paper, the specific UV absorbance (SUVA, 254 nm) of DOC in three watersheds increased by 9 to 36% during the storm, suggesting that DOC mobilized from catchment soils during storms is more aromatic than DOC entering the stream during baseflow.
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Moving beyond the banks: hyporheic restoration is fundamental to restoring ecological services and functions of streams.
TL;DR: Stream restoration needs to consider the hyporheic zone just as much as the surface and benthic regions when planning for the future ofStream restoration.