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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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The seasonal evolution of albedo across glaciers and the surrounding landscape of Taylor Valley, Antarctica

TL;DR: In this paper, a box with a camera, GPS, and shortwave radiometer was attached to a helicopter that flew transects four to five times a season along Taylor Valley.
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Stream tracer breakthrough curve decomposition into mass fractions: A simple framework to analyze and compare conservative solute transport processes

TL;DR: In this article, the authors present a new approach to analyze BTCs to quantify the amount of stream water transported by each dominant process, and parse the total quantity of injected tracer mass into three dominant process domains: advection and dispersion, transient storage, and gross loss of tracer.
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The significance of model structure in one-dimensional stream solute transport models with multiple transient storage zones – competing vs. nested arrangements

TL;DR: In this paper, the authors compare and contrast the application and interpretations from two model structures that include STS and HTS storage: a competing model structure, where both zones are connected to the stream at the same location and the stream interacts with the transient storage and hyporheic transient storage separately, and a nested model structure where STS is an intermediary between the stream and the HTS.
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Groundwater–surface-water interactions: current research directions

TL;DR: In this paper, the authors presented the results of a study at the Pacific Northwest Research Station of United States Department of Agriculture Forest Service, Corvallis, Oregon 97331 USA.
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Stream biogeochemical and suspended sediment responses to permafrost degradation in stream banks in Taylor Valley, Antarctica

TL;DR: In this article, the authors found substantial channel erosion and subsurface thermomechanical erosion undercutting banks of the Crescent Stream in the McMurdo Dry Valleys, which may substantially impact stream solute loads and potentially affect stream and lake ecosystems.