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Dean E. Anderson

Researcher at United States Geological Survey

Publications -  30
Citations -  2229

Dean E. Anderson is an academic researcher from United States Geological Survey. The author has contributed to research in topics: Eddy covariance & Wind speed. The author has an hindex of 21, co-authored 30 publications receiving 2152 citations. Previous affiliations of Dean E. Anderson include University of Nebraska–Lincoln & Oak Ridge National Laboratory.

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Comparing nocturnal eddy covariance measurements to estimates of ecosystem respiration made by scaling chamber measurements at six coniferous boreal sites

TL;DR: In this article, the authors used relationships between woody tissue, foliage, and soil respiration rates and temperature, with temperature records collected on site to estimate ecosystem respiration rate at six coniferous BOREAS sites at half-hour or 1-hour intervals, and then compared these estimates to nocturnal measurements of CO2 exchange by eddy covariance.
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Eddy fluxes of CO2, water vapor, and sensible heat over a deciduous forest

TL;DR: In this article, the effects of solar radiation, vapor pressure deficit and the aerodynamic and canopy resistances on mass and energy exchanges were examined over a fully-leafed deciduous forest in eastern Tennessee.
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Airflows and turbulent flux measurements in mountainous terrain Part 1. Canopy and local effects

TL;DR: In this article, the effects of local topography and canopy structure on turbulent flux measurements at a site located in mountainous terrain within a subalpine, coniferous forest were investigated.
Book

Unsaturated Zone Hydrology for Scientists and Engineers

TL;DR: In this paper, the authors describe the potential and thermodynamic properties of Soil Water, Solute, and Vapor Movement, as well as its properties in terms of water flow in Soil.
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Energy budget above a high-elevation subalpine forest in complex topography

TL;DR: In this paper, the authors measured the energy budget of a subalpine coniferous forest over two complete annual cycles and found that the energy balance was slightly better in the winter as opposed to summer, since numerous periods of high turbulence occur in winter.