Efficient prediction of ground surface temperature and moisture, with inclusion of a layer of vegetation

Deardorff, J. W.

doi:10.1029/JC083iC04p01889

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Efficient prediction of ground surface temperature and moisture, with inclusion of a layer of vegetation

Author(s): J. W. Deardorff

Publication date (Print): 1978

Journal: Journal of Geophysical Research

Publisher: American Geophysical Union (AGU)

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Most cited references 31

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Drought in the sahara: a biogeophysical feedback mechanism.

J Z Charney, Gregory J. Quirk, Robert P. Stone (1975)

Two integrations of a global general circulation model, differing only in the prescribed surface albedo in the Sahara, show that an increase in albedo resulting from a decrease in plant cover causes a decrease in rainfall. Thus any tendency for plant cover to decrease would be reinforced by a decrease in rainfall, and could initiate or perpetuate a drought.

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EVAPORATION, AND MOISTURE AND HEAT FIELDS IN THE SOIL

J. Philip (1957)

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Momentum, mass and heat exchange of vegetation

A. S. Thom (1972)

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Journal

Journal ID (publisher-id): JGREA2

Title: Journal of Geophysical Research

Abbreviated Title: J. Geophys. Res.

Publisher: American Geophysical Union (AGU)

ISSN (Print): 0148-0227

Publication date Created: 1978

Publication date (Print): 1978

Volume: 83

Issue: C4

Page: 1889

Article

DOI: 10.1029/JC083iC04p01889

SO-VID: 85c3d3ba-411e-4c47-9005-e38002ab9326

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http://doi.wiley.com/10.1002/tdm_license_1.1

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