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Cited by 375

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Baring High-Albedo Soils by Overgrazing: A Hypothesized Desertification Mechanism

Otterman, Joseph·1974·Science

Abstract

Observations are reported of high-albedo soils denuded by overgrazing which appear bright, in high contrast to regions covered by natural vegetation. Measurements and modeling show that the denuded surfaces are cooler, when compared under sunlit conditions. This observed "thermal depression" effect should, on theoretical grounds, result in a decreased lifting of air necessary for cloud formation and precipitation, and thus lead to regional climatic desertification.

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Metadata

Authors
Otterman, J.
Venue
Science
Published
1974-11-08
Volume
186
Issue
4163
Pages
531-533
ISSN
  • 0036-8075 (ISSN-L)
  • 1095-9203
OpenAlex
W2088481082
Cited by
375
References
0
FWCI
23.86
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: Baring High-Albedo Soils by Overgrazing: A Hypothesized Desertification Mechanism. https://app.cochat.ai/papers/10.1126/science.186.4163.531
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Otterman, J. (1974). Baring High-Albedo Soils by Overgrazing: A Hypothesized Desertification Mechanism. Science. https://doi.org/10.1126/science.186.4163.531

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Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).

Semantic Scholar’s data is described in: Kinney, R., et al. (2023). The Semantic Scholar Open Data Platform. arXiv:2301.10140.