1988
DOI: 10.1007/bf00140163
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The climatic impact of a Sonoran vegetation discontinuity

Abstract: The international fence separating Mexico and the United States is marked by a sharp vegetation discontinuity in the Sonoran Desert. Due to overgrazing, the Mexican side of the border has shorter grasses, more bare soil, and a higher albedo compared to the adjacent lands in the United States. In this investigation, long-term climate records are analyzed to determine the magnitude of any climatic differences associated with the spatial variation in the vegetation regime. The results suggest that summertime maxi… Show more

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Cited by 111 publications
(44 citation statements)
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References 38 publications
(43 reference statements)
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“…The increased drought amplified the regional reduction in biomass and production. In another case, the reduction in transpiration resulting from overgrazing in northern Mexico increased sensible heat flux, causing regional warming (39).…”
Section: Species Traitsmentioning
confidence: 99%
“…The increased drought amplified the regional reduction in biomass and production. In another case, the reduction in transpiration resulting from overgrazing in northern Mexico increased sensible heat flux, causing regional warming (39).…”
Section: Species Traitsmentioning
confidence: 99%
“…These results, which are in agreement with long-term temperature records from nearby areas in the Southwestern United States (Balling, 1988;Balling et al, 1998;Bryant et al, 1990;Small and Kurc, 2003), need to be validated by field observations capable of explaining the underlying processes. Therefore, the objective of this paper is to explain the difference of nighttime temperatures over grassdominated and shrub-dominated areas and identify the salient processes causing the climatic differences observed between these two land covers.…”
Section: Introductionsupporting
confidence: 76%
“…Evidence of the effects of human activities on climate systems have been described by modeling programs [2] [3] who predicted an increase in temperature associated to change in soil cover, essen-tially involving deforestation and the continuous emissions of greenhouse gases. Field evidence of these effects goes from local scales [4] [5] to a regional extent [6]- [8]. These processes have been described linked to transformation of natural forested areas into agriculture fields [9] [10], or due to larger climate processes [11].…”
Section: Introductionmentioning
confidence: 99%