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Open AccessJournal ArticleDOI

Amazonian Deforestation and Regional Climate Change

TLDR
The authors used a coupled numerical model of the global atmosphere and biosphere (Center for Ocean-Land- Atmosphere GCM) to assess the effects of Amazonian deforestation on the regional and global climate, and found that when the Amazonian tropical forests were replaced by degraded grass (pasture) in the model, there was a significant increase in the mean surface temperature (about 2.5°C) and a decrease in the annual evapo-transpiration (30% reduction), precipitation (25% reduction) and runoff (20% reduction).
Abstract
Large-scale conversion of tropical forests into pastures or annual crops could lead to changes in the climate. We have used a coupled numerical model of the global atmosphere and biosphere (Center for Ocean-Land- Atmosphere GCM) to assess the effects of Amazonian deforestation on the regional and global climate. We found that when the Amazonian tropical forests were replaced by degraded grass (pasture) in the model, there was a significant increase in the mean surface temperature (about 2.5°C) and a decrease in the annual evapo-transpiration (30% reduction), precipitation (25% reduction), and runoff (20% reduction) in the region. The differences between the two simulations were greatest during the dry season. The deforested case was associated with larger diurnal fluctuations of surface temperature and vapor pressure deficit; such effects have been observed in existing deforested arms in Amazonia. The calculated reduction in precipitation was larger than the calculated decrease in evapotranspirat...

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Investigating soil moisture-climate interactions in a changing climate: A review

TL;DR: In this paper, the authors provide a synthesis of past research on the role of soil moisture for the climate system, based both on modelling and observational studies, focusing on soil moisture-temperature and soil moistureprecipitation feedbacks, and their possible modifications with climate change.
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Modeling the Exchanges of Energy, Water, and Carbon Between Continents and the Atmosphere

TL;DR: Modern schemes incorporate biogeochemical and ecological knowledge and, when coupled with advanced climate and ocean models, will be capable of modeling the biological and physical responses of the Earth system to global change, for example, increasing atmospheric carbon dioxide.
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The role of deep roots in the hydrological and carbon cycles of Amazonian forests and pastures

TL;DR: In this article, the authors estimate that half of the closed forests of Brazilian Amazonia depend on deep root systems to maintain green canopies during the dry season, and as much as 15% of this deep-soil carbon turns over on annual or decadal timescales.
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Large-scale impoverishment of Amazonian forests by logging and fire

TL;DR: In this article, the authors present field surveys of wood mills and forest burning across Brazilian Amazonia which show that logging crews severely damage 10,000 to 15,000 km2 of forest that are not included in deforestation mapping programmes.
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Climatic impact of tropical lowland deforestation on nearby montane cloud forests.

TL;DR: In this article, Landsat and Geostationary Operational Environmental Satellite imagery show that deforested areas of Costa Rica's Caribbean lowlands remain relatively cloud-free when forested regions have well-developed dry season cumulus cloud fields.
References
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Journal ArticleDOI

Biomass Burning in the Tropics: Impact on Atmospheric Chemistry and Biogeochemical Cycles

TL;DR: Widespread burning of biomass serves to clear land for shifting cultivation, to convert forests to agricultural and pastoral lands, and to remove dry vegetation in order to promote agricultural productivity and the growth of higher yield grasses, but it may also disturb biogeochemical cycles, especially that of nitrogen.
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Climate and life

Journal ArticleDOI

A Comparative Study of the Effects of Albedo Change on Drought in Semi-Arid Regions.

TL;DR: In this paper, the effects of changes in albedo on rainfall in semi-arid areas were studied and the mechanism by which an increase of albedos reduces the rainfall during conditions of high evaporation was considered.
Journal ArticleDOI

A Global Climatology of Albedo, Roughness Length and Stomatal Resistance for Atmospheric General Circulation Models as Represented by the Simple Biosphere Model (SiB)

TL;DR: In this paper, the Simple Biosphere Model (SiB) was used to generate global monthly fields of surface albedo (0.4-4.0 microns), roughness length and minimum surface (stomatal) resistance.
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