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1000 Titel
  • The agricultural expansion in South America's Dry Chaco: regional hydroclimate effects
1000 Autor/in
  1. Bracalenti, María Agostina |
  2. Müller, Omar |
  3. Lovino, Miguel |
  4. Berbery, Ernesto Hugo |
1000 Verlag Copernicus Publications
1000 Erscheinungsjahr 2024
1000 Publikationstyp
  1. Artikel |
1000 Online veröffentlicht
  • 2024-07-25
1000 Erschienen in
1000 Quellenangabe
  • 28(14):3281-3303
1000 Copyrightjahr
  • 2024
1000 Lizenz
1000 Verlagsversion
  • https://doi.org/10.5194/hess-28-3281-2024 |
1000 Publikationsstatus
1000 Begutachtungsstatus
1000 Sprache der Publikation
1000 Abstract/Summary
  • <jats:p>Abstract. The Gran Chaco ecoregion is South America's largest remaining continuous stretch of dry forest. It has experienced intensive deforestation, mainly in the western part known as the Dry Chaco, resulting in the highest rate of dry-forest loss globally between 2000 and 2012. The replacement of natural vegetation with other land uses modifies the surface's biophysical properties, affecting heat and water fluxes and modifying the regional climate. This study examines land use and land cover changes (LULCCs) in the Dry Chaco from 2001 to 2015 and their effects on local and non-local climate and explores the potential impacts of future agricultural expansion in the region. To this end, Weather Research and Forecasting (WRF) model simulations are performed for two scenarios: the first one evaluates the observed land cover changes between 2001 and 2015 that covered 8 % of the total area of the Dry Chaco; the second scenario assumes an intensive agricultural expansion within the Dry Chaco. In both scenarios, deforestation processes lead to decreases in leaf area index (LAI), reductions in stomatal resistance, and increases in albedo, thus reducing the net surface radiation and, correspondingly, decreasing the turbulent fluxes, suggesting a decline in available energy in the boundary layer. The result is an overall weakening of the water cycle in the Dry Chaco and, most prominently, implying a reduction in precipitation. A feedback loop develops since dry soil absorbs significantly less solar radiation than moist soil. Finally, the simulations suggest that the Dry Chaco will intensify its aridity, extending drier and hotter conditions into the Humid Chaco. </jats:p>
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1000 Liste der Beteiligten
  1. https://frl.publisso.de/adhoc/uri/QnJhY2FsZW50aSwgTWFyw61hIEFnb3N0aW5h|https://orcid.org/0000-0001-9943-8368|https://orcid.org/0000-0002-8558-6324|https://orcid.org/0000-0003-2587-3345
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  1. Agencia Santafesina de Ciencia, Tecnología e Innovación |
  2. Agencia Nacional de Promoción Científica y Tecnológica |
  3. Consejo Nacional de Investigaciones Científicas y Técnicas |
  4. National Oceanic and Atmospheric Administration |
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1000 Dateien
1000 Förderung
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    1000 Förderer Agencia Santafesina de Ciencia, Tecnología e Innovación |
    1000 Förderprogramm -
    1000 Fördernummer -
  2. 1000 joinedFunding-child
    1000 Förderer Agencia Nacional de Promoción Científica y Tecnológica |
    1000 Förderprogramm -
    1000 Fördernummer -
  3. 1000 joinedFunding-child
    1000 Förderer Consejo Nacional de Investigaciones Científicas y Técnicas |
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    1000 Fördernummer -
  4. 1000 joinedFunding-child
    1000 Förderer National Oceanic and Atmospheric Administration |
    1000 Förderprogramm -
    1000 Fördernummer -
1000 Objektart article
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1000 Erstellt am 2024-10-03T10:07:31.144+0200
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1000 Zuletzt bearbeitet 2025-08-14T00:36:46.797+0200
1000 Objekt bearb. Thu Aug 14 00:36:46 CEST 2025
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