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Effects Of Tropical Deforestation On Climate And Agriculture Pdf

effects of tropical deforestation on climate and agriculture pdf

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Pablo O. Most experimental and modeling studies have focused on the resulting perturbations within Amazonia. Precipitation changes for and land-use scenarios, while significant within deforested areas, do not result in significant regional changes.

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Large-scale conversion of tropical forests into pastures or annual crops will likely lead to changes in the local microclimate of those regions. Larger diurnal fluctuations of surface temperature and humidity deficit, increased surface runoff during rainy periods and decreased runoff during the dry season, and decreased soil moistrue are to be expected. It is likely that evapotranspiration will be reduced because of less available radiative energy at the canopy level since grass presents a higher albedo than forests, also because of the reduced availability of soil moisture at the rooting zone primarily during the dry season. Recent results from general circulation model GCM simulations of Amazonian deforestation seem to suggest that the equilibrium climate for a grassy vegetation in Amazonia would be one in which regional precipitation would be significantly reduced. Global climate changes probably will occur if there is a marked change in rainfall patterns in tropical forest regions as a result of deforestation.

Metrics details. Some evidence suggests that forests attract rain and that deforestation contributes to changes in rainfall and temperature. The evidence, however, is scant, particularly on smaller spatial scales. The specific objectives of the study were: i to evaluate long-term trends in rainfall — and temperature — and their relationships with change in forest cover, and ii to assess the influence of remnant forests and topographical factors on the spatial variability of annual rainfall. This study investigated the forest-rainfall relationships in the Central Rift Valley of Ethiopia.

Thank you for visiting nature. You are using a browser version with limited support for CSS. To obtain the best experience, we recommend you use a more up to date browser or turn off compatibility mode in Internet Explorer. In the meantime, to ensure continued support, we are displaying the site without styles and JavaScript. An Erratum to this article was published on 28 January Tower, ground-based and satellite observations indicate that tropical deforestation results in warmer, drier conditions at the local scale. Understanding the regional or global impacts of deforestation on climate, and ultimately on agriculture, requires modelling.

Deforestation

Tropical forests are a major source of global hydrologic fluxes, profoundly influencing both global and regional climates see Kumagai et al. Humans have been modifying tropical forest land cover for food and energy production and for the development of tropical countries. Consequently, such modifications, that is, land use and land cover change LULCC , are being combined with climate change and are anticipated to impact the climate on local, regional, and even global scales via teleconnections Werth and Avissar ; Medvigy et al. Lawrence and Vandecar summarized difficulties in projecting the precipitation change induced by tropical deforestation on continental and local scales; for example, precipitation could be reduced or enhanced in accordance with the size and state of deforestation a single large patch is similar to distributed patches. Here, we must note that, in turn, such LULCC-driven hydroclimate change could lead to significant negative impacts on tropical forest ecological patterns and processes see Malhi et al.

Effects of tropical deforestation on climate and agriculture

Deforestation is associated with increased atmospheric CO 2 and alterations to the surface energy and mass balances that can lead to local and global climate changes. Previous modelling studies show that the global surface air temperature SAT response to deforestation depends on latitude, with most simulations showing that high latitude deforestation results in cooling, low latitude deforestation causes warming and that the mid latitude response is mixed. These earlier conclusions are based on simulated large scal land cover change, with complete removal of trees from whole latitude bands. All high latitude deforestation scenarios reduce mean global SAT, the opposite occurring for low latitude deforestation, although a decrease in SAT is simulated over low latitude deforested areas.

Skip to search form Skip to main content You are currently offline. Some features of the site may not work correctly. DOI: Lawrence and K.

Deforestation , clearance , clearcutting , or clearing is the removal of a forest or stand of trees from land that is then converted to non-forest use. The most concentrated deforestation occurs in tropical rainforests. The Food and Agriculture Organization of the United Nations defines deforestation as the conversion of forest to other land uses regardless of whether it is human-induced.

Possible climatic impacts of tropical deforestation

The United States Environmental Protection Agency defines deforestation as the "permanent removal of standing forests. Deforestation is the clearing, destroying, or otherwise removal of trees through deliberate, natural, or accidental means. It can occur in any area densely populated by trees and other plant life, but the majority of it is currently happening in the Amazon rainforest.

Possible climatic impacts of tropical deforestation

Deforestation is a primary contributor to climate change. Global models and national greenhouse gas inventories give similar results for deforestation emissions. Growing forests are a carbon sink with additional potential to mitigate the effects of climate change. Some of the effects of climate change , such as more wildfires , may increase deforestation. The vast majority of agricultural activity resulting in deforestation is subsidized by government tax revenue. The main area of concern of deforestation is in tropical rain forests since they are home to the majority of the planet's biodiversity.

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At this smaller scale as well, a critical deforestation threshold exists, beyond which rainfall declines. Future agricultural productivity in the tropics is at risk from a deforestation-induced increase in mean temperature and the associated heat extremes and from a decline in mean rainfall or rainfall frequency.


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2 Comments

  1. Kerstin S.

    10.12.2020 at 05:56
    Reply

    This study investigates the effect of roads growth toward the deforestation rate in 33 provinces in Indonesia from eight years period of time,

  2. Montague V.

    19.12.2020 at 10:58
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