2016
DOI: 10.1063/pt.3.3364
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Land’s complex role in climate change

Abstract: To mitigate climate change at local, regional, and global scales, we must begin to think beyond greenhouse gases.

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Cited by 77 publications
(40 citation statements)
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“…Agricultural production and land use change generate about one third of the greenhouse gases (GHGs) emissions worldwide and are among the key drivers of global warming [100]. If one considers the entire food system-from field to fork to landfill-this is a conservative estimate.…”
Section: Sdg 13: Combat Climate Change and Its Impactsmentioning
confidence: 99%
“…Agricultural production and land use change generate about one third of the greenhouse gases (GHGs) emissions worldwide and are among the key drivers of global warming [100]. If one considers the entire food system-from field to fork to landfill-this is a conservative estimate.…”
Section: Sdg 13: Combat Climate Change and Its Impactsmentioning
confidence: 99%
“…In particular, albedo and roughness length are well known for their influence on the surface energy balance and wind, affecting not only the amount of precipitation but also its spatial distribution at the local scale (Pielke and Avissar, 1990;Pielke, 2001;Pielke et al, 2007a;Pielke et al, 2007b;Werth and Avissar, 2002; Silva ). Adjacent patches that differ at P < 0.05 are separated by a thin black line Dias, 2006;Mahmood et al, 2013;Pielke et al, 2016). The replacement of forests and grasslands by farmlands caused an overall reduction of precipitation as high as 100 mm month -1 in Eastern Paraguay and widespread increases and decreases of the order of 50 mm month -1 in Western Paraguay (Figure 5f).…”
Section: Near-surface Temperature and Precipitationmentioning
confidence: 99%
“…Changes in land cover imply changes in the biophysical properties of the surface, such as albedo, leaf area, roughness length, root depth, stomatal resistance, and other properties that depend on the land-cover type. Changes in vegetation traits can affect the exchange of momentum, heat, and moisture between the atmosphere and the underlying surface, and thus influence climate at different spatial and temporal scales (Pielke and Avissar, 1990;Pielke et al, 2007b;Mahmood et al, 2013;Pielke et al, 2016). Although these effects may go unnoticed in the global average, they can be significant at regional scales because they directly affect the patterns of rainfall and temperature as well as air circulation processes (Pielke, 2001;Werth and Avissar, 2002;Silva Dias, 2006;Mahmood et al, 2013;Pielke et al, 2016).…”
Section: Introductionmentioning
confidence: 99%
“…But its main climate role is to diminish the greenhouse effect by the large amounts of carbon it stores. Vegetation acts also by evapotranspiration [6]: the humidity that forest delivers to the atmosphere (Figure 1) favours regional rainfalls, a phenomenon which contributed to the "green Sahara" 6000 years ago (Figure 2). A stronger evapotranspiration has also a cooling effect on the surface.…”
Section: What Do We Call Greenhouse Effect?mentioning
confidence: 99%