Regional Hydroclimatic Variability Due To Contemporary Deforestation in Southern Amazonia and Associated Boundary Layer Characteristics

Amazonian deforestation causes systematic changes in regional dry season precipitation. Some of these changes at contemporary large scales (a few hundreds of kilometers) of deforestation have been associated with a “dynamical mesoscale circulation,” induced by the replacement of rough forest with sm...

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Veröffentlicht in:	Journal of geophysical research. Atmospheres 2018-04, Vol.123 (8), p.3993-4014
Hauptverfasser:	Khanna, Jaya, Medvigy, David, Fisch, Gilberto, Araújo Tiburtino Neves, Theomar Trindade
Format:	Artikel
Sprache:	eng
Schlagworte:	Amazon Annual variations Atmospheric conditions Boundary layer Boundary layers Computer simulation Condensation Deforestation Dry season dynamical circulation Geophysics Hydroclimate Interannual variations Lifting condensation level Mesoscale circulation Numerical simulations Pasture Precipitation precipitation seasonality Regions Rondônia Seasonal variation Seasons surface roughness Wind speed
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