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Titel Mapping the Interplay of ET and Topography on Precipitation Processes in the Eastern Andes
VerfasserIn Xiaoming Sun, Ana Barros
Konferenz EGU General Assembly 2015
Medientyp Artikel
Sprache Englisch
Digitales Dokument PDF
Erschienen In: GRA - Volume 17 (2015)
Datensatznummer 250108529
Publikation (Nr.) Volltext-Dokument vorhandenEGU/EGU2015-8286.pdf
 
Zusammenfassung
We present recent work toward elucidating the role of evapotranspiration in the hydrometeorology of the eastern Andes Mountains using realistic and quasi-idealized ET withdrawal experiments with WRF at very high resolution (~1 km grid spacing). The results show that evapotranspiration fluxes modulated by landform govern moist processes in the lower troposphere, including cloud formation and precipitation processes that account for daily precipitation amounts as high as 50-70% depending on synoptic conditions and season. Using parsimonious model experiments and observations for the Amazon basin and the Central Andes, we demonstrate that vegetation acts as a “terrestrial hydrostat” regulating precipitation locally by controlling atmospheric moist instability, and remotely through changes in atmospheric transport patterns. References Sun, X., and A. P. Barros, 2014a: Isolating the role of surface evapotranspiration on moist convection along the eastern flanks of the tropical Andes using a quasi-idealized approach. J. Atmos. Sci., 72, 243-261. Sun, X., and A. P. Barros, 2014b: Impact of Amazonian evapotranspiration on moisture transport and convection along the eastern flanks of the Andes. Q. J. R. Meteorol. Soc., In Review.