The Amazonian Boundary Layer and Mesoscale Circulations

5Citations
Citations of this article
66Readers
Mendeley users who have this article in their library.
Get full text

Abstract

The interactions between the Amazonian boundary layer, the surface, atmospheric convection, aerosols, and larger-scale circulations are complex. The field experiments in Amazonia have provided rich insights into the daytime and nighttime boundary layer in different regions and seasons over both forest and pasture and into the coupling between the surface fluxes, the boundary layer, precipitation, and cloud radiative forcing. We discuss the typical diurnal cycle of Amazonian convection, the self-organization into mesoscale systems in different synoptic regimes, and the role of forest and river breeze circulations. We review the coupling between aerosols, smoke, and convection in the dry season; ozone transports by deep convection; and microphysical and electrical impacts on convection.

Cite

CITATION STYLE

APA

Betts, A. K., Fisch, G., Von Randow, C., Silva Dias, M. A. F., Cohen, J. C. P., Da Silva, R., & Fitzjarrald, D. R. (2013). The Amazonian Boundary Layer and Mesoscale Circulations. In Amazonia and Global Change (pp. 163–181). Wiley Blackwell. https://doi.org/10.1029/2008GM000720

Register to see more suggestions

Mendeley helps you to discover research relevant for your work.

Already have an account?

Save time finding and organizing research with Mendeley

Sign up for free