Land–atmosphere interactions in the tropics – a review

Gentine, Pierre; Massmann, Adam; Lintner, Benjamin R.; Hamed Alemohammad, Sayed; Fu, Rong; Green, Julia K.; Kennedy, Daniel; Vilà-Guerau de Arellano, Jordi

doi:10.5194/hess-23-4171-2019

Land–atmosphere interactions in the tropics – a review

Journal Article · Thu Oct 17 00:00:00 EDT 2019 · Hydrology and Earth System Sciences (Online)

DOI:https://doi.org/10.5194/hess-23-4171-2019· OSTI ID:1802206

Gentine, Pierre ^[1]; Massmann, Adam ^[2]; Lintner, Benjamin R. ^[3]; ^[2]; Fu, Rong ^[4]; Green, Julia K. ^[2]; ^[2]; ^[5]

Columbia Univ., New York, NY (United States). Earth Inst. Dept. of Earth and Environmental Engineering; OSTI
Columbia Univ., New York, NY (United States). Earth Inst. Dept. of Earth and Environmental Engineering
Rutgers Univ., New Brunswick, NJ (United States). Dept. of Environmental Sciences
Univ. of California, Los Angeles, CA (United States). Dept. of Atmospheric and Ocean Sciences
Wageningen Univ. (Netherlands). Meteorology and Air Quality Group

The continental tropics play a leading role in the terrestrial energy,water, and carbon cycles. Land–atmosphere interactions are integral in the regulation of these fluxes across multiple spatial and temporal scales over tropical continents. We review here some of the important characteristics of tropical continental climates and how land–atmosphere interactions regulate them. Along with a wide range of climates, the tropics manifest a diverse array of land–atmosphere interactions. Broadly speaking, in tropical rainforest climates, light and energy are typically more limiting than precipitation and water supply for photosynthesis and evapo transpiration (ET),whereas in savanna and semi-arid climates, water is the critical regulator of surface fluxes and land–atmosphere interactions. We discuss the impact of the land surface, how it affects shallow and deep clouds, and how these clouds in turn can feed back to the surface by modulating surface radiation and precipitation. Some results from recent research suggest that shallow clouds may be especially critical to land–atmosphere interactions. On the other hand, the impact of land-surface conditions on deep convection appears to occur over larger, non local scales and may be a more relevantl and–atmosphere feedback mechanism in transitional dry-to-wet regions and climate regimes.

View Accepted Manuscript (DOE)

Research Organization:: Columbia Univ., New York, NY (United States)

Sponsoring Organization:: USDOE Office of Science (SC)

Grant/Contract Number:: SC0011094; SC0014203

OSTI ID:: 1802206

Journal Information:: Hydrology and Earth System Sciences (Online), Journal Name: Hydrology and Earth System Sciences (Online) Journal Issue: 10 Vol. 23; ISSN 1607-7938

Publisher:: European Geosciences Union (EGU)Copyright Statement

Country of Publication:: United States

Language:: English

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