Patterns of water and heat flux across a biome gradient from tropical forest to savanna in Brazil


Autoria(s): Rocha, Humberto Ribeiro da; MANZI, Antonio O.; CABRAL, Osvaldo M.; MILLER, Scott D.; GOULDEN, Michael L.; SALESKA, Scott R.; COUPE, Natalia R.; WOFSY, Steven C.; Borma, Laura de Simone; Artaxo Netto, Paulo Eduardo; VOURLITIS, George; NOGUEIRA, Jose S.; CARDOSO, Fernando L.; NOBRE, Antonio D.; KRUIJT, Bart; Freitas, Helber Custodio de; RANDOW, Celso von; AGUIAR, Renata G.; MAIA, Jair F.
Contribuinte(s)

UNIVERSIDADE DE SÃO PAULO

Data(s)

20/10/2012

20/10/2012

2009

Resumo

We investigated the seasonal patterns of water vapor and sensible heat flux along a tropical biome gradient from forest to savanna. We analyzed data from a network of flux towers in Brazil that were operated within the Large-Scale Biosphere-Atmosphere Experiment in Amazonia (LBA). These tower sites included tropical humid and semideciduous forest, transitional forest, floodplain (with physiognomies of cerrado), and cerrado sensu stricto. The mean annual sensible heat flux at all sites ranged from 20 to 38 Wm(-2), and was generally reduced in the wet season and increased in the late dry season, coincident with seasonal variations of net radiation and soil moisture. The sites were easily divisible into two functional groups based on the seasonality of evaporation: tropical forest and savanna. At sites with an annual precipitation above 1900 mm and a dry season length less than 4 months (Manaus, Santarem and Rondonia), evaporation rates increased in the dry season, coincident with increased radiation. Evaporation rates were as high as 4.0 mm d(-1) in these evergreen or semidecidous forests. In contrast, ecosystems with precipitation less than 1700 mm and a longer dry season (Mato Grosso, Tocantins and Sao Paulo) showed clear evidence of reduced evaporation in the dry season. Evaporation rates were as low as 2.5 mm d(-1) in the transitional forests and 1 mm d(-1) in the cerrado. The controls on evapotranspiration seasonality changed along the biome gradient, with evaporative demand (especially net radiation) playing a more important role in the wetter forests, and soil moisture playing a more important role in the drier savannah sites.

LBA scientific committee

LBA scientific committee

Ministério da Ciência, Tecnologia e Inovação do Brasil (MCTI)

Brazilian Ministry of Science and Technology

Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

Fapesp[02/09289-9]

CNPq

Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)

Financiadora de Estudos e Projetos (FINEP)

Finep

NASA/LBA-Eco coordination and staff

NASA/LBA-Eco coordination and staff

Identificador

JOURNAL OF GEOPHYSICAL RESEARCH, v.114, 2009

0148-0227

http://producao.usp.br/handle/BDPI/29064

10.1029/2007JG000640

http://dx.doi.org/10.1029/2007JG000640

Idioma(s)

eng

Publicador

AMER GEOPHYSICAL UNION

Relação

Journal of Geophysical Research

Direitos

restrictedAccess

Copyright AMER GEOPHYSICAL UNION

Palavras-Chave #HYDROLOGIC-CYCLE #AMAZON FORESTS #CARBON #DYNAMICS #Environmental Sciences #Geosciences, Multidisciplinary
Tipo

article

original article

publishedVersion