Amazon Rainforest Exchange of Carbon and Subcanopy Air Flow: Manaus LBA Site-A Complex Terrain Condition


Autoria(s): Tota, Julio; Fitzjarrald, David Roy; da Silva Dias, Maria A. F.
Contribuinte(s)

UNIVERSIDADE DE SÃO PAULO

Data(s)

05/11/2013

05/11/2013

2012

Resumo

On the moderately complex terrain covered by dense tropical Amazon Rainforest (Reserva Biologica do Cuieiras-ZF2-02 degrees 36'17.1 '' S, 60 degrees 12'24.4 '' W), subcanopy horizontal and vertical gradients of the air temperature, CO2 concentration and wind field were measured for the dry and wet periods in 2006. We tested the hypothesis that horizontal drainage flow over this study area is significant and can affect the interpretation of the high carbon uptake rates reported by previous works at this site. A similar experimental design as the one by Tota et al. (2008) was used with a network of wind, air temperature, and CO2 sensors above and below the forest canopy. A persistent and systematic subcanopy nighttime upslope (positive buoyancy) and daytime downslope (negative buoyancy) flow pattern on a moderately inclined slope (12%) was observed. The microcirculations observed above the canopy (38 m) over the sloping area during nighttime presents a downward motion indicating vertical convergence and correspondent horizontal divergence toward the valley area. During the daytime an inverse pattern was observed. The microcirculations above the canopy were driven mainly by buoyancy balancing the pressure gradient forces. In the subcanopy space the microcirculations were also driven by the same physical mechanisms but probably with the stress forcing contribution. The results also indicated that the horizontal and vertical scalar gradients (e. g., CO2) were modulated by these micro-circulations above and below the canopy, suggesting that estimates of advection using previous experimental approaches are not appropriate due to the tridimensional nature of the vertical and horizontal transport locally. This work also indicates that carbon budget from tower-based measurement is not enough to close the system, and one needs to include horizontal and vertical advection transport of CO2 into those estimates.

NASA Terrestrial Ecology Branch

NASA Terrestrial Ecology Branch [NCC5-283, NNG-06GE09A]

FAPEAM RHPOSGRAD

FAPEAM RH-POSGRAD

MCTINPA

MCT-INPA

Fundacao Djalma Batista

Fundacao Djalma Batista

Identificador

SCIENTIFIC WORLD JOURNAL, NEW YORK, v. 52, n. 12, supl. 1, Part 6, pp. 2654-2663, DEC, 2012

1537-744X

http://www.producao.usp.br/handle/BDPI/41236

10.1100/2012/165067

http://dx.doi.org/10.1100/2012/165067

Idioma(s)

eng

Publicador

HINDAWI PUBLISHING CORPORATION

NEW YORK

Relação

SCIENTIFIC WORLD JOURNAL

Direitos

openAccess

Copyright HINDAWI PUBLISHING CORPORATION

Palavras-Chave #EDDY COVARIANCE #ALPINE FOREST #LONG-TERM #MICROMETEOROLOGICAL OBSERVATIONS #TALL VEGETATION #DIOXIDE FLUXES #HILLY TERRAIN #CO2 ADVECTION #WATER-VAPOR #CANOPY #MULTIDISCIPLINARY SCIENCES
Tipo

article

original article

publishedVersion