@Article{BroedelVCNAKTCHT:2017:SiSuFl,
author = "Broedel, Elis{\^a}ngela and Von Randow, Celso and Cuartas, Luz
Adriana and Nobre, Ant{\^o}nio Donato and Ara{\'u}jo, Alessandro
Carioca de and Kruijt, Bart and Tourigny, Etienne and
C{\^a}ndido, Luiz Ant{\^o}nio and Hodnett, Martin and Tomasella,
Javier",
affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE)} and {Instituto
Nacional de Pesquisas Espaciais (INPE)} and {Centro Nacional de
Monitoramento de Desastres Naturais (CEMADEN)} and {Instituto
Nacional de Pesquisas da Amaz{\^o}nia (INPA)} and Embrapa and
{Wageningen University} and {Barcelona Supercomputing Center
(BSC)} and {Instituto Nacional de Pesquisas da Amaz{\^o}nia
(INPA)} and {Centre for Ecology and Hydrology} and {Instituto
Nacional de Pesquisas Espaciais (INPE)}",
title = "Simulation of Surface Fluxes in Two Distinct Environments along a
Topographic Gradient in a Central Amazonian Forest using the
INtegrated LAND Surface Model",
journal = "Hydrology and Earth System Sciences Discussions",
year = "2017",
volume = "2017",
pages = "1--49",
keywords = "Landscape heterogeneity, plateau, valley, land surface model,
water balance, 45 carbon balance, central Amazon, Terra Firme
forest soil and vegetation parameters.",
abstract = "The Integrated Land Surface model (INLAND) land surface model, in
offline mode, was 25 adjusted and forced with prescribed climate
to represent two contrasting environments along a 26 topographic
gradient in a central Amazon Terra Firme forest, which is
distinguished by well- 27 drained, flat plateaus and poorly
drained, broad river valleys. To correctly simulate the valley 28
area, a lumped unconfined aquifer model was included in the INLAND
model to represent the 29 water table dynamics and results show
reasonable agreement with observations. Field data 30 from both
areas are used to evaluate the model simulations of energy, water
and carbon 31 fluxes. The model is able to characterize with good
accuracy the main differences that appear 32 in the seasonal
energy and carbon partitioning of plateau and valley fluxes, which
are related 33 to features of the vegetation associated with soils
and topography. The simulated latent heat 34 flux (LE) and net
ecosystem exchange of carbon (NEE), for example, are higher on the
35 plateau area while at the bottom of the valley the sensible
heat flux (H) is noticeably higher 36 than at the plateau, in
agreement with observed data. Differences in simulated
hydrological 37 fluxes are also linked to the topography, showing
a higher surface runoff (R) and lower 38 evapotranspiration (ET)
in the valley area. The different behavior of the fluxes on both
annual and diurnal time scales confirms the benefit of a tiling
mechanism in the presence of large 40 contrast and the importance
to incorporate subgrid-scale variability by including relief 41
attributes of topography, soil and vegetation to better
representing Terra Firme forests in 42 land surface models.",
doi = "10.5194/hess-2017-203",
url = "http://dx.doi.org/10.5194/hess-2017-203",
issn = "1812-2108",
language = "en",
targetfile = "broedel_simulation.pdf",
urlaccessdate = "04 maio 2024"
}