@Article{Restrepo-CoupeALBLMACCFGIMVZMS:2021:LeObIn,
author = "Restrepo-Coupe, Nat{\'a}lia and Albert, Loren P. and Longo,
Marcos and Baker, Ian and Levine, Naomi M. and Mercado, Lina M.
and Ara{\'u}jo, Alessandro C. da and Christofferson, Bradley
O'Donnell and Costa, Marcos H. and Fitzjarrald, David R. and
Galbraith, David and Imbuzeiro, Hewlley and Malhi, Yadvinder and
Von Randow, Celso and Zeng, Xubin and Moorcroft, Paul and Saleska,
Scott R.",
affiliation = "{University of Arizona} and {University of Arizona} and {Harvard
University} and {Colorado State University} and {Harvard
University} and {University of Exeter} and {Embrapa Amaz{\^o}nia
Oriental} and {University of Texas Rio Grande Valley} and
{Universidade Federal de Vi{\c{c}}osa (UFV)} and {University at
Albany} and {University of Leeds} and {Universidade Federal de
Vi{\c{c}}osa (UFV)} and {University of Oxford} and {Instituto
Nacional de Pesquisas Espaciais (INPE)} and {University of
Arizona} and {California Institute of Technology} and {University
of Arizona}",
title = "Understanding water and energy fluxes in the Amazonia: Lessons
from an observation-model intercomparison",
journal = "Global Change Biology",
year = "2021",
volume = "27",
number = "9",
pages = "1802--1819",
month = "Mar.",
keywords = "Amazonia, climate interactions, ecosystem, eddy covariance flux
seasonality, energy balance, evapotranspiration, land surface
models, tropical forests.",
abstract = "Tropical forests are an important part of global water and energy
cycles, but the mechanisms that drive seasonality of their
land-atmosphere exchanges have proven challenging to capture in
models. Here, we (1) report the seasonality of fluxes of latent
heat (LE), sensible heat (H), and outgoing short and longwave
radiation at four diverse tropical forest sites across
Amazonia-along the equator from the Caxiuana and Tapajos National
Forests in the eastern Amazon to a forest near Manaus, and from
the equatorial zone to the southern forest in Reserva Jaru; (2)
investigate how vegetation and climate influence these fluxes; and
(3) evaluate land surface model performance by comparing
simulations to observations. We found that previously identified
failure of models to capture observed dry-season increases in
evapotranspiration (ET) was associated with model overestimations
of (1) magnitude and seasonality of Bowen ratios (relative to
aseasonal observations in which sensible was only 20%-30% of the
latent heat flux) indicating model exaggerated water limitation,
(2) canopy emissivity and reflectance (albedo was only 10%-15% of
incoming solar radiation, compared to 0.15%-0.22% simulated), and
(3) vegetation temperatures (due to underestimation of dry-season
ET and associated cooling). These partially compensating
model-observation discrepancies (e.g., higher temperatures
expected from excess Bowen ratios were partially ameliorated by
brighter leaves and more interception/evaporation) significantly
biased seasonal model estimates of net radiation (R-n), the key
driver of water and energy fluxes (LE similar to 0.6 R-n and H
similar to 0.15 R-n), though these biases varied among sites and
models. A better representation of energy-related parameters
associated with dynamic phenology (e.g., leaf optical properties,
canopy interception, and skin temperature) could improve
simulations and benchmarking of current vegetation-atmosphere
exchange and reduce uncertainty of regional and global
biogeochemical models.",
doi = "10.1111/gcb.15555",
url = "http://dx.doi.org/10.1111/gcb.15555",
issn = "1354-1013",
language = "en",
targetfile = "coupe_understanding.pdf",
urlaccessdate = "29 jun. 2024"
}