Evapotranspiration in the Amazon: spatial patterns, seasonality, and recent trends in observations, reanalysis, and climate models
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Published:2021-04-28
Issue:4
Volume:25
Page:2279-2300
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ISSN:1607-7938
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Container-title:Hydrology and Earth System Sciences
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language:en
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Short-container-title:Hydrol. Earth Syst. Sci.
Author:
Baker Jessica C. A.ORCID, Garcia-Carreras LuisORCID, Gloor Manuel, Marsham John H.ORCID, Buermann Wolfgang, da Rocha Humberto R., Nobre Antonio D., de Araujo Alessandro CariocaORCID, Spracklen Dominick V.
Abstract
Abstract. Water recycled through transpiring forests influences the
spatial distribution of precipitation in the Amazon and has been shown to
play a role in the initiation of the wet season. However, due to the
challenges and costs associated with measuring evapotranspiration (ET)
directly and high uncertainty in remote-sensing
ET retrievals, the spatial and temporal patterns in Amazon ET remain poorly
understood. In this study, we estimated ET over the Amazon and 10
sub-basins using a catchment-balance approach, whereby ET is calculated
directly as the balance between precipitation, runoff, and change in
groundwater storage. We compared our results with ET from remote-sensing
datasets, reanalysis, models from Phase 5 and Phase 6 of the Coupled Model
Intercomparison Projects (CMIP5 and CMIP6 respectively), and in situ flux tower measurements to provide a comprehensive overview of current understanding. Catchment-balance analysis revealed a gradient in ET from east to west/southwest across the Amazon Basin, a strong seasonal cycle in
basin-mean ET primarily controlled by net incoming radiation, and no trend
in ET over the past 2 decades. This approach has a degree of uncertainty,
due to errors in each of the terms of the water budget; therefore, we
conducted an error analysis to identify the range of likely values.
Satellite datasets, reanalysis, and climate models all tended to overestimate
the magnitude of ET relative to catchment-balance estimates, underestimate
seasonal and interannual variability, and show conflicting positive and
negative trends. Only two out of six satellite and model datasets analysed
reproduced spatial and seasonal variation in Amazon ET, and captured the
same controls on ET as indicated by catchment-balance analysis. CMIP5 and
CMIP6 ET was inconsistent with catchment-balance estimates over all scales
analysed. Overall, the discrepancies between data products and models
revealed by our analysis demonstrate a need for more ground-based ET
measurements in the Amazon as well as a need to substantially improve model
representation of this fundamental component of the Amazon hydrological
cycle.
Funder
European Research Council Natural Environment Research Council
Publisher
Copernicus GmbH
Subject
General Earth and Planetary Sciences,General Engineering,General Environmental Science
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