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Atmospheric water balance in the Amazon basin: An isotopic evapotranspiration model

Gat, J. R., Matsui, E.·1991·Journal of Geophysical Research: Atmospheres

Abstract

An increase of 3‰ in the “d” value of the isotopic composition of precipitation over the Amazon Basin suggests that an isotopically fractionated evapotranspiration flux contributes to the atmospheric water balance over the region. A steady state evapotranspiration model for the Amazon Basin was developed, and it is shown that the observed increase in the “d” value corresponds to a situation where 20–40% of the total evapotranspiration flux is accompanied by an isotopic fractionation, such as by evaporation from an open water surface. The site of this fractionation, whether by evaporation from the flood plains, canopy interception or lakes, cannot be resolved with the presently available data set.

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Metadata

Authors
Gat, J. R., & Matsui, E.
Venue
Journal of Geophysical Research: Atmospheres
Published
1991-07-20
Volume
96
Issue
D7
Pages
13179-13188
ISSN
0148-0227 (ISSN-L)
OpenAlex
W2059872752
Cited by
405
References
0
FWCI
1.23
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: Atmospheric water balance in the Amazon basin: An isotopic evapotranspiration model. https://app.cochat.ai/papers/10.1029/91jd00054
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Gat, J. R., & Matsui, E. (1991). Atmospheric water balance in the Amazon basin: An isotopic evapotranspiration model. Journal of Geophysical Research: Atmospheres. https://doi.org/10.1029/91jd00054

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