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Title: Partitioning evapotranspiration using long‐term carbon dioxide and water vapor fluxes

Journal Article · · Geophysical Research Letters
DOI:https://doi.org/10.1002/2017GL074324· OSTI ID:1390369

Abstract The separate components of evapotranspiration (ET) elucidate the pathways and time scales over which water is returned to the atmosphere, but ecosystem‐scale measurements of transpiration ( T ) and evaporation ( E ) remain elusive. We propose a novel determination of E and T using multiyear eddy covariance estimates of ET and gross ecosystem photosynthesis (GEP). The method is applicable at water‐limited sites over time periods during which a linear regression between GEP (abscissa) and ET (ordinate) yields a positive ET axis intercept, an estimate of E . At four summer‐rainfall semiarid sites, T /ET increases to a peak coincident with maximum GEP and remains elevated as the growing season progresses, consistent with previous, direct measurements. The seasonal course of T /ET is related to increasing leaf area index and declining frequency of rainy days—an index of the wet surface conditions that promote E —suggesting both surface and climatic controls on ET partitioning.

Sponsoring Organization:
USDOE
OSTI ID:
1390369
Journal Information:
Geophysical Research Letters, Journal Name: Geophysical Research Letters Vol. 44 Journal Issue: 13; ISSN 0094-8276
Publisher:
American Geophysical Union (AGU)Copyright Statement
Country of Publication:
United States
Language:
English
Citation Metrics:
Cited by: 85 works
Citation information provided by
Web of Science

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