Enrique Vivoni

Dr. Enrique Vivoni

orcid

Research Focus & Metrics

Academic Career Length

31Years (1996-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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15 December 2000 in Journal of Geophysical Research: Oceans
Verified
Journal Article
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HNH. M. Nepf
H. M. Nepf
EVEnrique Vivoni
Enrique Vivoni

1 June 2016 in Journal of Hydrology
Verified
Journal Article
Closed access
SFSimone Fatichi
Simone Fatichi
EVEnrique Vivoni
Enrique Vivoni
FOFred L. Ogden
Fred L. Ogden
VIValeriy Y. Ivanov
Valeriy Y. Ivanov
BMBenjamin Mirus
Benjamin Mirus
DTDavid G Tarboton
David G Tarboton

20 June 2006 in Water Resources Research
Verified
Journal Article
Closed access
PDF file
BNBrent D. Newman
Brent D. Newman
Bradford WilcoxBradford Wilcox
Bradford Wilcox
SASteven R. Archer
Steven R. Archer
DBDavid D. Breshears
David D. Breshears
CDClifford N. Dahm
Clifford N. Dahm
EVEnrique Vivoni
Enrique Vivoni

27 November 2004 in Water Resources Research
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Journal Article
Closed access
PDF file
VIValeriy Y. Ivanov
Valeriy Y. Ivanov
EVEnrique Vivoni
Enrique Vivoni
RBRafael L. Bras
Rafael L. Bras
DEDara Entekhabi
Dara Entekhabi

1 February 2015 in Frontiers in Ecology and the Environment
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Journal Article
Closed access
GOGregory S Okin
Gregory S Okin
MHMariano Moreno De Las Heras
Mariano Moreno De Las Heras
PSPatricia M Saco
Patricia M Saco
HTHeather L Throop
Heather L Throop
EVEnrique Vivoni
Enrique Vivoni
DPDebra Pc Peters
Debra Pc Peters

18 November 2024 in Biogeosciences
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Journal Article
Open access
PDF file
JNJacob A. Nelson
Jacob A. Nelson
SWSophia Walther
Sophia Walther
FGFabian Gans
Fabian Gans
BKBasil Kraft
Basil Kraft
UWUlrich Weber
Ulrich Weber
MJMartin Jung
Martin Jung
Mapping in situ eddy covariance measurements of terrestrial land–atmosphere fluxes to the globe is a key method for diagnosing the Earth system from a data-driven perspective. We describe the first global products (called X-BASE) from a newly implemented upscaling framework, FLUXCOM-X, representing an advancement from the previous generation of FLUXCOM products in terms of flexibility and technical capabilities. The X-BASE products are comprised of estimates of CO2 net ecosystem exchange (NEE), gross primary productivity (GPP), evapotranspiration (ET), and for the first time a novel, fully data-driven global transpiration product (ETT), at high spatial (0.05°) and temporal (hourly) resolution. X-BASE estimates the global NEE at −5.75 ± 0.33 Pg C yr−1 for the period 2001–2020, showing a much higher consistency with independent atmospheric carbon cycle constraints compared to the previous versions of FLUXCOM. The improvement of global NEE was likely only possible thanks to the international effort to increase the precision and consistency of eddy covariance collection and processing pipelines, as well as to the extension of the measurements to more site years resulting in a wider coverage of bioclimatic conditions. However, X-BASE global net ecosystem exchange shows a very low interannual variability, which is common to state-of-the-art data-driven flux products and remains a scientific challenge. With 125 ± 2.1 Pg C yr−1 for the same period, X-BASE GPP is slightly higher than previous FLUXCOM estimates, mostly in temperate and boreal areas. X-BASE evapotranspiration amounts to 74.7×103 ± 0.9×103 km3 globally for the years 2001–2020 but exceeds precipitation in many dry areas, likely indicating overestimation in these regions. On average 57 % of evapotranspiration is estimated to be transpiration, in good agreement with isotope-based approaches, but higher than estimates from many land surface models. Despite considerable improvements to the previous upscaling products, many further opportunities for development exist. Pathways of exploration include methodological choices in the selection and processing of eddy covariance and satellite observations, their ingestion into the framework, and the configuration of machine learning methods. For this, the new FLUXCOM-X framework was specifically designed to have the necessary flexibility to experiment, diagnose, and converge to more accurate global flux estimates.