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Alexander J Winkler

Biographic Data

ID6821677
NAMEAlexander J Winkler
GIVEN NAMESAlexander J
FAMILY NAMEWinkler
SIGNATUREWINKLER A J
AFFILIATIONSMax Planck Institute for Biogeochemistry
ORCID0000-0001-6574-4471
VERIFIEDYes
TOTAL WORKS3
TOTAL CITATIONS0
AUTHOR COUNT3
EDITOR COUNT0
FIRST PUBLICATION YEAR2023
LATEST PUBLICATION YEAR2026
H-INDEX0
  • A theoretical framework for critical canopy temperature and its application to improve remote-sensing-based estimation of evapotranspiration

    Open Access•Zhe Shi, Wenli Zhao et al.•ARTICLE•Environmental Research Letters•2026

    Surface energy balance (SEB) models are widely employed for remote-sensing-based evapotranspiration estimation. A critical parameter in most SEB models is the surface temperature of wet or dry boundaries where sensible heat ( H ) or latent heat (LE) equals 0, which is difficult to measure or estimate. The wide application of SEB models is seriously limited due to this challenge. Therefore, this study introduces ‘critical canopy temperature ( T cc…

  • Precipitation leads the long-term vegetation increase in the conterminous United States drylands

    Open Access•Yang Chang, Yuhe Chang et al.•ARTICLE•Environmental Research Letters•2025

    Drylands, encompassing over 40% of the conterminous United States (CONUS), are crucial to the global carbon cycle and highly susceptible to climate change. However, Earth system models offer conflicting projections of future drought and vegetation activity in North America, and in-depth analyses of the long-term changes in greenness and its relationship with underlying climate drivers, considering both spatial and temporal variations at the ecosy…

  • Hybrid modeling of evapotranspiration: Inferring stomatal and aerodynamic resistances using combined physics-based and machine learning

    Open Access•Reda ElGhawi, Basil Kraft et al.•ARTICLE•Environmental Research Letters•2023

    The process of evapotranspiration transfers liquid water from vegetation and soil surfaces to the atmosphere, the so-called latent heat flux ( Q LE ), and modulates the Earth’s energy, water, and carbon cycle. Vegetation controls Q LE by regulating leaf stomata opening (surface resistance r s in the Big Leaf approach) and by altering surface roughness (aerodynamic resistance r a ). Estimating r s and r a across different vegetation types is a key…

No prominent works on this page.

  • Hybrid modeling of evapotranspiration: Inferring stomatal and aerodynamic resistances using combined physics-based and machine learning

    Open Access•Reda ElGhawi, Basil Kraft et al.•ARTICLE•Environmental Research Letters•2023

    The process of evapotranspiration transfers liquid water from vegetation and soil surfaces to the atmosphere, the so-called latent heat flux ( Q LE ), and modulates the Earth’s energy, water, and carbon cycle. Vegetation controls Q LE by regulating leaf stomata opening (surface resistance r s in the Big Leaf approach) and by altering surface roughness (aerodynamic resistance r a ). Estimating r s and r a across different vegetation types is a key…

  • Precipitation leads the long-term vegetation increase in the conterminous United States drylands

    Open Access•Yang Chang, Yuhe Chang et al.•ARTICLE•Environmental Research Letters•2025

    Drylands, encompassing over 40% of the conterminous United States (CONUS), are crucial to the global carbon cycle and highly susceptible to climate change. However, Earth system models offer conflicting projections of future drought and vegetation activity in North America, and in-depth analyses of the long-term changes in greenness and its relationship with underlying climate drivers, considering both spatial and temporal variations at the ecosy…

  • A theoretical framework for critical canopy temperature and its application to improve remote-sensing-based estimation of evapotranspiration

    Open Access•Zhe Shi, Wenli Zhao et al.•ARTICLE•Environmental Research Letters•2026

    Surface energy balance (SEB) models are widely employed for remote-sensing-based evapotranspiration estimation. A critical parameter in most SEB models is the surface temperature of wet or dry boundaries where sensible heat ( H ) or latent heat (LE) equals 0, which is difficult to measure or estimate. The wide application of SEB models is seriously limited due to this challenge. Therefore, this study introduces ‘critical canopy temperature ( T cc…

Plant Water Relations and Carbon Dynamics (2 works) · Algorithm (1 works) · Artificial Intelligence (1 works) · Atmospheric sciences (1 works) · Bowen ratio (1 works) · Canopy (1 works) · Climatology (1 works) · Closure (psychology (1 works) · Computer Science (1 works) · Energy balance (1 works)

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