Improvement in the Estimation of Daily Net Surface Radiation in China

Xiao, Mingzhong; Kong, Dongdong

doi:10.1061/(asce)ir.1943-4774.0001539

J. Irrig. Drain Eng.

2021

DOI: 10.1061/(asce)ir.1943-4774.0001539

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Improvement in the Estimation of Daily Net Surface Radiation in China

Mingzhong Xiao

Dongdong Kong

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Cited by 4 publications

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Evapotranspiration (ET) dominates land surface water resource availability and net radiation partition, which is a vital component in the water and energy cycles on the global scale (Wang & Dickinson, 2012;Xiao & Kong, 2021), where about 58%-65% of precipitation back to the atmosphere through ET, and about 51%-58% of land surface net radiation is consumed by ET (also known as latent heat flux) (Brutsaert, 2005;Held & Soden, 2006). Under the warming climate, the hydrological cycle is expected to intensify (Held & Soden, 2006), and terrestrial ET should increase (Allan et al, 2020).

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Contributions of Anthropogenic Forcings to Evapotranspiration Changes Over 1980–2020 Using GLEAM and CMIP6 Simulations

et al. 2021

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Anthropogenic impacts on terrestrial evapotranspiration (ET) changes during 1980–2020 were evaluated based on newly released observed‐based GLEAM ET and Coupled Model Intercomparison Project Phase 6 (CMIP6) through optional fingerprint method. Global assessments show that anthropogenic forcings dominate the increasing ET trend, other than natural forcing (NAT). On the global scale, anthropogenic forcings explain ∼84.2% of the observed ET trend, while the signal of natural forcing cannot be detected. Among anthropogenic forcings, greenhouse gases (GHG) are the primary driving factor for ET changes, and GHG‐only has already explained ∼78.8% of the observed ET trend. This study for the first time demonstrates that the GHG signal can be detected in the observed‐based ET and can be separable from NAT and aerosol (AER) signals. At the regional scale, CMIP6 simulations work well in North Hemisphere, but are deficient in South Hemisphere. GHG still dominates ET changes in the North Hemisphere, except for Europe, where the influence of AER forcing stands out, and attributable changes to AER is 2.4 times of GHG. Our first quantitative detection and attribution of ET contribute to advance the understanding of anthropogenic activities on hydrological cycle changes.

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Contributions of Anthropogenic Forcings to Evapotranspiration Changes Over 1980–2020 Using GLEAM and CMIP6 Simulations

et al. 2021

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Investigating the role of two-dimensional and three-dimensional urban structures in seasonal surface radiation budget

Chen,

Cao,

et al. 2025

Building and Environment

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A hybrid optimized model for predicting evapotranspiration in early and late rice based on a categorical regression tree combination of key influencing factors

Zhao,

Qing,

Bai

et al. 2023

Computers and Electronics in Agriculture

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Improvement in the Estimation of Daily Net Surface Radiation in China

Cited by 4 publications

References 31 publications

Contributions of Anthropogenic Forcings to Evapotranspiration Changes Over 1980–2020 Using GLEAM and CMIP6 Simulations

Contributions of Anthropogenic Forcings to Evapotranspiration Changes Over 1980–2020 Using GLEAM and CMIP6 Simulations

Investigating the role of two-dimensional and three-dimensional urban structures in seasonal surface radiation budget

A hybrid optimized model for predicting evapotranspiration in early and late rice based on a categorical regression tree combination of key influencing factors

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