Preprints
https://doi.org/10.5194/essd-2025-456
https://doi.org/10.5194/essd-2025-456
13 Aug 2025
 | 13 Aug 2025
Status: this preprint is currently under review for the journal ESSD.

Energy-conservation datasets of global land surface radiation and heat fluxes from 2000–2020 generated by CoSEB

Junrui Wang, Ronglin Tang, Meng Liu, and Zhao-Liang Li

Abstract. Accurately estimating global land surface radiation [including downward shortwave radiation (SWIN), downward longwave radiation (LWIN), upward shortwave radiation (SWOUT), upward longwave radiation (LWOUT) and net radiation (Rn)] and heat fluxes [including latent heat flux (LE), soil heat flux (G) and sensible heat flux (H)] is essential for quantifying the exchange of radiation, heat and water between the land and atmosphere under global climate change. This study presents the first energy-conservation datasets of global land surface radiation and heat fluxes from 2000 to 2020, generated by our model of Coordinated estimates of land Surface Energy Balance components (CoSEB) that was renewed with a combination of GLASS and MODIS remote sensing data, ERA5-Land reanalysis datasets, topographic data, CO2 concentration data, and observations at 258 eddy covariance sites worldwide from the AmeriFlux, FLUXNET, EuroFlux, OzFlux, ChinaFLUX and TPDC. The developed CoSEB-based datasets are strikingly advantageous in that [1] they are the first RS-based global datasets that satisfy both surface radiation balance (SWIN - SWOUT + LWIN - LWOUT = Rn) and heat balance (LE + H + G = Rn) among the eight fluxes, as demonstrated by both the radiation imbalance ratio [RIR, defined as 100 % × (SWINSWOUT + LWIN - LWOUT)/Rn] and energy imbalance ratio [EIR, defined as 100 % × (Rn - G - LE - H)/Rn] of 0, [2] the radiation and heat fluxes are characterized by high accuracies, where (1) the RMSEs for daily estimates of SWIN, SWOUT, LWIN, LWOUT, Rn, LE, H and G from the CoSEB-based datasets were 28.51 W/m2, 10.39 W/m2, 14.29 W/m2, 10.62 W/m2, 22.40 W/m2, 24.38 W/m2, 22.67 W/m2 and 6.77 W/m2, respectively, as well as for 8-day estimates were 12.81 W/m2, 7.08 W/m2, 9.22 W/m2, 8.34 W/m2, 13.38 W/m2, 19.99 W/m2, 17.44 W/m2 and 4.25 W/m2, respectively, (2) the CoSEB-based datasets, in comparison to the mainstream products/datasets (i.e. GLASS, BESS-Rad, BESSV2.0, FLUXCOM, MOD16A2, PML_V2 and ETMonitor) that generally separately estimated subsets of the eight flux components, better agreed with the in situ observations. Our developed datasets hold significant potential for application across diverse fields such as agriculture, forestry, hydrology, meteorology, ecology, and environmental science, which can facilitate comprehensive studies on the variability, impacts, responses, adaptation strategies, and mitigation measures of global and regional land surface radiation and heat fluxes under the influences of climate change and human activities. The CoSEB-based datasets are open access and available through the National Tibetan Plateau Data Center (TPDC) at https://doi.org/10.11888/Terre.tpdc.302559 (Tang et al., 2025a) and through the Science Data Bank (ScienceDB) at https://doi.org/10.57760/sciencedb.27228 (Tang et al., 2025b).

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Junrui Wang, Ronglin Tang, Meng Liu, and Zhao-Liang Li

Status: open (until 19 Sep 2025)

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Junrui Wang, Ronglin Tang, Meng Liu, and Zhao-Liang Li

Data sets

Energy-conservation datasets of global land surface radiation and heat fluxes from 2000-2020 generated by CoSEB R. Tang et al. https://doi.org/10.11888/Terre.tpdc.302559

Energy-conservation datasets of global land surface radiation and heat fluxes from 2000-2020 generated by CoSEB R. Tang et al. https://doi.org/10.57760/sciencedb.27228

Junrui Wang, Ronglin Tang, Meng Liu, and Zhao-Liang Li

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Short summary
Existing remote sensing datasets could not provide all land-atmosphere radiation/heat flux components while satisfying energy balances. This study generates the first global dataset (2000–2020) based on our renewed Coordinated estimates of land Surface Energy Balance model, providing all high-accuracy components with perfect energy balance. This advancement enhances the study of Earth’s surface energy dynamics, enables better water management, and improves renewable energy planning.
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