Significant albedo-induced cooling effects across tropical and subtropical dryland biomes
- 1Beijing Normal University
- 2Chinese Academy of Sciences
Abstract
Terrestrial ecosystems can significantly regulate climate through carbon uptake and alterations in surface albedo. However, current climate mitigation assessments largely focus on carbon sinks while overlooking albedo-induced radiative effects. We developed an integrated framework to quantify the net climate effect of global terrestrial ecosystems from 2001 to 2019 by combining net ecosystem productivity with albedo-induced radiative forcing. We estimated the Net Equivalent Carbon Dioxide Stock Change (NESC), which incorporates both Net Cumulative Carbon uptake Equivalent (NCCE) and the Emission Equivalent of Shortwave Forcing (EESF). Results show that global terrestrial ecosystems generated a net cooling effect of 397.52 Gt CO2e during the study period. Among biomes, tropical and subtropical grasslands, savannas and shrublands, and deserts and xeric shrublands, contributed a cooling effect of 95.33 Gt CO2e due to increased albedo, nearly one-quarter of the total NCCE across the 14 biomes, largely driven by declines in photosynthetic vegetation and soil drying in Land use and land cover (LULC) non-conversion areas. These findings provide new perspectives for re-evaluating the climate value of terrestrial ecosystems and a scientific basis for incorporating surface albedo into future nature-based solutions for climate mitigation.
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BibTeX
@article{pei2026significant,
title = {{Significant albedo-induced cooling effects across tropical and subtropical dryland biomes}},
author = {Hongze Pei and Jieming Chou and Chaoyang Wang and Jingwen Liu and Haofeng Jin and Peng Zhou and Yaqi Wang and Hao Guo and Yuanmeng Li and Weixing Zhao and Jiawen Zhu},
journal = {Environmental Research Letters},
year = {2026},
month = nov,
doi = {10.1088/1748-9326/aebd00},
url = {https://iopscience.iop.org/article/10.1088/1748-9326/aebd00},
note = {CC BY 4.0},
}
RIS
TY - JOUR
TI - Significant albedo-induced cooling effects across tropical and subtropical dryland biomes
AU - Hongze Pei
AU - Jieming Chou
AU - Chaoyang Wang
AU - Jingwen Liu
AU - Haofeng Jin
AU - Peng Zhou
AU - Yaqi Wang
AU - Hao Guo
AU - Yuanmeng Li
AU - Weixing Zhao
AU - Jiawen Zhu
PY - 2026
DA - 2026/11/03
JO - Environmental Research Letters
DO - 10.1088/1748-9326/aebd00
UR - https://iopscience.iop.org/article/10.1088/1748-9326/aebd00
AB - Terrestrial ecosystems can significantly regulate climate through carbon uptake and alterations in surface albedo. However, current climate mitigation assessments largely focus on carbon sinks while overlooking albedo-induced radiative effects. We developed an integrated framework to quantify the net climate effect of global terrestrial ecosystems from 2001 to 2019 by combining net ecosystem productivity with albedo-induced radiative forcing. We estimated the Net Equivalent Carbon Dioxide Stock Change (NESC), which incorporates both Net Cumulative Carbon uptake Equivalent (NCCE) and the Emission Equivalent of Shortwave Forcing (EESF). Results show that global terrestrial ecosystems generated a net cooling effect of 397.52 Gt CO2e during the study period. Among biomes, tropical and subtropical grasslands, savannas and shrublands, and deserts and xeric shrublands, contributed a cooling effect of 95.33 Gt CO2e due to increased albedo, nearly one-quarter of the total NCCE across the 14 biomes, largely driven by declines in photosynthetic vegetation and soil drying in Land use and land cover (LULC) non-conversion areas. These findings provide new perspectives for re-evaluating the climate value of terrestrial ecosystems and a scientific basis for incorporating surface albedo into future nature-based solutions for climate mitigation.
SN - 1748-9326
ER -