Decreased dust particles amplify the cloud cooling effect by regulating cloud ice formation over the Tibetan Plateau

Ice-nucleating particles (INPs) can initiate cloud ice formation, influencing cloud radiative effects (CRE) and climate. However, the knowledge of INP sources, concentrations, and their impact on CRE over the Tibetan Plateau (TP)-a highly climate-sensitive region-remains largely hypothetical. Here, we integrated data from multisource satellite observations and snowpack samples collected from five glaciers to demonstrate that dust particles constitute primary INP sources over the TP. The springtime dust influxes lead to seasonally elevated ice concentrations in mixed-phase clouds. Furthermore, the decadal reduction in dustiness from 2007 to 2019 results in decreased springtime dust INPs, thereby amplifying the cooling effect of clouds over the TP, with a 1.98 ± 0.39-watt per square meter reduction in surface net CRE corresponding to a 0.01 decrease in dust optical depth. Our findings elucidate previously unidentified pathways of climate feedback from an atmospheric INP perspective, especially highlighting the crucial role of dust in aerosol-cloud interactions.

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Publication Details

Journal
Science Advances
Published
2024-09-13
DOI
https://doi.org/10.1126/sciadv.ado0885
Citations
15
Primary Topic
Atmospheric aerosols and clouds
Type
article
Field-Weighted Citation Impact
4.24
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article

Decreased dust particles amplify the cloud cooling effect by regulating cloud ice formation over the Tibetan Plateau

X P Meng, Zhijun Wu, Lixiang Zhai, Chuanfeng Zhao et al.
15 citations
Science Advances
Atmospheric aerosols and clouds
4.24
article

Decreased dust particles amplify the cloud cooling effect by regulating cloud ice formation over the Tibetan Plateau

X P Meng, Zhijun Wu, Lixiang Zhai, Chuanfeng Zhao, Min Hu, Shao‐Meng Li, Yan Yu, Paul Ginoux, Paul J. DeMott, Tong Fei Zhu, Rui Xu, Jianzhong Xu, Yafei Yan, Jingchuan Chen
article en
15 citations

Abstract

Ice-nucleating particles (INPs) can initiate cloud ice formation, influencing cloud radiative effects (CRE) and climate. However, the knowledge of INP sources, concentrations, and their impact on CRE over the Tibetan Plateau (TP)-a highly climate-sensitive region-remains largely hypothetical. Here, we integrated data from multisource satellite observations and snowpack samples collected from five glaciers to demonstrate that dust particles constitute primary INP sources over the TP. The springtime dust influxes lead to seasonally elevated ice concentrations in mixed-phase clouds. Furthermore, the decadal reduction in dustiness from 2007 to 2019 results in decreased springtime dust INPs, thereby amplifying the cooling effect of clouds over the TP, with a 1.98 ± 0.39-watt per square meter reduction in surface net CRE corresponding to a 0.01 decrease in dust optical depth. Our findings elucidate previously unidentified pathways of climate feedback from an atmospheric INP perspective, especially highlighting the crucial role of dust in aerosol-cloud interactions.

Science AdvancesVol. 10(37)
Shanghai Jiao Tong University (CN), NOAA Geophysical Fluid Dynamics Laboratory (US), Chinese Academy of Sciences (CN), Nanjing University of Information Science and Technology (CN), Peking University (CN), Shanghai Normal University (CN), Northwest Institute of Eco-Environment and Resources (CN), State Key Joint Laboratory of Environment Simulation and Pollution Control (CN), Colorado State University (US)
Climate action
Openalex Percentile: Top 5%
Atmospheric aerosols and clouds
4.24
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