The Contribution of Ephemeral Lakes to Global Dust Cycle and Direct Radiative Effect

Abstract Despite their tiny size, ephemeral lakes with their dry smooth surface may play a major role in the dust life cycle at global scale. However, their impacts on Earth's climate systems, and in particular direct radiative effects have been unexplored. Our results show that ephemeral lakes contribute as much as 52% of dust emission in the Southern Hemisphere (SH), but only 10% in the Northern Hemisphere and 13% globally. Due to the action of physical processes, dust mineralogy of the lakes differs from their surroundings. With no reliable data sets, we performed a sensitivity analysis of dust absorption. With increasing absorption from lakes, lake dust's radiative cooling decreases from −0.1 to −0.03 Wm −2 , globally. These findings highlight the dominant role of ephemeral lakes in the SH dust budget and underscore the need to include them in climate models to better represent dust‐radiation interactions and ocean biogeochemical feedback.

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Publication Details

Journal
Geophysical Research Letters
Published
2025-09-09
DOI
https://doi.org/10.1029/2025gl116689
Citations
1
Primary Topic
Atmospheric chemistry and aerosols
Type
article
Field-Weighted Citation Impact
1.30

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article

The Contribution of Ephemeral Lakes to Global Dust Cycle and Direct Radiative Effect

Paul Ginoux, Q. Q. Song
1 citations
Geophysical Research Letters
Atmospheric chemistry and aerosols
1.30
article

The Contribution of Ephemeral Lakes to Global Dust Cycle and Direct Radiative Effect

Paul Ginoux, Q. Q. Song
article en
1 citations

Abstract

Abstract Despite their tiny size, ephemeral lakes with their dry smooth surface may play a major role in the dust life cycle at global scale. However, their impacts on Earth's climate systems, and in particular direct radiative effects have been unexplored. Our results show that ephemeral lakes contribute as much as 52% of dust emission in the Southern Hemisphere (SH), but only 10% in the Northern Hemisphere and 13% globally. Due to the action of physical processes, dust mineralogy of the lakes differs from their surroundings. With no reliable data sets, we performed a sensitivity analysis of dust absorption. With increasing absorption from lakes, lake dust's radiative cooling decreases from −0.1 to −0.03 Wm −2 , globally. These findings highlight the dominant role of ephemeral lakes in the SH dust budget and underscore the need to include them in climate models to better represent dust‐radiation interactions and ocean biogeochemical feedback.

Geophysical Research LettersVol. 52(17)
NOAA Geophysical Fluid Dynamics Laboratory (US), Princeton University (US), University of Maryland, Baltimore County (US)
National Aeronautics and Space Administration, U.S. Department of Commerce, National Oceanic and Atmospheric Administration
Openalex Percentile: Top 18%
Atmospheric chemistry and aerosols
1.30
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