Why Does the Norwegian Sea‐Barents Sea Region Have the Smallest Amount of Stratocumulus in Summer?

Abstract The melting of sea ice in the Arctic has sparked research into how clouds form in exposed ice‐free zones. This study delves into the seasonal distribution of stratocumulus clouds over the Norwegian Sea‐Barents Sea region and presents a conceptual model for the underlying mechanisms. In spring, autumn, and winter, increased surface water vapor flux provides water vapor from the sea surface. Concurrently, warm air enters the area through the southwest wind of the Norwegian Strait. Under conditions of unstable stratification, the water vapor is lifted to the condensation level, promoting the formation of stratocumulus clouds. Conversely, in summer, evaporation is suppressed due to stable stratification, which hinders vertical vapor transport. Enhanced dry advection reduces the transport of water vapor, leading to a decrease in the amount of stratocumulus clouds during summer. This research enriches our understanding of the physical mechanisms influencing cloud formation and cloud‐climate feedbacks in the Arctic region.

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Publication Details

Journal
Geophysical Research Letters
Published
2025-10-16
DOI
https://doi.org/10.1029/2025gl116907
Primary Topic
Atmospheric chemistry and aerosols
Type
article
Field-Weighted Citation Impact
0.00

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article

Why Does the Norwegian Sea‐Barents Sea Region Have the Smallest Amount of Stratocumulus in Summer?

Chen Zhou, Wenrong Bai, Naifu Shao, Lei Zhu et al.
Geophysical Research Letters
Atmospheric chemistry and aerosols
article

Why Does the Norwegian Sea‐Barents Sea Region Have the Smallest Amount of Stratocumulus in Summer?

Chen Zhou, Wenrong Bai, Naifu Shao, Lei Zhu, Yunying Li, Ping Tian, Mengyu Huang, Ru Zhou, Chunsong Lu, Zhiwei Zhang
article en

Abstract

Abstract The melting of sea ice in the Arctic has sparked research into how clouds form in exposed ice‐free zones. This study delves into the seasonal distribution of stratocumulus clouds over the Norwegian Sea‐Barents Sea region and presents a conceptual model for the underlying mechanisms. In spring, autumn, and winter, increased surface water vapor flux provides water vapor from the sea surface. Concurrently, warm air enters the area through the southwest wind of the Norwegian Strait. Under conditions of unstable stratification, the water vapor is lifted to the condensation level, promoting the formation of stratocumulus clouds. Conversely, in summer, evaporation is suppressed due to stable stratification, which hinders vertical vapor transport. Enhanced dry advection reduces the transport of water vapor, leading to a decrease in the amount of stratocumulus clouds during summer. This research enriches our understanding of the physical mechanisms influencing cloud formation and cloud‐climate feedbacks in the Arctic region.

Geophysical Research LettersVol. 52(20)
National University of Defense Technology (CN), Nanjing University of Information Science and Technology (CN), People's Liberation Army No. 150 Hospital (CN), Beijing Meteorological Bureau (CN), Chinese People 's Liberation Army No. 85 Hospital (CN), Jilin Weather Modification Office (CN), China Nonferrous Metals Changsha Investigation Design Institute (CN), Chinese People’s Liberation Army 263 hospital (CN), Nanjing University (CN)
National Natural Science Foundation of China, Nanjing University of Information Science and Technology, Nanjing University
Openalex Percentile: Top 66%
Atmospheric chemistry and aerosols
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