The role of sulfate aerosol in the formation of cloudiness over the sea

Aloyan, A. E.; Yermakov, A. N.; Arutyunyan, V. O.

doi:10.1134/s0001433816040022

Cited by 5 publications

(1 citation statement)

References 10 publications

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“…High clouds in winters for Asian and global emission enhancement are associated with the transport of sulfate aerosols through the UTLS (Shindell et al, 2008;Ren et al, 2020). Sulfate aerosols are known to play an important role in the formation of high clouds (Aloyan et al, 2016). Previous studies have also reported high cloud formation in the lower stratosphere (between 50 and 200 hPa) in the Arctic both during the winter and summer seasons (Fadnavis et al, 2019;Cairo and Colavitto 2020).…”

Section: Impacts Of Sulfate Forcing On Cloudsmentioning

confidence: 97%

The Arctic Temperature Response to Global and Regional Anthropogenic Sulfate Aerosols

Acharya

Murukesh

Müller

et al. 2021

Front. Environ. Sci.

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The mechanisms behind Arctic warming and associated climate changes are difficult to discern. Also, the complex local processes and feedbacks like aerosol-cloud-climate interactions are yet to be quantified. Here, using the Community Earth System Model (CAM5) experiments, with emission enhancement of anthropogenic sulfate 1) five-fold globally, 2) ten-times over Asia, and 3) ten-times over Europe we show that regional emissions of sulfate aerosols alter seasonal warming over the Arctic, i.e., colder summer and warmer winter. European emissions play a dominant role in cooling during the summer season (0.7 K), while Asian emissions dominate the warming during the winter season (maximum ∼0.6 K) in the Arctic surface. The cooling/warming is associated with a negative/positive cloud radiative forcing. During the summer season increase in low–mid level clouds, induced by sulfate emissions, favours the solar dimming effect that reduces the downwelling radiation to the surface and thus leads to surface cooling. Warmer winters are associated with enhanced high-level clouds that induce a positive radiative forcing at the top of the atmosphere. This study points to the importance of international strategies being implemented to control sulfate emissions to combat air pollution. Such strategies will also affect the Arctic cooling/warming associated with a cloud radiative forcing caused by sulfate emission change.

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