Stratospheric Ozone-induced Cloud Radiative Effects on Antarctic Sea Ice

@article{Xia2020StratosphericOC,
  title={Stratospheric Ozone-induced Cloud Radiative Effects on Antarctic Sea Ice},
  author={Yan Xia and Yongyun Hu and Jiping Liu and Yi Huang and Fei Xie and Jintai Lin},
  journal={Advances in Atmospheric Sciences},
  year={2020},
  volume={37},
  pages={505-514}
}
Recent studies demonstrate that the Antarctic Ozone Hole has important influences on Antarctic sea ice. While most of these works have focused on effects associated with atmospheric and oceanic dynamic processes caused by stratospheric ozone changes, here we show that stratospheric ozone-induced cloud radiative effects also play important roles in causing changes in Antarctic sea ice. Our simulations demonstrate that the recovery of the Antarctic Ozone Hole causes decreases in clouds over… 
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References

SHOWING 1-10 OF 43 REFERENCES
Has the ozone hole contributed to increased Antarctic sea ice extent?
Since the 1970s sea ice extent has decreased dramatically in the Northern Hemisphere and increased slightly in the Southern Hemisphere, a difference that is potentially explained by ozone depletion
Strong modification of stratospheric ozone forcing by cloud and sea-ice adjustments
Abstract. We investigate the climatic impact of stratospheric ozone recovery (SOR), with a focus on the surface temperature change in atmosphere–slab ocean coupled climate simulations. We find that
The Antarctic Sea Ice Response to the Ozone Hole in Climate Models
AbstractIt has been suggested that the increase of Southern Hemisphere sea ice extent since the 1970s can be explained by ozone depletion in the Southern Hemisphere stratosphere. In a previous study,
Anthropogenic influence on recent circulation‐driven Antarctic sea ice changes
Observations reveal an increase of Antarctic sea ice over the past three decades, yet global climate models tend to simulate a sea ice decrease for that period. Here we combine observations with
Non-annular atmospheric circulation change induced by stratospheric ozone depletion and its role in the recent increase of Antarctic sea ice extent
Based on a new analysis of passive microwave satellite data, we demonstrate that the annual mean extent of Antarctic sea ice has increased at a statistically significant rate of 0.97% dec−1 since the
Mitigation of 21st century Antarctic sea ice loss by stratospheric ozone recovery
We investigate the effect of stratospheric ozone recovery on Antarctic sea ice in the next half‐century, by comparing two ensembles of integrations of the Whole Atmosphere Community Climate Model,
Can natural variability explain observed Antarctic sea ice trends? New modeling evidence from CMIP5
The recent observed positive trends in total Antarctic sea ice extent are at odds with the expectation of melting sea ice in a warming world. More problematic yet, climate models indicate that sea
Signatures of the Antarctic ozone hole in Southern Hemisphere surface climate change
Roughly 90% of atmospheric ozone is found in the lower stratosphere in the ozone layer. Since about the 1970s, anthropogenic emissions of ozone-depleting gases have led to depletion of ~3–4% of the
Antarctic climate response to stratospheric ozone depletion in a fine resolution ocean climate model
We investigate the impact of stratospheric ozone depletion on Antarctic climate, paying particular attention to the question of whether eddy parameterizations in the ocean fundamentally alter the
Climate system response to stratospheric ozone depletion and recovery
We review what is presently known about the climate system response to stratospheric ozone depletion and its projected recovery, focusing on the responses of the atmosphere, ocean and cryosphere.
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