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Effects of the Antarctic elevation on the atmospheric circulation

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Abstract

The orographic effects of Antarctica on the atmospheric circulation are investigated through idealized orographic reduction numerical experiments performed using the NCAR CAM5 model. The investigation shows that, in the absence of the orography over the continent, the troposphere becomes warmer and wetter, the sea level pressure reduces, and the precipitation is enhanced. Furthermore, over the continent, the height of the tropopause increases, the stationary waves become weaker, and the southern polar jet gets more energetic. The radiative budget also gets altered, with more outgoing longwave radiation over the continent, which drives circulation changes beneath. The mean atmospheric circulation is weakened with weakening and shrinking of the Polar cell and widening of the Ferrel cell in the Southern Hemisphere, which decreases the contribution by mean flow towards poleward energy transport. An increase in transient eddy due to an enhancement of baroclinicity over the region supports poleward energy transport and compensates for a higher outgoing longwave radiation over the Antarctic continent. These significant changes observed in idealized Antarctic orographic reduction demonstrate the importance of the present Antarctic orography and ice cover for the Southern Hemisphere. The impact of these changes provides valuable insights on the future role of Antarctic orography on the earth’s climate system from a fundamental point of view.

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Acknowledgments

The authors thank Mr. Raju Pathak for providing initial help in the computational work and IIT Delhi HPC facility for providing computational support. The authors would also like to thank anonymous reviewers for their constructive comments, which have improved the quality of this manuscript. The NCAR CAM model of the CESM project supported by the National Science Foundation and Office of Science (BER) of US Department of Energy is used. For data analysis and plotting, NCAR NCL 6.4.0 was used.

Funding

The research was partially supported by the DST Centre of Excellence in Climate Modeling at the Indian Institute of Technology Delhi, India. K. Tewari acknowledges the Ph.D. fellowship from MHRD and the financial assistance received from Japan Student Service Organization (JASSO) for the ILDP Exchange program for his visit to Hiroshima University, Japan, during which a part of this work was carried out.

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Correspondence to Saroj K. Mishra.

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Tewari, K., Mishra, S.K., Dewan, A. et al. Effects of the Antarctic elevation on the atmospheric circulation. Theor Appl Climatol 143, 1487–1499 (2021). https://doi.org/10.1007/s00704-020-03456-1

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  • DOI: https://doi.org/10.1007/s00704-020-03456-1

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