Amplification of warming of high-latitude climate in the Northern and Southern hemispheres in 1956–2023
https://doi.org/10.29235/1561-8323-2025-69-4-322-329
Abstract
The results of the analysis of differences in climate norms in different months of the year during the modern climate warming period (1990–2023) and the preceding period (1956–1989) in the high latitudes of the Northern and Southern hemispheres (60–90°N and 60–90°S) are presented. A comparative analysis of changes in temperature gradient was conducted for near-equatorial (0–10°N and 0–10°S) and polar (65–90°N and 65–90°S) latitudes of the Northern and Southern hemispheres. The decrease in the gradient value was most significant in transitional seasons of the year and especially in autumn. In the Southern hemisphere, the largest decrease in temperature gradient occurred in winter and spring (June–October). The possible causes of climate warming in the high latitudes of the Northern and Southern hemispheres are considered.
About the Author
V. F. LoginovBelarus
Loginov Vladimir F. – Academician, D. Sc. (Geography), Professor, Chief Researcher
10, F. Skorina Str., 220076, Minsk
References
1. Loginov V. F. Diagnosis of global climate. St. Petersburg, 2021. 304 p. (in Russian).
2. Serreze M. C., Francis J. A. The Arctic amplification debate. Climatic Change, 2006, vol. 76, pp. 241–264. https://doi.org/10.1007/s10584-0059017-y
3. Alekseev G. V. Arctic dimension of global warming. Led i sneg = Ice and Snow, 2014, vol. 54, no. 2, pp. 53–68 (in Russian).
4. Alekseev G., Kuzmina S., Bobylev L., Urazgildeeva A., Gnatiuk N. Impact of atmospheric heat and moisture transport on the Arctic warming. International Journal of Climatology, 2019, vol. 39, no. 8, pp. 3582–3592. https://doi.org/10.1002/joc.6040
5. Cao Y., Liang Sh., Chen X., He T., Wang D., Cheng X. Enhanced wintertime greenhouse effect reinforcing Arctic amplification and initial sea-ice melting. Scientific Reports, 2017, vol. 7, art. 8462. https://doi.org/10.1038/s41598-017-08545-2
6. Andry O., Bintanja R., Hazeleger W. Time-dependent variations in the Arctic’s surface albedo feedback and the link to seasonality in sea ice. Journal of Climate, 2016, vol. 30, no. 1, pp. 393–410. https://doi.org/10.1175/jcli-d-15-0849.1
7. Bekryaev R. V., Polyakov I. V., Alexeev V. A. Role of polar amplification in long-term surface air temperature variations and modern arctic warming. Journal of Climate, 2010, vol. 23, no. 14, pp. 3888–3906. https://doi.org/10.1175/ 2010JCLI3297.1
8. Blackport R., Screen J. A. Insignificant effect of Arctic amplification on the amplitude of midlatitude atmospheric waves. Science Advances, 2020, vol. 6, no. 8, art. aay2880. https://doi.org/10.1126/sciadv.aay2880
9. Kashiwase H., Ohshima K. I., Nihashi S., Eicken H. Evidence for ice-ocean albedo feedback in the Arctic Ocean shifting to a seasonal ice zone. Scientific Reports, 2017, vol. 7, no. 1, art. 8170. https://doi.org/10.1038/s41598-017-08467-z
10. Blackport R., Screen J. A., Wiel K., Bintanja R. Minimal influence of reduced Arctic sea ice on coincident cold winters in mid-latitudes. Nature Climate Change, 2019, vol. 9, pp. 697–704. https://doi.org/10.1038/s41558-019-0551-4
11. Taylor P. C., Hegyi B. M., Boeke R. C., Boisvert L. N. On the increasing importance of air-sea exchanges in a thawing arctic: a review. Atmosphere, 2018, vol. 9, no. 2, art. 41. https://doi.org/10.3390/atmos9020041
12. Worby A. P., Allison I. Ocean-atmosphere energy exchange over thin, variable concentration Antarctic pack ice. Annals of Glaciology, 1991, vol. 15, pp. 184–190. https://doi.org/10.3189/1991AoG15-1-184-190
13. Yu L. Jin X., Schulz E. W. Surface heat budget in the Southern Ocean from 42° S to the Antarctic marginal ice zone: four atmospheric reanalyses versus icebreaker Aurora Australis measurements. Polar Research, 2019, vol. 38, art. 3349. https://doi.org/10.33265/polar.v38.3349
14. Vitinsky Yu. I., Ohl A. I., Sazonov B. I. The Sun and the Earth’s Atmosphere. Leningrad, 1976. 351 p. (in Russian).
15. Loginov V. F. Modern Climate Change. St. Petersburg, 2024. 267 р. (in Russian).