aariПроблемы Арктики и АнтарктикиArctic and Antarctic Research0555-26482618-6713Государственный научный центр Российской Федерации Арктический и антарктический научно-исследовательский институт10.30758/0555-2648-2024-70-2-222-237aari-614Research ArticleГЛЯЦИОЛОГИЯ И КРИОЛОГИЯGLACIOLOGY AND CRYOLOGY OF THE EARTHФакторы активизации термоденудации и активность термоцирков на Центральном Ямале в 2010–2018 гг.Factors of thermal denudation activation and thermicirques activity on central Yamal in 2010–2018https://orcid.org/0000-0001-8855-3483ХомутовА. В.KhomutovA. V.

Тюмень

Artem V. Khomutov

Tyumen

artcryo@yandex.ruhttps://orcid.org/0000-0002-1426-6091БабкинаЕ. А.BabkinaE. A.

Тюмень

Elena A. Babkina

Tyumen

https://orcid.org/0000-0002-4948-8938ХайруллинР. Р.KhairullinR. R.

Корнойбург

Rustam R. Khairullin

Korneuburg

https://orcid.org/0000-0003-3491-4487ДворниковЮ. А.DvornikovYu. A.

Москва, Пущино

Yury A. Dvornikov - Smart Urban Nature Laboratory, PFUR; Laboratory of Carbon Monitoring in Terrestrial Ecosystems, IPBPSS RAS

Moscow, Pushchino

Институт криосферы Земли Тюменского научного центра СО РАНРоссияEarth Cryosphere Institute, Tyumen Scientific Centre, Siberian Branch of the Russian Academy of SciencesRussian FederationООО «b.geos»Австрияb.geos GmbHAustriaРоссийский университет дружбы народов; Институт физико-химических и биологических проблем почвоведения РАНРоссияPeoples’ Friendship University of Russia; Institute of Physicochemical and Biological Problems of Soil Science of the Russian Academy of SciencesRussian Federation202427062024702222237Copyright © Хомутов А.В., Бабкина Е.А., Хайруллин Р.Р., Дворников Ю.А., 20242024Хомутов А.В., Бабкина Е.А., Хайруллин Р.Р., Дворников Ю.А.Khomutov A.V., Babkina E.A., Khairullin R.R., Dvornikov Y.A.Данная работа распространяется под лицензией Creative Commons Attribution 4.0.This work is licensed under a Creative Commons Attribution 4.0 License.https://www.aaresearch.science/jour/article/view/614

Рассмотрены климатические факторы активизации термоденудационных процессов, приводящих к образованию термоцирков, в центральной части полуострова Ямал. На основе сопоставления разновременных дистанционных материалов, сопровождавшегося анализом климатических данных, проведен анализ активности термоцирков в период 2010–2018 гг. Помимо «классических» термоцирков, характеризующихся в анализируемый временной период разной степенью активности, выделено существенное количество эмбриональных термоденудационных форм.

The paper presents research findings of the climatic factors responsible for the activation of thermal denudation processes leading to the formation of thermocirques in the central part of the Yamal Peninsula in the north of West Siberia. Based on a comparison of multi-temporal remote sensing (2010, 2013 and 2018) coupled with climate data, an analysis of the thermocirques activity in 2010–2018 was carried out. Thermocirques are specific topographic forms that arise because of the activation of cryogenic earth flows, the formation of which is caused by an increased seasonal thawing of the upper part of the ground ice on the slopes as compared to the previous years. Analysis of the monitoring data showed that in 2012 and 2013 all the types of surfaces are characterized by a significant increase in seasonal thawing compared to the previous period 1993–2011 (12 % increase on slopes), due to the summer air temperature, the amount of summer precipitation and the increased duration of the warm period. The results of the thermocirques activity analysis are shown on a map. The results of this local study were compared with those of a regional (Yamal and Gydan Peninsulas) remote sensing study of thermocirques. This showed a higher accuracy of the local study based on field monitoring and very-high-resolution satellite imagery. The analysis of the thermocirques activity showed that 1) over the period from 2010 to 2018 thermal denudation activity in the study area increased due to the anomalous climatic conditions in the spring-summer season of 2012, and then gradually decreased; 2) in addition to “classical” thermocirques, which were at different stages of activity in the time periods analyzed (2010, 2013 and 2018), a significant number of embryonic thermocirques were identified. Such thermocirques, just as the majority of small “classical” thermocirques, can only be identified on very-high-resolution satellite imagery.

изменение климатамноголетнемерзлые породыподземный ледполуостров Ямалсезонное протаиваниетермоденудациятермоциркclimate changeground icepermafrostseasonal thawingthermal denudationthermocirqueYamal PeninsulaРабота выполнена Институтом криосферы Земли ТюмНЦ СО РАН в рамках государственного задания Министерства науки и высшего образования Российской Федерации (тема № FWRZ2021-0012). Данные мониторинга глубины сезонного протаивания (с 1993 по 2018 г.) и термоцирков (с 2012 по 2017 г.) получены в рамках интеграционных проектов СО РАН № 122 и 144. Мониторинг термоцирков в 2018–2020 гг., а также первоначальный этап анализа их активности проведены в рамках гранта РФФИ № 18-05-60222. 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The authors declare that there are no conflicts of interest present.