Enhanced Wintertime Convergence of Atmospheric and Oceanic Heat Transports in the Barents Sea Region under Present Climate Warming

Латонин Михаил Михайлович; Башмачников Игорь Львович; Семенов Владимир Анатольевич

doi:10.2205/2025ES000967

ВАК 1.6 УДК 551.5 ГРНТИ 37.21 ОКСО 05.02.03 ББК 26 ТБК 63 BISAC SCI УДК 55 УДК 550.34 УДК 550.383 ГРНТИ 37.23 ГРНТИ 37.25 ГРНТИ 37.01 ГРНТИ 37.15 ГРНТИ 37.31 ГРНТИ 38.01 ГРНТИ 36.00 ГРНТИ 37.00 ГРНТИ 38.00 ГРНТИ 39.00 ГРНТИ 52.00 ОКСО 05.00.00

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ENHANCED WINTERTIME CONVERGENCE OF ATMOSPHERIC AND OCEANIC HEAT TRANSPORTS IN THE BARENTS SEA REGION UNDER PRESENT CLIMATE WARMING Enhanced Wintertime Convergence of Atmospheric and Oceanic Heat Transports in the Barents Sea Region under Present Climate Warming

АА Аа

Опубликовано в Russian Journal of Earth Sciences · Том 25, Номер 2 · Страницы 1–11 · Рубрика: Спецвыпуск: "Наука о данных, геоинформатика и системный анализ в изучении Земли"

DOI: https://doi.org/10.2205/2025ES000967 · EDN: DRHLZX

Получено: 15.11.2024 Одобрено: 15.04.2025 Опубликовано: 23.05.2025 Язык публикаций: ENG

Авторы

ЛА

Латонин Михаил Михайлович

ORCID Scopus ResearcherID SPIN

БА

Башмачников Игорь Львович

ORCID

СЕ

Семенов Владимир Анатольевич

ORCID Scopus SPIN

ЛА

Латонин Михаил Михайлович

Ученая степень: кандидат географических наук

Международный центр по окружающей среде и дистанционному зондированию имени Нансена Научный сотрудник · Россия · Санкт-Петербург

Федеральное государственное бюджетное учреждение науки Институт физики атмосферы им. А.М. Обухова Российской академии наук Научный сотрудник · Отдел исследования климатических процессов · Россия · Москва

ORCID Scopus ResearcherID SPIN

БА

Башмачников Игорь Львович

Ученая степень: кандидат географических наук

Международный центр по окружающей среде и дистанционному зондированию имени Нансена Директор · Россия · Санкт-Петербург

Санкт-Петербургский государственный университет Доцент · Россия · Санкт-Петербург

ORCID

СЕ

Семенов Владимир Анатольевич

Ученая степень: доктор физико-математических наук

Ученое звание: академик author.academy_titles.32 ; профессор author.academy_titles.32

Институт физики атмосферы им. А.М. Обухова РАН Россия

Институт Географии РАН Россия

ORCID Scopus SPIN

АННОТАЦИЯ

A distinctive feature of the Barents Sea climate system is a suggested positive feedback in the ocean–sea ice–atmosphere system that can enhance regional climate variations. The objective of this study is to assess the effectiveness of this positive feedback for the advective heat fluxes in the winter season using the ORAS4 ocean reanalysis and ERA5 atmospheric reanalysis data for the period 1959–2017. Based on the signs of the linear trends of the oceanic heat transport, two periods were identified for the analysis: 1959–1987 and 1987–2017. Composite maps of surface wind fields indicate an increase in the effectiveness of the positive feedback in the Barents Sea region during the present period relative to the previous one. This is manifested in the strengthening of the southern winds over the southeastern part of the sea in years with the maximum oceanic heat transport and in the weakening of the northern winds over the northwestern part of the sea in years with the minimum oceanic heat transport. The convergence of the atmospheric sensible heat transport over the Barents Sea has a maximum in the lower troposphere, 1000–900 hPa. An increasing synchronization of the convergence of atmospheric and oceanic heat transports in the Barents Sea region, derived in this study, contributes to an acceleration of the local warming.

КЛЮЧЕВЫЕ СЛОВА

Barents Sea, advective heat fluxes, atmospheric and oceanic circulation, convergence, Arctic warming, climate feedbacks, reanalysis datasets

Финансирование

This study was funded by the Russian Science Foundation (RSF), grant number 23-77-01046 (https://rscf.ru/en/project/23-77-01046/). M. M. L. would like to thank Alexander P. Makshtas for the valuable discussion on the methodology and advice.

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Контент доступен под лицензией Creative Commons «С указанием авторства версии 4.0 Международная» Creative Commons

ГОСТ

Латонин М. М., Башмачников И. Л., Семенов В. А. Enhanced Wintertime Convergence of Atmospheric and Oceanic Heat Transports in the Barents Sea Region under Present Climate Warming // Russian Journal of Earth Sciences. 2024. №. 2. С. 1-11. DOI: https://doi.org/10.2205/2025ES000967. EDN: DRHLZX. (дата обращения: 28.09.2026).

MLA

Латонин Михаил Михайлович, Башмачников И. Л., Семенов В. А.. "Enhanced Wintertime Convergence of Atmospheric and Oceanic Heat Transports in the Barents Sea Region under Present Climate Warming." Russian Journal of Earth Sciences 25.2 (2024): 1-11. DOI: https://doi.org/10.2205/2025ES000967. EDN: DRHLZX.

APA

Латонин М. М., Башмачников И. Л., Семенов В. А. (2024). Enhanced Wintertime Convergence of Atmospheric and Oceanic Heat Transports in the Barents Sea Region under Present Climate Warming. Russian Journal of Earth Sciences, 25(2), 1-11. https://doi.org/10.2205/2025ES000967 EDN: DRHLZX.

Chicago

Латонин Михаил Михайлович, Башмачников И. Л., Семенов В. А.. "Enhanced Wintertime Convergence of Atmospheric and Oceanic Heat Transports in the Barents Sea Region under Present Climate Warming." Russian Journal of Earth Sciences 25, no. 2 (2024): 1-11. https://doi.org/10.2205/2025ES000967. EDN: DRHLZX.

WIKI

{{cite journal | author = Латонин М. М., Башмачников И. Л., Семенов В. А. | title = Enhanced Wintertime Convergence of Atmospheric and Oceanic Heat Transports in the Barents Sea Region under Present Climate Warming | journal = Russian Journal of Earth Sciences | year = 2024 | volume = 25 | issue = 2 | pages = 1-11 | doi = 10.2205/2025ES000967 }} EDN: DRHLZX

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ENHANCED WINTERTIME CONVERGENCE OF ATMOSPHERIC AND OCEANIC HEAT TRANSPORTS IN THE BARENTS SEA REGION UNDER PRESENT CLIMATE WARMING Enhanced Wintertime Convergence of Atmospheric and Oceanic Heat Transports in the Barents Sea Region under Present Climate Warming

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