МЕХАНИЗМ КОМПЕНСАЦИИ БЬЕРКНЕСА КАК ВОЗМОЖНЫЙ ТРИГГЕР НИЗКОЧАСТОТНОЙ ИЗМЕНЧИВОСТИ АРКТИЧЕСКОГО УСИЛЕНИЯ
Аннотация и ключевые слова
Аннотация (русский):
Причины Арктического усиления широко обсуждаются, и целостной картины пока не получено. В этом исследовании изучалась роль Атлантического меридионального океанического и атмосферного переноса тепла в Арктику в возникновении Арктического усиления. Рассматривались интегральные адвективные потоки в слое Атлантических вод и в нижней тропосфере. Результаты показывают сильную связь между меридиональными потоками тепла и региональным Арктическим усилением в Евразийской Арктике на десятилетних временных масштабах (10–15 лет). Мы утверждаем, что низкочастотная изменчивость Арктического усиления регулируется цепочкой океанический перенос тепла — атмосферный перенос тепла — Арктическое усиление. Отклик атмосферы на воздействие океана происходит с задержкой в три года и объясняется компенсационным механизмом Бьеркнеса. В свою очередь атмосферный перенос тепла и влаги напрямую влияет на величину Арктического усиления, причём с отставанием последнего на один год. Таким образом, изменчивость океанического переноса тепла на южной границе морей Северо-Европейского бассейна может быть предиктором величины Арктического усиления над Евразийским бассейном Северного Ледовитого океана с заблаговременностью в четыре года. Результаты согласуются с концепцией десятилетней изменчивости климата Арктики, выраженной через индекс колебания Северного Ледовитого океана.

Ключевые слова:
океанический перенос тепла, атмосферный перенос тепла, десятилетняя изменчивость, климат Арктики, взаимодействие, Евразийский бассейн
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