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Влияние температуры на поверхности океана в тропиках на антарктический морской лед в период глобального потепления
Abstract
При наблюдаемом глобальном потеплении морской ледяной покров в Антарктике в отличие от Арктики не проявлял тенденций к сокращению, в то время как глобальные климатические модели показывают его уменьшение. Цель исследования – объяснить этот климатический феномен на основе идеи о совместной динамике океанических структур Южного океана – Антарктического полярного фронта (АПФ) и границы максимального распространения морского льда, положение которых меняется под влиянием аномалий температуры на поверхности океана в низких широтах.
About the Authors
Генрих АлексеевRussian Federation
Наталья Глок
Анастасия Вязилова
Николай Иванов
Наталья Харланенкова
Александр Смирнов
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