Endogenous Heat of Hot Intramantle Vortices as One of the Possible Reasons for the Formation of the Circulation in the Beaufort Sea and the Northern Part of the Chukchi Sea
摘要
It has been shown that along with wind, the cause of formation of the circulation structure of the Beaufort circulation, including anticyclonic circulation in the upper layers and cyclonic circulation in the lower layers, can be endogenous heat fluxes from the outlets of hot intramantle vortices.