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Formation of extreme surface turbulent heat fluxes from the ocean to the atmosphere in the North Atlantic


Дәйексөз келтіру

Толық мәтін

Ашық рұқсат Ашық рұқсат
Рұқсат жабық Рұқсат берілді
Рұқсат жабық Тек жазылушылар үшін

Аннотация

The role of extreme surface turbulent fluxes in total oceanic heat loss in the North Atlantic is studied. The atmospheric circulation patterns enhancing ocean–atmosphere heat flux in regions with significant contributions of the extreme heat fluxes (up to 60% of the net heat loss) are analyzed. It is shown that extreme heat fluxes in the Gulf Stream and the Greenland and Labrador Seas occur in zones with maximal air pressure gradients, i.e., in cyclone–anticyclone interaction zones.

Авторлар туралы

N. Tilinina

Shirshov Institute of Oceanology

Хат алмасуға жауапты Автор.
Email: tilinina@sail.msk.ru
Ресей, Moscow, 117218

S. Gulev

Shirshov Institute of Oceanology

Email: tilinina@sail.msk.ru
Ресей, Moscow, 117218

A. Gavrikov

Shirshov Institute of Oceanology

Email: tilinina@sail.msk.ru
Ресей, Moscow, 117218

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