circulation méridienne de retournement atlantique
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Concept
Atlantic Meridional Overturning Circulation L11
The Atlantic Meridional Overturning Circulation (AMOC) is a zonally-integrated component of the Atlantic Ocean's surface and deep currents, driven by the difference in density between warm, salty water in the equatorial region and cold, freshwater in the polar region.
Translations
- دوران انقلاب خط الزوال الأطلسي ar primary
- Atlantische Umwälzzirkulation German primary
- Atlantic meridional overturning circulation English primary
- circulación de vuelco meridional del Atlántico Spanish primary
- circulation méridienne de retournement atlantique French primary
- Capovolgimento meridionale della circolazione atlantica it primary
- 大西洋南北熱塩循環 ja primary
- Circulação meridional de capotamento do Atlântico pt primary
- Атлантическая меридиональная опрокидывающая циркуляция ru primary
- 大西洋经向翻转环流 zh primary
Etymology
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