Lagrangian Decomposition of the Atlantic Ocean Heat Transport at 26.5°N

The Atlantic Meridional Overturning Circulation (AMOC) plays a critical role in the global climate system through the redistribution of heat, freshwater and carbon. At 26.5°N, the meridional heat transport has traditionally been partitioned geometrically into vertical and horizontal circulation cell...

Повний опис

Бібліографічні деталі
Автори: Tooth, OJ, Foukal, NP, Johns, WE, Johnson, HL, Wilson, C
Формат: Journal article
Мова:English
Опубліковано: Wiley Open Access 2024

Схожі ресурси