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

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...

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Bibliographic Details
Main Authors:	Tooth, OJ, Foukal, NP, Johns, WE, Johnson, HL, Wilson, C
Format:	Journal article
Language:	English
Published:	Wiley Open Access 2024

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