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Loop Current variability as trigger of coherent Gulf Stream transport anomalies
Structure and variability of the Antilles Current at 26.5°N
Estimating the Freshwater Flux from the Greenland Ice Sheet Workshop Report, American Geophysical Union, 2018
The Atlantic meridional overturning circulation (AMOC) has been observed continuously at 26° N since April 2004. The AMOC and its …
The North Atlantic Ocean is in a state of reduced overturning
The Atlantic Meridional Overturning Circulation (AMOC) is responsible for a variable and climatically important northward transport of …