AMOC

Loop Current variability as trigger of coherent Gulf Stream transport anomalies
Loop Current variability as trigger of coherent Gulf Stream transport anomalies
Structure and variability of the Antilles Current at 26.5°N
Structure and variability of the Antilles Current at 26.5°N
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 …
The North Atlantic Ocean is in a state of reduced overturning