Meridional overturning circulation
Lagrangian Views of the Pathways of the Atlantic Meridional Overturning Circulation
23
High frequency variability of the Atlantic meridional overturning circulation
16
Geothermal Heating and its Influence on the Meridional Overturning Circulation
36
The effect of Arctic precipitation changes on the Atlantic meridional overturning circulation
54
The Observed North Atlantic Meridional Overturning Circulation: Its Meridional Coherence and Ocean Bottom Pressure
21
Impact of hydrographic data assimilation on the modelled Atlantic meridional overturning circulation
14
Atlantic Ocean CO2 uptake reduced by weakening of the meridional overturning circulation
34
On the relation between Meridional Overturning Circulation and sea-level gradients in the Atlantic
12
Impact of the GeoMIP G1 sunshade geoengineering experiment on the Atlantic meridional overturning circulation
8
Climate sensitivity and meridional overturning circulation in the late Eocene using GFDL CM2.1
22
Can sparse proxy data constrain the strength of the Atlantic meridional overturning circulation?
14
Links between the Southern Annular Mode and the Atlantic Meridional Overturning Circulation in a Climate Model
19
Difference between the North Atlantic and Pacific meridional overturning circulation in response to the uplift of the Tibetan Plateau
12
Impact of North Atlantic – GIN Sea exchange on deglaciation evolution of the Atlantic Meridional Overturning Circulation
6
Surface constraints on the depth of the Atlantic meridional overturning circulation: Southern Ocean versus North Atlantic
30
Uncertainty in twenty-first century projections of the Atlantic Meridional Overturning Circulation in CMIP3 and CMIP5 models
44
Changes in extreme regional sea surface height due to an abrupt weakening of the Atlantic meridional overturning circulation
11
The location of diapycnal mixing and the meridional overturning circulation
43
Towards measuring the meridional overturning circulation from space
6
Discovery and quantification of the Atlantic Meridional Overturning Circulation: the importance of 25N
36