[PDF] Top 20 On the relation between Meridional Overturning Circulation and sea-level gradients in the Atlantic
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On the relation between Meridional Overturning Circulation and sea-level gradients in the Atlantic
... relations between AMOC strength and an Atlantic sea level difference for three types of forcing, but they turned out to be unsuitable as an AMOC ...of sea-level change add up ... See full document
12
High frequency variability of the Atlantic meridional overturning circulation
... Surprisingly, there is no systematic relation between the model resolution and the magnitude of variability. This con- tradicts to the general assumption that if the resolution is in- creased, variability ... See full document
16
Mid-pliocene Atlantic Meridional Overturning Circulation not unlike modern
... the Atlantic Meridional Overturning Circulation (AMOC) was significantly stronger in the mPWP compared to today (Raymo et ...North Atlantic at the time (Dowsett et ...weak ... See full document
10
Observed decline of the Atlantic meridional overturning circulation 2004–2012
... anti-correlation between sea-surface height (SSH) between 30 ◦ and 50 ◦ N in the Atlantic and ac- cumulated ...the Atlantic multidecadal oscillation ... See full document
10
Difference between the North Atlantic and Pacific meridional overturning circulation in response to the uplift of the Tibetan Plateau
... intensifying meridional oceanic cir- culation, which transports warmer subtropical water north- ward and leads to the buoyancy loss and evaporation increase ...averaged sea-ice coverage (Fig. 6c) and ... See full document
12
The Observed North Atlantic Meridional Overturning Circulation: Its Meridional Coherence and Ocean Bottom Pressure
... of meridional transport time series from the Rapid Climate Change–Meridional Overturning Circulation (RAPID MOC) array at 26 8 N and from Argo float and altimetry data at 41 8 N reveal that, ... See full document
21
The contribution of eastern-boundary density variations to the Atlantic meridional overturning circulation at 26.5 N
... The Moroccan coastal upwelling undergoes seasonal changes induced by the coast-parallel trade winds. The band between 25 ◦ N and 43 ◦ N along the African coast exhibits strongest coastal upwelling during summer ... See full document
16
Variations of the Atlantic meridional overturning circulation in control and transient simulations of the last millennium
... forcing level appropriate for 1500 ...North Atlantic basin which will likely have an impact on the AMOC: the path of the NAC is too zonal, the northward heat transport is reduced, and the sea ice ... See full document
18
Mechanisms of Atlantic Meridional Overturning Circulation variability simulated by the NEMO model
... higher sea level pressures over most of the subpolar gyre and particularly the Labrador Sea, and lower pressure over the subtropical gyre, ...difference between high and mid-latitudes, 1Pa (at ... See full document
12
Changes in extreme regional sea surface height due to an abrupt weakening of the Atlantic meridional overturning circulation
... In the HR model, a northward shift in the latitude of the Gulf Stream separation occurs after about 25 years (Fig. 12b). During the last decade of the 0.5 Sv model sim- ulation, the position of the Gulf Stream separation ... See full document
11
Low-frequency oscillations of the Atlantic Ocean meridional overturning circulation in a coupled climate model
... and sea-ice model CLIO (Goosse and Fichefet, ...North Atlantic Ocean to avoid the convergence of meridians near the north ...thermodynamic-dynamic sea-ice model ... See full document
11
Discovery and quantification of the Atlantic Meridional Overturning Circulation: the importance of 25N
... geostrophic circulation from hydrographic sections has gone on to yield many estimates of the Atlantic MOC strength (see Sections 5 and 7), but in the late 1970’s the interesting study was application of ... See full document
36
Impact of North Atlantic – GIN Sea exchange on deglaciation evolution of the Atlantic Meridional Overturning Circulation
... Labrador Sea (shown as “NADW (Lab S)”, blue solid line) and GIN Sea (shown as “NADW (GIN S)”, red solid line) for PB PreBA (a) and PB REC (b) ...GIN Sea is defined as the vertical maximum value of ... See full document
6
Can sparse proxy data constrain the strength of the Atlantic meridional overturning circulation?
... In all three pairs of experiments for Target 3 and 4, the AMOC corrections relative to the first guess had the correct sign. However, there were large differences between the tem- perature fields of those ... See full document
14
Impact of the GeoMIP G1 sunshade geoengineering experiment on the Atlantic meridional overturning circulation
... larger between the northern North Atlantic and the southern North Atlantic which could strengthening the current flowing from south to ...smaller between sea surface and the air at the ... See full document
8
How did Marine Isotope Stage 3 and Last Glacial Maximum climates differ? – Perspectives from equilibrium simulations
... The MIS 3 climate seems to have been very sensitive to in- solation changes, at least in the model. Very few reliable ter- restrial seasonal temperature reconstructions are available for MIS 3 in North America, Europe ... See full document
19
A study of the variability in the Benguela Current volume transport
... South Atlantic and transports a blend of relatively fresh and cool Atlantic water and rela- tively warm and salty Indian Ocean water ...overall meridional heat and freshwater transport in the South ... See full document
11
Tracing water masses with 129I and 236U in the subpolar North Atlantic along the GEOTRACES GA01 section
... at sea (Pierre Branellec, Floriane Desprez de Gésincourt, Michel Hamon, Catherine Kermabon, Philippe Le Bot, Stéphane Leizour, Olivider Ménage, Fabien Pérault, and Emmanuel de ... See full document
20
On the near-inertial variations of meridional overturning circulation in the South China Sea
... Abstract. We examine near-inertial variability of the merid- ional overturning circulation in the South China Sea (SC- SMOC) using a global 1/12 ◦ ocean reanalysis. Based on wavelet analysis and ... See full document
10
CLIVAR Exchanges No 24 Special issue on: CLIVAR Pacific
... Walker circulation and accelerate the formation of an El Niño ...cyclonic circulation and the equatorial westerly anomalies will also be gradually strengthened and move ... See full document
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