Results 111 to 120 of about 1,076,103 (215)
Atlantic Meridional Overturning Circulation slowdown suppresses Atlantic Niño variability
f The Atlantic Niño is the dominant mode of interannual variability in the Tropical Atlantic with significant impacts on local and remote climate patterns.
Pedro Freire-Souza +3 more
doaj +1 more source
Abstract The North Atlantic Subpolar Gyre (NASG) has warmed much less than the global ocean over recent decades, thereby suggesting a human‐caused slowdown of the Atlantic Meridional Overturning Circulation (AMOC). This North Atlantic “warming hole” is also found in climate projections, yet with a model‐dependent timing, location and intensity. Here we
Hervé Douville +2 more
wiley +1 more source
New Constraint on Future Ocean Heat Uptake Revealed by Considering Model Spread of Radiative Forcing
Abstract Radiative forcing (F) $(F)$ is the fundamental driver of ocean heat uptake (N) $(N)$; however, its contribution to intermodel spread in N $N$ has not been quantified. We address this gap by leveraging a new set of CMIP6 experiments that diagnoses time‐varying F $F$ for the first time in 11 models.
Quran Wu, Jonathan Gregory
wiley +1 more source
Circulation characteristics in three eddy-permitting models of the North Atlantic [PDF]
A systematic intercomparison of three realistic eddy-permitting models of the North Atlantic circulation has been performed. The models use different concepts for the discretization of the vertical coordinate, namely geopotential levels, isopycnal layers,
Killworth, P. D. +31 more
core +1 more source
Symmetric instability in the Atlantic meridional overturning circulation
The role of symmetric instability in mixing momentum, buoyancy and poten- tial vorticity is examined in several constituent currents of the Atlantic Meridional Overturning Circulation: the North Brazil Current and its rings, the Deep Western Boundary Current in the Tropical Atlantic, and the East Greenland Current of the Sub-polar North Atlantic ...
openaire +1 more source
The last deglaciation provides an opportunity to assess the response of El Niño–Southern Oscillation to rapid warming and disruptions of the Atlantic Meridional Overturning Circulation, both projected in the near future.
Marco Yseki +7 more
doaj +1 more source
Abstract The drawdown of atmospheric CO2 likely triggered Antarctic glaciation during the Eocene‐Oligocene Transition (34 Ma). Accurately constraining this shift from “greenhouse” to an “icehouse” climate is essential for understanding global carbon cycle dynamics.
Keehwan Lee +5 more
wiley +1 more source
More Stabilizing Radiative Feedbacks in CO2 Removal Scenarios
Abstract Recent studies show that global mean surface temperature exhibits a transient hysteresis during CO2 ${\mathrm{C}\mathrm{O}}_{2}$ removal, where temperatures remain elevated after CO2 ${\mathrm{C}\mathrm{O}}_{2}$ concentrations return to pre‐industrial levels.
Ivan Mitevski, Gabriel A. Vecchi
wiley +1 more source
The RAPID‐MOCHA‐WBTS array in the subtropical gyre of the North Atlantic has measured the Atlantic Meridional Overturning Circulation (AMOC) and the overturning streamfunction in depth coordinates since 2004.
D. A. Smeed +11 more
doaj +1 more source
Coupling of equatorial Atlantic surface stratification to glacial shifts in the tropical rainbelt
The modern state of the Atlantic meridional overturning circulation promotes a northerly maximum of tropical rainfall associated with the Intertropical Convergence Zone (ITCZ).
R. C. Portilho-Ramos +7 more
doaj +1 more source

