Rapid changes of glacial climate simulated in a coupled climate model

By A. Ganopolski, Stefan Rahmstorf. Nature, 2001

1,057 citations recorded by the source corpus.

Subfields: Atmospheric Science, Environmental Chemistry

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Citations in the corpus

Transient simulation of the last glacial inception. Part I: glacial inception as a bifurcation in the climate system (2005, result): “Interestingly, in an additional experiment with warmer North Atlantic SST, which corresponds to the ‘‘warm’’ mode of the Atlantic thermohaline circulation (Ganopolski and Rahmstorf 2001), snowfall over the EUI was twice that in the ‘‘cold’’ mode, but differed little over the NAI (not shown).”
The role of the oceans in climate (2003, background): “Ganopolski and Rahmstorf (2001) found that deep-water formation south of Iceland was a stable climate mode, with overturning north of the GIS Ridge being a marginally unstable state.”
Different ocean states and transient characteristics in Last Glacial Maximum simulations and implications for deglaciation (2013, background): “These changes have been linked to large and abrupt shifts in the AMOC (e.g. Dansgaard et al., 1993; Bard et al., 2000; Ganopolski and Rahmstorf, 2001; Knorr and Lohmann, 2003, 2007; Liu et al., 2009; Barker et al., 2010; Menviel et al., 2011).”
Timing of abrupt climate change: A precise clock (2003, methodology): “This is evident by visual inspection of Figure 1; it is also supported by mechanistic simulations of these events [Ganopolski and Rahmstorf, 2001, 2002] and by the fact that analysing these events with methods appropriate for cycles fails to reliably detect the regularity that is so striking in…”
Glacial CO2 cycle as a succession of key physical and biogeochemical processes (2011, background): “The NADW formation area retreats southward and the AMOC cell shoals (Ganopolski and Rahmstorf, 2001).”
The last deglaciation: timing the bipolar seesaw (2011, background): “The ﬁrst calls on the bipolar ocean seesaw, whereby weakening of the AMOC during GS-2 and the YD, due to freshwater discharge into the North Atlantic (Ganopolski and Rahmstorf, 2001; Mc-Manus et al., 2004), reduces both northward ocean heat transport and deepwater production in the North Atlantic,…”
Modeling the effect of freshwater pulses on the early Holocene climate: the influence of high-frequency climate variability (2002, background): “…our experiments, for instance, with freshwater release rates that vary in time or with much larger fluxes than in our case [e.g., Rahmstorf, 1995; Schiller et al., 1997; Mikolajewicz et al., 1997; Fanning and Weaver, 1997; Crucifix et al., 2001; Ganopolski and Rahmstorf, 2001; Rind et al., 2001].”
Beyond the bipolar seesaw: Toward a process understanding of interhemispheric coupling (2018, methodology): “The ocean model uses the Gent and McWilliams (1990) parameterisation of mesoscale eddy activity.”
Coherent Resonant Millennial-Scale Climate Oscillations Triggered by Massive Meltwater Pulses (2003, methodology): “Similar structures can be found in the hysteresis diagrams of Ganopolski and Rahmstorf (2001).”
Changes in North Atlantic deep-water formation associated with the Dansgaard–Oeschger temperature oscillations (60–10 ka) (2002, neutral): “PII: S 0 2 7 7 - 3 7 9 1 ( 0 1 ) 0 0 1 3 7 - 8 Rahmstorf, 1994; Manabe and Stouffer, 1995; Schiller et al., 1997; Ganopolski and Rahmstorf, 2001; Rind et al., in press).”
On the driving processes of the Atlantic meridional overturning circulation (2007, background): “Latitude shifts in convection can be triggered by small forcing if the ocean circulation is close to a threshold; the resulting climate change patterns resemble DO events [Ganopolski and Rahmstorf, 2001a].”
The repeated replacement model – Rapid climate change and population dynamics in Late Pleistocene Europe (2012, background): “The standard scheme of a DO-Event (Ganopolski and Rahmstorf, 2001) is rapid climatic amelioration followed by an extended cooling phase and subsequent restart of”
Marine isotope stage 3 sea level fluctuations: Data synthesis and new outlook (2008, background): “Depending on the model in question, either D-O stadials or interstadials are considered to be the ‘‘perturbed’’ or ‘‘agitated’’ states in the system [Ganopolski and Rahmstorf, 2001; Stocker and Johnsen, 2003].”
Nonlinearities, Feedbacks and Critical Thresholds within the Earth's Climate System (2004, background): “Ganopolski and Rahmstorf (2001) proposed the following mechanism.”
The role of the thermohaline circulation in abrupt climate change (2002, background): “A number of ocean and coupled atmosphere–ocean models have found the existence of three distinct modes of the conveyor that are qualitatively the same as the modern, glacial and Heinrich modes identified by palaeoclimate dat”