2015
DOI: 10.1007/s00382-015-2561-x
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Indications for a North Atlantic ocean circulation regime shift at the onset of the Little Ice Age

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Cited by 29 publications
(34 citation statements)
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“…The latter resulted, on the one hand, in a baroclinic spin-up of the SPG due to increasing recirculation of subtropical water into the subpolar region and, on the other hand, in a LIA-like basin-wide cooling due to weakened heat transport by the AMOC. These results agree with SST reconstructions from the Nordic Seas and the eastern subpolar North Atlantic (Schleussner et al 2015; these SST reconstructions are also shown in Fig. 7c, d), although their simulated SPG spin-up differs from reconstructed evidence of a weaker SPG during the LIA (e.g., Copard et al 2012;Moffa-Sánchez et al 2014a), which is more in accordance with our study.…”
Section: The Medieval Climate Anomaly: Little Ice Age Transitionsupporting
confidence: 82%
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“…The latter resulted, on the one hand, in a baroclinic spin-up of the SPG due to increasing recirculation of subtropical water into the subpolar region and, on the other hand, in a LIA-like basin-wide cooling due to weakened heat transport by the AMOC. These results agree with SST reconstructions from the Nordic Seas and the eastern subpolar North Atlantic (Schleussner et al 2015; these SST reconstructions are also shown in Fig. 7c, d), although their simulated SPG spin-up differs from reconstructed evidence of a weaker SPG during the LIA (e.g., Copard et al 2012;Moffa-Sánchez et al 2014a), which is more in accordance with our study.…”
Section: The Medieval Climate Anomaly: Little Ice Age Transitionsupporting
confidence: 82%
“…These results contrast with previous studies in which similar abrupt events were attributed to the volcanic forcing alone in climate simulations of the past millennium (Miller et al 2012;Schleussner and Feulner 2013;Schleussner et al 2015). The sensitivity experiments used here, however, still include changes in the other imposed external forcings (see Sect.…”
Section: Attribution Of the Spg Changes In The Last Millenniumcontrasting
confidence: 55%
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“…In particular, Seidenkrantz et al (2007) report an oceanic warming south of Greenland for Greenland. From independent proxy data it is known that during that time, the sea ice extent could be lower than average 500 which, again, could be a signature of the ocean circulation response triggered by negative anomalies in the radiative forcing (Schleussner et al, 2015;Otterå et al, 2010).…”
mentioning
confidence: 99%
“…30 It is instructive to also apply this methodology to study regime shifts in paleoclimate dynamics, 154 particularly for investigating in depth the important differences between interglacial and glacial climate variability and the nature of the transitions between those regimes. 91 As an example, we study the 2 m resolution d 18 O isotope record from the GISP2 ice core from Greenland 153 covering both the Holocene and the last glacial period (Fig.…”
Section: Use Case: Time Irreversibility In Glacial-deglacial Dynamicsmentioning
confidence: 99%