2014
DOI: 10.1016/j.epsl.2014.05.016
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Labrador current variability over the last 2000 years

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Cited by 54 publications
(67 citation statements)
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“…Our findings are in line with other high-resolution ocean sediment records, e.g. by Sicre et al (2014) who report a warming signal in the subpolar North Atlantic in contrast to a cooling in the Nordic Seas in sub-decadal ocean sediment records from North Iceland and North East Newfoundland. Signatures of a major environmental shift at the MCA-LIA transition are also reported from two calcite and quartz based sediment records from the Denmark Strait (Andrews and Jennings 2014).…”
Section: Analysis Of the Ocean Sediment Recordssupporting
confidence: 93%
“…Our findings are in line with other high-resolution ocean sediment records, e.g. by Sicre et al (2014) who report a warming signal in the subpolar North Atlantic in contrast to a cooling in the Nordic Seas in sub-decadal ocean sediment records from North Iceland and North East Newfoundland. Signatures of a major environmental shift at the MCA-LIA transition are also reported from two calcite and quartz based sediment records from the Denmark Strait (Andrews and Jennings 2014).…”
Section: Analysis Of the Ocean Sediment Recordssupporting
confidence: 93%
“…This MCA-LIA climate transition, consistent with a suggested shift to more negative NAO conditions (Seidenkrantz et al, 2007(Seidenkrantz et al, , 2008Trouet et al, 2009Trouet et al, , 2012Olsen et al, 2012;Sicre et al, 2014), may be attributed to some combination of explosive volcanism and reductions in solar irradiance, especially the Sp€ orer Minimum. A cross-correlation analysis further shows that the maximum correlation is obtained at zero lag (Fig.…”
Section: Discussionmentioning
confidence: 52%
“…Other SST reconstructions show, in contrast, warmer conditions during the LIA than during the MCA, for example, in the eastern subpolar North Atlantic (e.g., Miettinen et al 2012; Fig. 7d) or off northeastern Newfoundland (Sicre et al 2014). These SST reconstructions thus draw a characteristic pattern of cold Nordic and Labrador seas opposed to a warm eastern subpolar North Atlantic and North Atlantic Current that resembles the simulated post-shift SST anomaly pattern (Fig.…”
Section: The Medieval Climate Anomaly: Little Ice Age Transitionmentioning
confidence: 73%