Ice Age Terminations

By M. Guazzaroni, Florencio Pazos, J. M. Vieites, Marta Godoy, O. Golyshina, T. Chernikova, Agnes Waliczek, V. Cono, Carmen Méndez, J. Salas and 4 more. Science, 2009

919 citations recorded by the source corpus.

Subfields: Atmospheric Science, Environmental Chemistry, Paleontology

View Paper: https://www.semanticscholar.org/paper/14f44bb74ee0bc98c4da8f59207aa7b3ad5ae806

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Citations in the corpus

StalAge – An algorithm designed for construction of speleothem age models (2011, background): “…plasma mass University of Mainz, Johannþ49 6131 3924767; fax: þ49 tapuerca s/n, 09002-Burgos, . lz), dirk.hoffmann@cenieh.es All rights reserved. spectrometry (MCeICPMS) has further increased the precision of speleothem U-series ages in recent years (Hoffmann et al., 2007; Cheng et al., 2009).”
Astronomical and glacial forcing of East Asian summer monsoon variability (2015, positive): “Abrupt methane and speleothem d 18 O changes are contemporaneous with high-latitude cooling during glacial terminations (Cheng et al., 2009), con ﬁ rming a strong coupling of rapid monsoon and ice volume changes during deglaciations.”
The polar ocean and glacial cycles in atmospheric CO2 concentration (2010, background): “4), the Heinrich-associated cold intervals within the last ice age 78,79 , and at previous deglaciations 80,81 .”
Extreme deepening of the Atlantic overturning circulation during deglaciation (2010, background): “The association of AMOC see-saw oscillations with glacial terminations during the late Pleistocene seems ubiquitou”
A Review of the Role of the Atlantic Meridional Overturning Circulation in Atlantic Multidecadal Variability and Associated Climate Impacts (2019, background): “The AMOC is suggested to have played a critical role in abrupt climate change events centered in the Atlantic seen inmany paleoclimate records (e.g., Alley, 2007; Broecker et al., 1985; Cheng et al., 2009; Clark et al., 2002; McManus et al., 2004; Rahmstorf, 2002).”
Deglaciation in the tropical Indian Ocean driven by interplay between the regional monsoon and global teleconnections (2013, background): “The LGM δ18O minimum in the Hulu Cave record is at 19.0 kyr BP, and the post-LGM δ18O maximum in Hulu is at 16.0 kyr BP (Cheng et al., 2009; Southon et al., 2012), both of which coincide with timing of the correlative δ18Osw events in the Malabar core.”