Thomas Blunier , Period Antarctica and Greenland During the Last Glacial Timing of Millennial - Scale Climate

نویسنده

  • Thomas Blunier
چکیده

http://www.sciencemag.org/cgi/content/full/291/5501/109 version of this article at: including high-resolution figures, can be found in the online Updated information and services, http://www.sciencemag.org/cgi/content/full/291/5501/109/DC1 can be found at: Supporting Online Material found at: can be related to this article A list of selected additional articles on the Science Web sites http://www.sciencemag.org/cgi/content/full/291/5501/109#related-content http://www.sciencemag.org/cgi/content/full/291/5501/109#otherarticles , 4 of which can be accessed for free: cites 7 articles This article 184 article(s) on the ISI Web of Science. cited by This article has been http://www.sciencemag.org/cgi/content/full/291/5501/109#otherarticles 26 articles hosted by HighWire Press; see: cited by This article has been http://www.sciencemag.org/cgi/collection/atmos Atmospheric Science : subject collections This article appears in the following

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Timing of millennial-scale climate change in Antarctica and Greenland during the last glacial period.

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Fig. 1. Squared-cross-correlation as a function of lag between (a) the predictions of M1 and Antarctic temperatures, and (b) M2 predictions Schmittner et al. (2003) argue that during the last glacial period, at millennial timescales, temperature changes in Greenland preceded changes of the opposite sign in Antarctica by 400–500 yr. They provide support for this conclusion by comparing a simple ...

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Was millennial scale climate change during the Last Glacial triggered by explosive volcanism?

The mechanisms responsible for millennial scale climate change within glacial time intervals are equivocal. Here we show that all eight known radiometrically-dated Tambora-sized or larger NH eruptions over the interval 30 to 80 ka BP are associated with abrupt Greenland cooling (>95% confidence). Additionally, previous research reported a strong statistical correlation between the timing of Sou...

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Centennial-scale mineral dust peaks in last glacial Greenland ice cores match the timing of lowest Greenland temperatures, yet little is known of equivalent changes in dust-emitting regions, limiting our understanding of dust-climate interaction. Here, we present the most detailed and precise age model for European loess dust deposits to date, based on 125 accelerator mass spectrometry 14C ages...

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تاریخ انتشار 2006