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245 00 |a Onset of deglacial warming in West Antarctica driven by local orbital forcing |h [electronic resource].
260        |a [S.l.] : |b Macmillan Publishers Limited, |c 2013-08-22.
490        |a Nature Magazine Volume 500 |b Letter.
506        |a Please contact the owning institution for licensing and permissions. It is the user's responsibility to ensure use does not violate any third party rights.
520 3    |a The cause of warming in the Southern Hemisphere during the most recent deglaciation remains a matter of debate. Hypotheses for a Northern Hemisphere trigger, through oceanic redistributions of heat, are based in part on the abrupt onset of warming seen in East Antarctic ice cores and dated to 18,000 years ago, which is several thousand years after high-latitude Northern Hemisphere summer insolation intensity began increasing from its minimum, approximately 24,000 years ago. An alternative explanation is that local solar insolation changes cause the Southern Hemisphere to warm independently. Here we present results from a new, annually resolved ice-core record from West Antarctica that reconciles these two views. The records show that 18,000 years ago snow accumulation inWest Antarctica began increasing, coincident with increasing carbon dioxide concentrations,warming in EastAntarctica and cooling in the Northern Hemisphere associated with an abrupt decrease in Atlantic meridional overturning circulation. However, significant warming in West Antarctica began at least 2,000 years earlier. Circum-Antarctic sea-ice decline, driven by increasing local insolation, is the likely cause of this warming. The marine-influencedWest Antarctic records suggest a more active role for the Southern Ocean in the onset of deglaciation than is inferred fromice cores in the East Antarctic interior, which are largely isolated from sea-ice changes.
533        |a Electronic reproduction. |c Florida International University, |d 2015. |f (dpSobek) |n Mode of access: World Wide Web. |n System requirements: Internet connectivity; Web browser software.
600        |a. |z Antarctica
600        |a. |z Southern Hemisphere
650        |a climate change.
650        |a ice cores.
710 2    |a WAIS Divide Project.
830    0 |a dpSobek.
830    0 |a Sea Level Rise.
852        |a dpSobek |c Sea Level Rise
856 40 |u http://dpanther.fiu.edu/dpService/dpPurlService/purl/FI15060348/00001 |y Click here for full text
992 04 |a http://dpanther.fiu.edu/sobek/content/FI/15/06/03/48/00001/FI15060348_thm.jpg
997        |a Sea Level Rise


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