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|a Varying planetary heat sink led to global-warming slowdown and acceleration |h [electronic resource]. |
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|a [S.l.] : |b American Association of the Advancement of Science, |c 2014. |
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|a Science Magazine Volume 345. |
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|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. |
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|a A vacillating global heat sink at intermediate ocean depths is associated with different
climate regimes of surface warming under anthropogenic forcing: The latter part of the
20th century saw rapid global warming as more heat stayed near the surface. In the 21st
century, surface warming slowed as more heat moved into deeper oceans. In situ and
reanalyzed data are used to trace the pathways of ocean heat uptake. In addition to the
shallow La Niña–like patterns in the Pacific that were the previous focus, we found that
the slowdown is mainly caused by heat transported to deeper layers in the Atlantic
and the Southern oceans, initiated by a recurrent salinity anomaly in the subpolar North
Atlantic. Cooling periods associated with the latter deeper heat-sequestration
mechanism historically lasted 20 to 35 years. |
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|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. |
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|t Varying planetary heat sink led to global-warming slowdown and acceleration |
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|a dpSobek |c Sea Level Rise |
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|u http://dpanther.fiu.edu/dpService/dpPurlService/purl/FI15042677/00001 |y Click here for full text |
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|3 FULL TEXT- Varying planetary heat sink led to global-warming slowdown and acceleration |u http://science.sciencemag.org/content/345/6199/897 |y Varying planetary heat sink led to global-warming slowdown and acceleration |
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|a http://dpanther.fiu.edu/sobek/content/FI/15/04/26/77/00001/FI15042677_thm.jpg |
