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245 00 |a Pacific Ocean Heat Content During the Past 10,000 years |h [electronic resource] |y English.
260        |a [S.l.] : |b American Association for the Advancement of Science, |c 2013-11-01.
490        |a Science Magazine Volume 342 |y English.
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 Observed increases in ocean heat content (OHC) and temperature are robust indicators of global warming during the past several decades. We used high-resolution proxy records from sediment cores to extend these observations in the Pacific 10,000 years beyond the instrumental record. We show that water masses linked to North Pacific and Antarctic intermediate waters were warmer by 2.1 T 0.4°C and 1.5 T 0.4°C, respectively, during the middle Holocene Thermal Maximum than over the past century. Both water masses were ~0.9°C warmer during the Medieval Warm period than during the Little Ice Age and ~0.65° warmer than in recent decades. Although documented changes in global surface temperatures during the Holocene and Common era are relatively small, the concomitant changes in OHC are large.
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 Pacific Ocean
650        |a climate change.
650        |a Earth (Planet)--Surface temperature.
650        |a paleoclimate.
700        |a Yair Rosenthal.
700        |a Braddock K. Linsley.
700        |a Delia W. Oppo.
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/FI15050343/00001 |y Click here for full text
992 04 |a http://dpanther.fiu.edu/sobek/content/FI/15/05/03/43/00001/FI15050343_thm.jpg
997        |a Sea Level Rise


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