Annually resolved North Atlantic marine climate over the last millennium.
Annually resolved North Atlantic marine climate over the last millennium.
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DOI:
10.1038/ncomms13502
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发表时间:
2016-12-06
影响因子:
16.6
通讯作者:
Hall, I. R.
中科院分区:
文献类型:
--
作者:
Reynolds, D. J.;Scourse, J. D.;Halloran, P. R.;Nederbragt, A. J.;Wanamaker, A. D.;Butler, P. G.;Richardson, C. A.;Heinemeier, J.;Eiriksson, J.;Knudsen, K. L.;Hall, I. R.
Owing to the lack of absolutely dated oceanographic information before the modern instrumental period, there is currently significant debate as to the role played by North Atlantic Ocean dynamics in previous climate transitions (for example, Medieval Climate Anomaly-Little Ice Age, MCA-LIA). Here we present analyses of a millennial-length, annually resolved and absolutely dated marine δ18O archive. We interpret our record of oxygen isotope ratios from the shells of the long-lived marine bivalve Arctica islandica (δ18O-shell), from the North Icelandic shelf, in relation to seawater density variability and demonstrate that solar and volcanic forcing coupled with ocean circulation dynamics are key drivers of climate variability over the last millennium. During the pre-industrial period (AD 1000–1800) variability in the sub-polar North Atlantic leads changes in Northern Hemisphere surface air temperatures at multi-decadal timescales, indicating that North Atlantic Ocean dynamics played an active role in modulating the response of the atmosphere to solar and volcanic forcing. A lack of annually resolved climate records from the marine archive limits our understanding of oceanic processes. Here, the authors present a millennial-length, annually-resolved and absolutely-dated marine δ18O record from the shells of marine bivalves and offer insight into North Atlantic climate dynamics.
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通讯作者:
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