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Annually resolved North Atlantic marine climate over the last millennium

Annually resolved North Atlantic marine climate over the last millennium

Titill: Annually resolved North Atlantic marine climate over the last millennium
Höfundur: Reynolds, D. J.
Scourse, J. D.
Halloran, P. R.
Nederbragt, A. J.
Wanamaker, A. D.
Butler, P. G.
Richardson, C. A.
Heinemeier, J.
Eiriksson, Jon   orcid.org/0000-0001-5598-2417
Knudsen, K. L.
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Útgáfa: 2016-12-06
Tungumál: Enska
Umfang: 13502
Háskóli/Stofnun: Háskóli Íslands
University of Iceland
Svið: Verkfræði- og náttúruvísindasvið (HÍ)
School of Engineering and Natural Sciences (UI)
Deild: Jarðvísindastofnun (HÍ)
Institute of Earth Sciences (UI)
Birtist í: Nature Communications;7
ISSN: 2041-1723
DOI: 10.1038/ncomms13502
Efnisorð: Ocean sciences; Palaeoceanography; Palaeoclimate; Haffræði; Jarðsaga; Loftslag
URI: https://hdl.handle.net/20.500.11815/383

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Reynolds, D. J. et al. Annually resolved North Atlantic marine climate over the last millennium. Nat. Commun. 7, 13502 doi: 10.1038/ncomms13502 (2016).


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.


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