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DOI10.1126/science.aau6592
A sea change in our view of overturning in the subpolar North Atlantic
Lozier, M. S.1; Li, F.1; Bacon, S.2; Bahr, F.3; Bower, A. S.3; Cunningham, S. A.4; de Jong, M. F.5,6; de Steur, L.5,6,22; deYoung, B.7; Fischer, J.8; Gary, S. F.4; Greenan, B. J. W.9; Holliday, N. P.2; Houk, A.10; Houpert, L.4; Inall, M. E.4,11; Johns, W. E.10; Johnson, H. L.12; Johnson, C.4; Karstensen, J.8; Koman, G.10; Le Bras, I. A.13; Lin, X.14,15,16; Mackay, N.17,23; Marshall, D. P.18; Mercier, H.19; Oltmanns, M.8; Pickart, R. S.3; Ramsey, A. L.3; Rayner, D.2; Straneo, F.13; Thierry, V.20; Torres, D. J.3; Williams, R. G.21; Wilson, C.17; Yang, J.3; Yashayaev, I.9; Zhao, J.3,24
发表日期2019
ISSN0036-8075
EISSN1095-9203
卷号363期号:6426页码:516-+
英文摘要

To provide an observational basis for the Intergovernmental Panel on Climate Change projections of a slowing Atlantic meridional overturning circulation (MOC) in the 21st century, the Overturning in the Subpolar North Atlantic Program (OSNAP) observing system was launched in the summer of 2014. The first 21-month record reveals a highly variable overturning circulation responsible for the majority of the heat and freshwater transport across the OSNAP line. In a departure from the prevailing view that changes in deep water formation in the Labrador Sea dominate MOC variability, these results suggest that the conversion of warm, salty, shallow Atlantic waters into colder, fresher, deep waters that move southward in the Irminger and Iceland basins is largely responsible for overturning and its variability in the subpolar basin.


WOS研究方向Science & Technology - Other Topics
来源期刊SCIENCE
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/92558
作者单位1.Duke Univ, Div Earth & Ocean Sci, Durham, NC 27708 USA;
2.Natl Oceanog Ctr, Southampton, Hants, England;
3.Woods Hole Oceanog Inst, Woods Hole, MA 02543 USA;
4.Scottish Assoc Marine Sci, Oban, Argyll, Scotland;
5.Royal Netherlands Inst Sea Res, Texel, Netherlands;
6.Univ Utrecht, Texel, Netherlands;
7.Mem Univ, Dept Phys & Phys Oceanog, St John, NF, Canada;
8.GEOMAR Helmholtz Ctr Ocean Res Kiel, Kiel, Germany;
9.Bedford Inst Oceanog, Dartmouth, NS, Canada;
10.Univ Miami, Dept Ocean Sci, Miami, FL USA;
11.Univ Edinburgh, Sch Geosci, Edinburgh, Midlothian, Scotland;
12.Univ Oxford, Dept Earth Sci, Oxford, England;
13.UCSD, Scripps Inst Oceanog, La Jolla, CA USA;
14.Ocean Univ China, Phys Oceanog Lab, Qingdao, Peoples R China;
15.Ocean Univ China, Inst Adv Ocean Studies, Qingdao, Peoples R China;
16.Qingdao Natl Lab Marine Sci & Technol, Qingdao, Peoples R China;
17.Natl Oceanog Ctr, Liverpool, Merseyside, England;
18.Univ Oxford, Dept Phys, Oxford, England;
19.CNRS, Lab Oceanog Phys & Spatiale, Plouzane, France;
20.IFREMER, Lab Oceanog Phys & Spatiale, Plouzane, France;
21.Univ Liverpool, Dept Earth Ocean & Ecol Sci, Liverpool, Merseyside, England;
22.Norwegian Polar Res Inst, Tromso, Norway;
23.Univ Exeter, Dept Geog, Exeter, Devon, England;
24.Univ Maryland, Ctr Environm Sci, Cambridge, MD USA
推荐引用方式
GB/T 7714
Lozier, M. S.,Li, F.,Bacon, S.,et al. A sea change in our view of overturning in the subpolar North Atlantic[J],2019,363(6426):516-+.
APA Lozier, M. S..,Li, F..,Bacon, S..,Bahr, F..,Bower, A. S..,...&Zhao, J..(2019).A sea change in our view of overturning in the subpolar North Atlantic.SCIENCE,363(6426),516-+.
MLA Lozier, M. S.,et al."A sea change in our view of overturning in the subpolar North Atlantic".SCIENCE 363.6426(2019):516-+.
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