globalchange  > 气候减缓与适应
DOI: 10.1038/ngeo1797
论文题名:
Continental-scale temperature variability during the past two millennia
作者: Ahmed M.; Anchukaitis K.J.; Asrat A.; Borgaonkar H.P.; Braida M.; Buckley B.M.; Büntgen U.; Chase B.M.; Christie D.A.; Cook E.R.; Curran M.A.J.; Diaz H.F.; Esper J.; Fan Z.-X.; Gaire N.P.; Ge Q.; Gergis J.; González-Rouco J.F.; Goosse H.; Grab S.W.; Graham N.; Graham R.; Grosjean M.; Hanhijärvi S.T.; Kaufman D.S.; Kiefer T.; Kimura K.; Korhola A.A.; Krusic P.J.; Lara A.; Lézine A.-M.; Ljungqvist F.C.; Lorrey A.M.; Luterbacher J.; Masson-Delmotte V.; McCarroll D.; McConnell J.R.; McKay N.P.; Morales M.S.; Moy A.D.; Mulvaney R.; Mundo I.A.; Nakatsuka T.; Nash D.J.; Neukom R.; Nicholson S.E.; Oerter H.; Palmer J.G.; Phipps S.J.; Prieto M.R.; Rivera A.; Sano M.; Severi M.; Shanahan T.M.; Shao X.; Shi F.; Sigl M.; Smerdon J.E.; Solomina O.N.; Steig E.J.; Stenni B.; Thamban M.; Trouet V.; Turney C.S.M.; Umer M.; van Ommen T.; Verschuren D.; Viau A.E.; Villalba R.; Vinther B.M.; Von Gunten L.; Wagner S.; Wahl E.R.; Wanner H.; Werner J.P.; White J.W.C.; Yasue K.; Zorita E.
刊名: Nature Geoscience
ISSN: 17520894
出版年: 2013
卷: 6, 期:5
起始页码: 339
结束页码: 346
语种: 英语
Scopus关键词: climate change ; cooling ; decadal variation ; eighteenth century ; global change ; Little Ice Age ; Medieval Warm Period ; nineteenth century ; reconstruction ; regional climate ; Southern Hemisphere ; spatiotemporal analysis ; Arctic ; Asia ; Europe ; North America
英文摘要: Past global climate changes had strong regional expression. To elucidate their spatio-temporal pattern, we reconstructed past temperatures for seven continental-scale regions during the past one to two millennia. The most coherent feature in nearly all of the regional temperature reconstructions is a long-term cooling trend, which ended late in the nineteenth century. At multi-decadal to centennial scales, temperature variability shows distinctly different regional patterns, with more similarity within each hemisphere than between them. There were no globally synchronous multi-decadal warm or cold intervals that define a worldwide Medieval Warm Period or Little Ice Age, but all reconstructions show generally cold conditions between ad 1580 and 1880, punctuated in some regions by warm decades during the eighteenth century. The transition to these colder conditions occurred earlier in the Arctic, Europe and Asia than in North America or the Southern Hemisphere regions. Recent warming reversed the long-term cooling; during the period ad 1971-2000, the area-weighted average reconstructed temperature was higher than any other time in nearly 1,400 years.
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/106800
Appears in Collections:气候减缓与适应
科学计划与规划

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作者单位: Department of Botany, Federal Urdu University of Arts Science and Technology, Karachi 75300, Pakistan; Lamont Doherty Earth Observatory, Columbia University, Palisades NY 10964, United States; Woods Hole Oceanographic Institution, Woods Hole MA 2543, United States; School of Earth Sciences, Addis Ababa University, Addis Ababa, Ethiopia; Indian Institute of Tropical Meteorology, Pune 411008, India; Dipartimento di Matematica e Geoscienze, University of Trieste, Trieste 34128, Italy; Swiss Federal Research Institute WSL, Birmensdorf 8903, Switzerland; Département Paléoenvironnements et Paléoclimats (PAL), Université Montpellier, Montpellier 34095, France; Department of Archaeology, History, Cultural Studies and Religion, University of Bergen, Bergen 5020, Norway; Laboratorio de Dendrocronología y Cambio Global, Universidad Austral de Chile, Casilla 567 Valdivia, Chile; Center for Climate and Resilience Research, Universidad de Chile, Casilla 2777 Santiago, Chile; Australian Antarctic Division, Kingston TAS 7050, Australia; Antarctic Climate and Ecosystems Cooperative Research Centre, University of Tasmania, Sandy Bay TAS 7005, Australia; Cooperative Institute for Research in Environmental Sciences, National Oceanic and Atmospheric Administration, Boulder CO 80305, United States; Department of Geography, Johannes Gutenberg University, Mainz 55099, Germany; Xishuangbanna Tropical Botanical Garden, Chinese Academy of Sciences, Yunnan 666303, China; Faculty of Science, Nepal Academy of Science and Technology, Khumaltar, GPO Box 3323, Lalitpur, Nepal; Institute of Geographical Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China; School of Earth Sciences, University of Melbourne, Melbourne VIC 3010, Australia; Departamento Astrofísica y CC de la Atmósfera, Universidad Complutense de Madrid, Madrid 28040, Spain; Lemaitre Center for Earth and Climate Research, Earth and Life Institute, Université Catholique de Louvain, Louvain-la-Neuve 1348, Belgium; School of Geography, Archaeology and Environmental Studies, University of the Witwatersrand, Wits 2050, South Africa; Hydrologic Research Center, San Diego CA 92130, United States; Oeschger Centre for Climate Change Research, Institute of Geography, University of Bern, Bern 3012, Switzerland; Department of Environmental Sciences, University of Helsinki, Helsinki 00014, Finland; School of Earth Sciences and Environmental Sustainability, Northern Arizona University, Flagstaff AZ 86011, United States; International Project Office, Past Global Changes (PAGES), Bern 3012, Switzerland; Department of Symbiotic System Science, Fukushima University, Fukushima 960-1248, Japan; Department of Physical Geography and Quaternary Geology, Stockholm University, Stockholm 106 91, Sweden; Laboratoire d'Oceanographie et du Climat: Experimentations et Approches Numeriques, Université Pierre et Marie Curie, Paris cedex 575252, France; Department of History, Stockholm University, Stockholm 106 91, Sweden; National Institute of Water and Atmospheric Research Ltd., National Climate Centre, Auckland 1011, New Zealand; Department of Geography, Climatology, Climate Dynamics and Climate Change, Justus Liebig University, Giessen 35390, Germany; Laboratoire des Science du Climat et de l'Environnement, Gif-sur-Yvette 91 191, France; Department of Geography, Swansea University, Swansea SA2 8PP, United Kingdom; Desert Research Institute, Nevada System of Higher Education, Reno NV 89512, United States; Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales (IANIGLA), CCT-CONICET-Mendoza, Mendoza 5500, Argentina; British Antarctic Survey, Cambridge CB3 0ET, United Kingdom; Department of Earth and Environmental Sciences, Nagoya University, Nagoya 464-8601, Japan; School of Environment and Technology, University of Brighton, Brighton BN2 4GJ, United Kingdom; Department of Earth, Ocean and Atmospheric Sciences, Florida State University, Tallahassee FL 32308, United States; Department of Glaciology, Alfred Wegener Institute for Polar and Marine Research in the Helmholtz Association, Bremerhaven 27570, Germany; College of Life and Environmental Sciences, University of Exeter, Exeter EX4 4RJ, United Kingdom; Climate Change Research Centre, University of New South Wales, Sydney NSW 2052, Australia; ARC Centre of Excellence for Climate System Science, University of New South Wales, Sydney NSW 2052, Australia; Centro de Estudios Cientificos, Valdivia, Chile; Department of Chemistry Ugo Schiff, University of Florence, Sesto Fiorentino 50019, Italy; Jackson School of Geosciences, University of Texas at Austin, Austin TX 78712, United States; LASG, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China; Institute of Geography, Russian Academy of Sciences, Moscow 119017, Russian Federation; Department of Earth and Space Sciences, University of Washington, Seattle WA 98195, United States; National Centre for Antarctic and Ocean Research, Goa 403 804, India; Laboratory of Tree-Ring Research, University of Arizona, Tucson AZ 85721, United States; Department of Biology, Ghent University, Ghent 9000, Belgium; Department of Geography, University of Ottawa, Ottawa K1N 6N5, Canada; Niels Bohr Institute, University of Copenhagen, Copenhagen 2100, Denmark; Institute for Coastal Research, Helmholtz-Zentrum Geesthacht, Geesthacht 21502, Germany; National Climatic Data Center, National Oceanic and Atmospheric Administration, Boulder CO 80305, United States; Institute of Arctic and Alpine Research, University of Colorado, Boulder CO 80309, United States; Department of Forest Science, Shinshu University, Nagano 399-4598, Japan

Recommended Citation:
Ahmed M.,Anchukaitis K.J.,Asrat A.,et al. Continental-scale temperature variability during the past two millennia[J]. Nature Geoscience,2013-01-01,6(5)
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