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DOI10.1126/science.1120514
The spatial extent of 20th-century warmth in the context of the past 1200 years
Osborn T.J.; Briffa K.R.
发表日期2006
ISSN0036-8075
起始页码841
结束页码844
卷号311期号:5762
英文摘要Periods of widespread warmth or cold are identified by positive or negative deviations that are synchronous across a number of temperature-sensitive proxy records drawn from the Northern Hemisphere, the most significant and longest duration feature during the last 1200 years is the geographical extent of warmth in the middle to late 20th century. Positive anomalies during 890 to 1170 and negative anomalies during 1580 to 1850 are consistent with the concepts of a Medieval Warm Period and a Little Ice Age, but comparison with instrumental temperatures shows the spatial extent of recent warmth to be of greater significance than that during the medieval period.
英文关键词Atmospheric thermodynamics; Temperature distribution; Thermal effects; Negative deviations; Temperature-sensitive proxy records; Warmth; Environmental engineering; global warming; spatial distribution; twentieth century; article; climate change; environmental impact; geography; geological time; global climate; priority journal; temperature sensitivity
语种英语
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/244957
作者单位Climatic Research Unit, School of Environmental Sciences, University of East Anglia, Norwich NR4 7TJ, United Kingdom
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Osborn T.J.,Briffa K.R.. The spatial extent of 20th-century warmth in the context of the past 1200 years[J],2006,311(5762).
APA Osborn T.J.,&Briffa K.R..(2006).The spatial extent of 20th-century warmth in the context of the past 1200 years.Science,311(5762).
MLA Osborn T.J.,et al."The spatial extent of 20th-century warmth in the context of the past 1200 years".Science 311.5762(2006).
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