Recent global temperature "plateau" in the context of a new proxy reconstruction

被引:29
作者
Crowley, Thomas J. [1 ]
Obrochta, Stephen P. [2 ]
Liu, Junhua [3 ]
机构
[1] Braeheads Inst, Renfrew, Scotland
[2] Univ Tokyo, Atmosphere & Ocean Res Inst, Kashiwa, Chiba, Japan
[3] Univ Space Res Assoc, Columbia, MD USA
关键词
Global Warming; Temperature Reconstruction; Natural Variability; ICE CORE; CLIMATE; SURFACE; RECORD;
D O I
10.1002/2013EF000216
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Stable global temperatures of the last 10-15 years have been a topic of considerable discussion. A new proxy extension of the global temperature record enables better placement of this feature in a longer historical perspective. The fixed-grid composite covers the interval 1801-1984, with an extension to 1782, and anchors the global temperature record in the last major cold interval of the Little Ice Age, when carbon dioxide concentration was at preanthropogenic levels. Except for greater and longer cooling (approximately twice the length of Pinatubo) associated with the Tambora eruption, the proxy agrees with the most widely cited previous assessment of global temperature over this interval, lending more confidence to a centennial extension of the global temperature record. The proxy correlation is as high as 0.83 for the interval 1907-1984 (df=8, p=0.001), with the 21st century 1.0 degrees C +/- 0.2 degrees C warmer than the nonvolcanic base state. This remarkable linearity requires a clear theoretical understanding as to how an exceedingly complex system can, on the global average, behave in such a simple way. Removal of the linear radiatively forced component from the global temperature record yields an estimate of natural variability for the last 230 years and indicates no unusual natural variability during the recent 10-15 years. Based on the estimate of unforced variability over the last 170 years, there is about a 40% chance of continued "natural cooling" over the next few years, with about a 10% chance of cooling persisting into the next decade.
引用
收藏
页码:281 / 294
页数:14
相关论文
共 40 条
[1]   Global warming in an independent record of the past 130 years [J].
Anderson, D. M. ;
Mauk, E. M. ;
Wahl, E. R. ;
Morrill, C. ;
Wagner, A. J. ;
Easterling, D. ;
Rutishauser, T. .
GEOPHYSICAL RESEARCH LETTERS, 2013, 40 (01) :189-193
[2]   Sulphate record from a northeast Greenland ice core over the last 1200 years based on continuous flow analysis [J].
Bigler, M ;
Wagenbach, D ;
Fischer, H ;
Kipfstuhl, J ;
Millar, H ;
Sommer, S ;
Stauffer, B .
ANNALS OF GLACIOLOGY, VOL 35, 2002, 35 :250-256
[3]   Reduced sensitivity of recent tree-growth to temperature at high northern latitudes [J].
Briffa, KR ;
Schweingruber, FH ;
Jones, PD ;
Osborn, TJ ;
Shiyatov, SG ;
Vaganov, EA .
NATURE, 1998, 391 (6668) :678-682
[4]   Uncertainty estimates in regional and global observed temperature changes: A new data set from 1850 [J].
Brohan, P. ;
Kennedy, J. J. ;
Harris, I. ;
Tett, S. F. B. ;
Jones, P. D. .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2006, 111 (D12)
[5]   Technical details concerning development of a 1200 yr proxy index for global volcanism [J].
Crowley, T. J. ;
Unterman, M. B. .
EARTH SYSTEM SCIENCE DATA, 2013, 5 (01) :187-197
[6]   Causes of climate change over the past 1000 years [J].
Crowley, TJ .
SCIENCE, 2000, 289 (5477) :270-277
[7]   How warm was the medieval warm period? [J].
Crowley, TJ ;
Lowery, TS .
AMBIO, 2000, 29 (01) :51-54
[8]   The impact of volcanic forcing on tropical temperatures during the past four centuries [J].
D'Arrigo, Rosanne ;
Wilson, Rob ;
Tudhope, Alexander .
NATURE GEOSCIENCE, 2009, 2 (01) :51-56
[9]   The Atlantic multidecadal oscillation and its relation to rainfall and river flows in the continental US [J].
Enfield, DB ;
Mestas-Nuñez, AM ;
Trimble, PJ .
GEOPHYSICAL RESEARCH LETTERS, 2001, 28 (10) :2077-2080
[10]   Evaluating adjusted forcing and model spread for historical and future scenarios in the CMIP5 generation of climate models [J].
Forster, Piers M. ;
Andrews, Timothy ;
Good, Peter ;
Gregory, Jonathan M. ;
Jackson, Lawrence S. ;
Zelinka, Mark .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2013, 118 (03) :1139-1150