Accelerated Recent Warming and Temperature Variability Over the Past Eight Centuries in the Central Asian Altai From Blue Intensity in Tree Rings

被引:25
作者
Davi, N. K. [1 ,2 ]
Rao, M. P. [2 ,3 ]
Wilson, R. [2 ,4 ]
Andreu-Hayles, L. [2 ,5 ,6 ]
Oelkers, R. [2 ,7 ]
D'Arrigo, R. [2 ]
Nachin, B. [2 ,8 ]
Buckley, B. [2 ]
Pederson, N. [9 ]
Leland, C. [2 ]
Suran, B. [10 ]
机构
[1] William Paterson Univ, Dept Environm Sci, Wayne, NJ 07470 USA
[2] Columbia Univ, Lamont Doherty Earth Observ, Tree Ring Lab, Palisades, NY 10964 USA
[3] Univ Corp Atmospher Res, Cooperat Programs Adv Earth Syst Sci, Boulder, CO USA
[4] Univ St Andrews, Sch Earth & Environm Sci, St Andrews, Fife, Scotland
[5] CREAF, Barcelona, Spain
[6] ICREA, Barcelona, Spain
[7] Columbia Univ, Dept Earth & Environm Sci, New York, NY USA
[8] Natl Univ Mongolia, Grad Sch, Ulaanbaatar, Mongolia
[9] Harvard Univ, Harvard Forest, Petersham, MA USA
[10] Natl Univ Mongolia, Sch Engn & Appl Sci, Dept Environm & Forest Engn, Ulaanbaatar, Mongolia
基金
美国国家科学基金会;
关键词
Central Asia; delta blue intensity; dendrochronology; Mongolia; paleoclimate; tree rings; SUPERPOSED EPOCH ANALYSIS; MAXIMUM-LATEWOOD-DENSITY; VOLCANIC-ERUPTIONS; NORTHERN-HEMISPHERE; SUMMER TEMPERATURE; SOUTHERN ALTAI; TIME-SERIES; DENDROCLIMATOLOGY; RECONSTRUCTIONS; CHRONOLOGY;
D O I
10.1029/2021GL092933
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Warming in Central Asia has been accelerating over the past three decades and is expected to intensify through the end of this century. Here, we develop a summer temperature reconstruction for western Mongolia spanning eight centuries (1269-2004 C.E.) using delta blue intensity measurements from annual rings of Siberian larch. A significant cooling response is observed in the year following major volcanic events and up to five years post-eruption. Observed summer temperatures since the 1990s are the warmest over the past eight centuries, an observation that is also well captured in Coupled Model Intercomparison Project (CMIP5) climate model simulations. Projections for summer temperature relative to observations suggest further warming of between similar to 3 degrees C and 6 degrees C by the end of the century (2075-2099 cf. 1950-2004) under the representative concentration pathways 4.5 and 8.5 (RCP4.5 and RCP8.5) emission scenarios. We conclude that projected future warming lies beyond the range of natural climate variability for the past millennium as estimated by our reconstruction.
引用
收藏
页数:11
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