Agreement between reconstructed and modeled boreal precipitation of the Last Interglacial

被引:55
|
作者
Scussolini, Paolo [1 ]
Bakker, Pepijn [2 ,3 ]
Guo, Chuncheng [4 ]
Stepanek, Christian [5 ]
Zhang, Qiong [6 ]
Braconnot, Pascale [7 ]
Cao, Jian [8 ]
Guarino, Maria-Vittoria [9 ]
Coumou, Dim [1 ,10 ]
Prange, Matthias [2 ]
Ward, Philip J. [1 ]
Renssen, Hans [11 ]
Kageyama, Masa [7 ]
Otto-Bliesner, Bette [12 ]
Aerts, Jeroen C. J. H. [1 ]
机构
[1] Vrije Univ Amsterdam, Inst Environm Studies, Amsterdam, Netherlands
[2] MARUM, Bremen, Germany
[3] Vrije Univ Amsterdam, Dept Earth Sci, Amsterdam, Netherlands
[4] Bjerknes Ctr Climate Res, NORCE Norwegian Res Ctr, Bergen, Norway
[5] Helmholtz Ctr Polar & Marine Res, Alfred Wegener Inst, Bremerhaven, Germany
[6] Stockholm Univ, Dept Phys Geog, Stockholm, Sweden
[7] Univ Paris Saclay, Lab Sci Climat & Environm, Gif Sur Yvette, France
[8] Nanjing Univ Informat Sci & Technol, Earth Syst Modeling Ctr, Nanjing, Jiangsu, Peoples R China
[9] British Antarctic Survey, Cambridge, England
[10] Potsdam Inst Climate Impact Res, Potsdam, Germany
[11] Univ South Eastern Norway, Bo, Norway
[12] Natl Ctr Atmospher Res, POB 3000, Boulder, CO 80307 USA
基金
瑞典研究理事会; 美国国家科学基金会; 欧洲研究理事会;
关键词
EXPERIMENTAL-DESIGN; PMIP4; CONTRIBUTION; ASIAN MONSOON; TEMPERATURES; SENSITIVITY; PRECESSION; HOLOCENE; PERIODS; VERSION;
D O I
10.1126/sciadv.aax7047
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
The last extended time period when climate may have been warmer than today was during the Last Interglacial (LIG; ca. 129 to 120 thousand years ago). However, a global view of LIG precipitation is lacking. Here, seven new LIG climate models are compared to the first global database of proxies for LIG precipitation. In this way, models are assessed in their ability to capture important hydroclimatic processes during a different climate. The models can reproduce the proxy-based positive precipitation anomalies from the preindustrial period over much of the boreal continents. Over the Southern Hemisphere, proxy-model agreement is partial. In models, LIG boreal monsoons have 42% wider area than in the preindustrial and produce 55% more precipitation and 50% more extreme precipitation. Austral monsoons are weaker. The mechanisms behind these changes are consistent with stronger summer radiative forcing over boreal high latitudes and with the associated higher temperatures during the LIG.
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页数:11
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