Constrained tropical land temperature-precipitation sensitivity reveals decreasing evapotranspiration and faster vegetation greening in CMIP6 projections

被引:11
|
作者
Zhu, Boyuan [1 ,2 ]
Cheng, Yongzhou [1 ,2 ]
Hu, Xuyue [1 ,2 ]
Chai, Yuanfang [3 ]
Berghuijs, Wouter R. [4 ]
Borthwick, Alistair G. L. [5 ,6 ]
Slater, Louise [7 ]
机构
[1] Changsha Univ Sci & Technol, Sch Hydraul & Environm Engn, Changsha 410114, Peoples R China
[2] Key Lab Water Sediment Sci & Water Disaster Preven, Changsha 410114, Peoples R China
[3] Beijing Normal Univ, Fac Geog Sci, State Key Lab Earth Surface Proc & Resource Ecol, Beijing 100875, Peoples R China
[4] Free Univ Amsterdam, Dept Earth Sci, NL-1081 HV Amsterdam, Netherlands
[5] Univ Edinburgh, Sch Engn, Edinburgh EH9 3JL, Scotland
[6] Univ Plymouth, Sch Engn Comp & Math, Plymouth PL4 8AA, England
[7] Univ Oxford, Sch Geog & Environm, Oxford OX1 3QY, England
基金
中国国家自然科学基金; 英国科研创新办公室; 英国自然环境研究理事会;
关键词
EMERGENT CONSTRAINT; CLIMATE SENSITIVITY; CARBON; CYCLE; EVAPORATION; EMISSIONS;
D O I
10.1038/s41612-023-00419-x
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Over the tropical land surface, accurate estimates of future changes in temperature, precipitation and evapotranspiration are crucial for ecological sustainability, but remain highly uncertain. Here we develop a series of emergent constraints (ECs) by using historical and future outputs from the Coupled Model Inter-comparison Project Phase 6 (CMIP6) Earth System Models under the four basic Shared Socio-economic Pathway scenarios (SSP126, SSP245, SSP370, and SSP585). Results show that the temperature sensitivity to precipitation during 2015-2100, which varies substantially in the original CMIP6 outputs, becomes systematically negative across SSPs after application of the EC, with absolute values between -1.10 & DEG;C mm(-1) day and -3.52 & DEG;C mm(-1) day, and with uncertainties reduced by 9.4% to 41.4%. The trend in tropical land-surface evapotranspiration, which was increasing by 0.292 mm yr(-1) in the original CMIP6 model outputs, becomes significantly negative (-0.469 mm yr(-1)) after applying the constraint. Moreover, we find a significant increase of 58.7% in the leaf area index growth rate.
引用
收藏
页数:9
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