Response of the Southern Hemisphere extratropical cyclone climatology to climate intervention with stratospheric aerosol injection

被引:0
|
作者
Reboita, Michelle Simoes [1 ]
Ribeiro, Joao Gabriel Martins [1 ]
Crespo, Natalia Machado [2 ]
da Rocha, Rosmeri Porfirio [3 ]
Odoulami, Romaric C. [4 ]
Sawadogo, Windmanagda [5 ]
Moore, John [6 ]
机构
[1] Univ Fed Itajuba, Inst Recursos Nat, Itajuba, Brazil
[2] Charles Univ Prague, Fac Math & Phys, Dept Atmospher Phys, Prague 18000, Czech Republic
[3] Univ Sao Paulo, Inst Astron Geofis & Ciencias Atmosfer, Sao Paulo, Brazil
[4] Univ Cape Town, African Climate & Dev Initiat, Cape Town, South Africa
[5] Univ Augsburg, Inst Geog, D-86159 Augsburg, Germany
[6] Arctic Ctr U Lapland, Rovaniemi, Finland
来源
ENVIRONMENTAL RESEARCH-CLIMATE | 2024年 / 3卷 / 03期
基金
新加坡国家研究基金会;
关键词
stratospheric aerosol injection; solar radiation modification; extratropical cyclones; future projections; Southern Hemisphere; NUMERICAL SCHEME; DIGITAL DATA; SEA-ICE; BEHAVIOR; SIMULATIONS; PROJECTIONS; CENTERS; WINTER;
D O I
10.1088/2752-5295/ad519e
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Little is known about how climate intervention through stratospheric aerosol injection (SAI) may affect the climatology of the Southern Hemisphere extratropical cyclones under warming scenarios. To address this knowledge gap, we tracked extratropical cyclones from 2015 to 2099 in a set of projections of three international projects: the Assessing Responses and Impacts of Solar Climate Intervention on the Earth System with Stratospheric Aerosol Injection (ARISE), the Stratospheric Aerosol Geoengineering Large Ensemble (GLENS), and the Geoengineering Model Intercomparison Project (GeoMIP/G6sulfur). Comparisons were performed between no-SAI and SAI scenarios as well as between different timeslices and their reference period (2015-2024). Among the findings, both no-SAI and SAI project a decrease in cyclone frequency towards the end of the century although weaker under SAI scenarios. On the other hand, cyclones tend to be stronger under no-SAI scenarios while keeping their intensity more similar to the reference period under SAI scenarios. This means that under SAI scenarios the climatology of cyclones is less affected by global warming than under no-SAI. Other features of these systems, such as travelling distance, lifetime, and mean velocity show small differences between no-SAI and SAI scenarios and between reference and future periods.
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页数:15
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