Quantifying risks avoided by limiting global warming to 1.5 or 2 °C above pre-industrial levels

被引:0
|
作者
Rachel Warren
Oliver Andrews
Sally Brown
Felipe J. Colón-González
Nicole Forstenhäusler
David E. H. J. Gernaat
P. Goodwin
Ian Harris
Yi He
Chris Hope
Desmond Manful
Timothy J. Osborn
Jeff Price
Detlef Van Vuuren
Rebecca Mary Wright
机构
[1] University of East Anglia,Tyndall Centre for Climate Change Research, School of Environmental Sciences
[2] University of Bristol,School of Geographical Sciences
[3] Bournemouth University,Department of Life and Environment Sciences
[4] London School of Hygiene and Tropical Medicine,Department of Infectious Disease Epidemiology
[5] PBL Netherlands Environmental Assessment Agency,School of Ocean and Earth Sciences
[6] University of Southampton,Climatic Research Unit, School of Environmental Sciences
[7] University of East Anglia,Judge Business School
[8] University of Cambridge,Copernicus Institute for Sustainable Development
[9] Utrecht University,undefined
来源
Climatic Change | 2022年 / 172卷
关键词
Climate change; Mitigation; Paris Agreement; Avoided impacts; Economic damages; Fluvial flooding; Hotspots;
D O I
暂无
中图分类号
学科分类号
摘要
The Paris Agreement aims to constrain global warming to ‘well below 2 °C’ and to ‘pursue efforts’ to limit it to 1.5 °C above pre-industrial levels. We quantify global and regional risk-related metrics associated with these levels of warming that capture climate change–related changes in exposure to water scarcity and heat stress, vector-borne disease, coastal and fluvial flooding and projected impacts on agriculture and the economy, allowing for uncertainties in regional climate projection. Risk-related metrics associated with 2 °C warming, depending on sector, are reduced by 10–44% globally if warming is further reduced to 1.5 °C. Comparing with a baseline in which warming of 3.66 °C occurs by 2100, constraining warming to 1.5 °C reduces these risk indicators globally by 32–85%, and constraining warming to 2 °C reduces them by 26–74%. In percentage terms, avoided risk is highest for fluvial flooding, drought, and heat stress, but in absolute terms risk reduction is greatest for drought. Although water stress decreases in some regions, it is often accompanied by additional exposure to flooding. The magnitude of the percentage of damage avoided is similar to that calculated for avoided global economic risk associated with these same climate change scenarios. We also identify West Africa, India and North America as hotspots of climate change risk in the future.
引用
收藏
相关论文
共 50 条
  • [21] Risks for the global freshwater system at 1.5 °C and 2 °C global warming
    Doell, Petra
    Trautmann, Tim
    Gerten, Dieter
    Schmied, HannesMueller
    Ostberg, Sebastian
    Saaed, Fahad
    Schleussner, Carl-Friedrich
    ENVIRONMENTAL RESEARCH LETTERS, 2018, 13 (04):
  • [22] Multimodel assessment of flood characteristics in four large river basins at global warming of 1.5, 2.0 and 3.0 K above the pre-industrial level
    Huang, Shaochun
    Kumar, Rohini
    Rakovec, Oldrich
    Aich, Valentin
    Wang, Xiaoyan
    Samaniego, Luis
    Liersch, Stefan
    Krysanova, Valentina
    ENVIRONMENTAL RESEARCH LETTERS, 2018, 13 (12):
  • [23] Storylines of the 2018 Northern Hemisphere heatwave at pre-industrial and higher global warming levels
    Wehrli, Kathrin
    Hauser, Mathias
    Seneviratne, Sonia, I
    EARTH SYSTEM DYNAMICS, 2020, 11 (04) : 855 - 873
  • [24] The sensitivity of the Indian summer monsoon to a global warming of 2A°C with respect to pre-industrial times
    May, Wilhelm
    CLIMATE DYNAMICS, 2011, 37 (9-10) : 1843 - 1868
  • [25] Potential impacts of global warming levels 1.5°C and above on climate extremes in Botswana
    Akinyemi, Felicia O.
    Abiodun, Babatunde J.
    CLIMATIC CHANGE, 2019, 154 (3-4) : 387 - 400
  • [26] Potential impacts of global warming levels 1.5 °C and above on climate extremes in Botswana
    Felicia O. Akinyemi
    Babatunde J. Abiodun
    Climatic Change, 2019, 154 : 387 - 400
  • [27] Reduced heat exposure by limiting global warming to 1.5 °C
    King, Andrew D.
    Donat, Markus G.
    Lewis, Sophie C.
    Henley, Benjamin J.
    Mitchell, Daniel M.
    Stott, Peter A.
    Fischer, Erich M.
    Karoly, David J.
    NATURE CLIMATE CHANGE, 2018, 8 (07) : 549 - 551
  • [28] Reduced heat exposure by limiting global warming to 1.5 °C
    Andrew D. King
    Markus G. Donat
    Sophie C. Lewis
    Benjamin J. Henley
    Daniel M. Mitchell
    Peter A. Stott
    Erich M. Fischer
    David J. Karoly
    Nature Climate Change, 2018, 8 : 549 - 551
  • [29] Sea level rise from melting glaciers and ice sheets caused by climate warming above pre-industrial levels
    Rignot, E.
    PHYSICS-USPEKHI, 2021, 65 (11) : 1129 - 1138
  • [30] European climate change at global mean temperature increases of 1.5 and 2 °C above pre-industrial conditions as simulated by the EURO-CORDEX regional climate models
    Kjellstrom, Erik
    Nikulin, Grigory
    Strandberg, Gustav
    Christensen, Ole Bossing
    Jacob, Daniela
    Keuler, Klaus
    Lenderink, Geert
    van Meijgaard, Erik
    Schar, Christoph
    Somot, Samuel
    Sorland, Silje Lund
    Teichmann, Claas
    Vautard, Robert
    EARTH SYSTEM DYNAMICS, 2018, 9 (02) : 459 - 478