Projected Air Temperature Extremes and Maximum Heat Conditions Over the Middle-East-North Africa (MENA) Region

被引:0
作者
Athanasios Ntoumos
Panos Hadjinicolaou
George Zittis
Yiannis Proestos
Jos Lelieveld
机构
[1] The Cyprus Institute,Climate and Atmosphere Research Centre (CARE
[2] 2121,C)
[3] Max Plank Institute for Chemistry,Department of Atmospheric Chemistry
来源
Earth Systems and Environment | 2022年 / 6卷
关键词
Heat extremes; Emission scenarios; Global climate models; Projections; MENA;
D O I
暂无
中图分类号
学科分类号
摘要
This study analyzes projected heat extremes over the Middle-East–North Africa (MENA) region until the end of the twenty-first century with a number of temperature indices based on absolute values and thresholds to describe hot conditions. We use model projected daily near-surface air (2-m) temperature (Tmax\documentclass[12pt]{minimal} \usepackage{amsmath} \usepackage{wasysym} \usepackage{amsfonts} \usepackage{amssymb} \usepackage{amsbsy} \usepackage{mathrsfs} \usepackage{upgreek} \setlength{\oddsidemargin}{-69pt} \begin{document}$$T_\mathrm{{max}}$$\end{document} and Tmin\documentclass[12pt]{minimal} \usepackage{amsmath} \usepackage{wasysym} \usepackage{amsfonts} \usepackage{amssymb} \usepackage{amsbsy} \usepackage{mathrsfs} \usepackage{upgreek} \setlength{\oddsidemargin}{-69pt} \begin{document}$$T_\mathrm{{min}}$$\end{document}) to derive the indices for the period 1980–2100. The data were taken from 18 CMIP5 models combining historical (1980–2005) and scenario runs (2006–2100 under RCP2.6, RCP4.5, and RCP8.5 pathways). Results show a domain-wide projected warming for all emission scenarios. Our findings for a business-as-usual pathway indicate excessive warming of more than 8 ∘\documentclass[12pt]{minimal} \usepackage{amsmath} \usepackage{wasysym} \usepackage{amsfonts} \usepackage{amssymb} \usepackage{amsbsy} \usepackage{mathrsfs} \usepackage{upgreek} \setlength{\oddsidemargin}{-69pt} \begin{document}$$^\circ $$\end{document}C in the northern part of the domain (south Europe) for the annual warmest day (TXx) and night (TNx). In the hottest parts of the domain record high temperatures reached 50 ∘\documentclass[12pt]{minimal} \usepackage{amsmath} \usepackage{wasysym} \usepackage{amsfonts} \usepackage{amssymb} \usepackage{amsbsy} \usepackage{mathrsfs} \usepackage{upgreek} \setlength{\oddsidemargin}{-69pt} \begin{document}$$^\circ $$\end{document}C in the recent past, which could increase to at least 56 ∘\documentclass[12pt]{minimal} \usepackage{amsmath} \usepackage{wasysym} \usepackage{amsfonts} \usepackage{amssymb} \usepackage{amsbsy} \usepackage{mathrsfs} \usepackage{upgreek} \setlength{\oddsidemargin}{-69pt} \begin{document}$$^\circ $$\end{document}C by the end of the century, while temperatures over 50 ∘\documentclass[12pt]{minimal} \usepackage{amsmath} \usepackage{wasysym} \usepackage{amsfonts} \usepackage{amssymb} \usepackage{amsbsy} \usepackage{mathrsfs} \usepackage{upgreek} \setlength{\oddsidemargin}{-69pt} \begin{document}$$^\circ $$\end{document}C are expected to occur in a large part of the MENA region. A significant increase is projected in the number of hot days (TX >40∘\documentclass[12pt]{minimal} \usepackage{amsmath} \usepackage{wasysym} \usepackage{amsfonts} \usepackage{amssymb} \usepackage{amsbsy} \usepackage{mathrsfs} \usepackage{upgreek} \setlength{\oddsidemargin}{-69pt} \begin{document}$$>40^\circ $$\end{document}C) and nights (TN >30∘\documentclass[12pt]{minimal} \usepackage{amsmath} \usepackage{wasysym} \usepackage{amsfonts} \usepackage{amssymb} \usepackage{amsbsy} \usepackage{mathrsfs} \usepackage{upgreek} \setlength{\oddsidemargin}{-69pt} \begin{document}$$>30 ^\circ $$\end{document}C) all over the region. For the period of 2071–2100 excessive hot days and nights will become the normal during summer in large parts of the MENA with some locations expected to exceed 180 and 100 days, respectively. Calculations of the corresponding heat index suggest that several areas across the MENA region may reach temperature levels critical for human survival.
引用
收藏
页码:343 / 359
页数:16
相关论文
共 393 条
[1]  
Almazroui M(2021)Projected changes in climate extremes using CMIP6 simulations over SREX regions Earth Syst Environ 11 22893-22907
[2]  
Saeed F(2011)Observed and model simulated 20th century Arctic temperature variability: Canadian Earth System Model CanESM2 Atmos Chem Phys Discuss 12 2097-2120
[3]  
Saeed S(2013)Historic and future increase in the global land area affected by monthly heat extremes Environ Res Lett 25 6646-6665
[4]  
Ismail M(2020)WFDE5: bias-adjusted ERA5 reanalysis data for impact studies Earth Syst Sci Data 123 6669-6689
[5]  
Ehsan MA(2012)GFDL’s ESM2 global coupled climate-carbon earth system models. Part I: physical formulation and baseline simulation characteristics J Clim 24 4973-4991
[6]  
Islam MN(2018)Seasonal and regional patterns of future temperature extremes: high-resolution dynamic downscaling over a complex terrain J Geophys Res Atmos 5 572-597
[7]  
Abid MA(2011)The community climate system model version 4 J Clim 92 299-341
[8]  
O’Brien E(2013)Climate and carbon cycle changes from 1850 to 2100 in MPI-ESM simulations for the Coupled Model Intercomparison Project phase 5 J Adv Model Earth Syst 24 3520-3544
[9]  
Kamil S(2009)Associations between elevated atmospheric temperature and human mortality: a critical review of the literature Clim Change 7 2039-2064
[10]  
Rashid IU(2011)The GFDL CM3 coupled climate model: characteristics of the ocean and sea ice simulations J Clim 77 279-292