Heat wave magnitude over India under changing climate: Projections from CMIP5 and CMIP6 experiments

被引:44
|
作者
Das, Jew [1 ]
Umamahesh, Nanduri Venkata [1 ]
机构
[1] Natl Inst Technol Warangal, Dept Civil Engn, Warangal, Telangana, India
关键词
climate extreme; CMIP5; CMIP6; HWMI; India; MULTIMODEL ENSEMBLE; EXTREMES; MODEL; HEATWAVES; DROUGHTS; IMPACT;
D O I
10.1002/joc.7246
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Atmospheric warming is expected to increase the magnitude and frequency of extreme climatic events namely floods, droughts, heat waves, and so on. Thus, the present study attempts to answer the following research questions; (i) What are the possible implications on future heat wave events due to the projected temperature? (ii) What are the expected changes in heat wave properties under different classifications of heat wave events under different climate scenarios? (iii) Whether the future projection of heat wave events differ significantly under CMIP5 and CMIP6 experiments over India? To answer the above questions, the present study uses the bias-corrected future projections of maximum temperature (Tmax) from 26 GCMs that is, 13 from CMIP5 and 13 from CMIP6 experiments. In addition, two RCPs (4.5 and 8.5) under CMIP5 and four SSPs (126, 245, 370, and 585) under CMIP6 scenarios are considered. The Heat Wave Magnitude Index (HWMI) is used to characterize the heat wave over India. The essential findings from the study indicate that the Tmax anomaly is likely to increase (SSP126 < SSP245 < SSP370 < SSP585 and RCP4.5 < RCP8.5) in future causing more intense, high frequency, and long duration heat wave events over India. Presently unaffected large regions of southern, northeast, and western parts are expected to be severely affected by heat wave events. More intense heat wave events are likely to occur under RCP8.5 scenario as compared to SSP585 scenario. The percentage of affected area is projected to increase significantly from SSP126 to SSP585 under extreme and very extreme heat wave events. Under RCP8.5 scenario, the average duration of heat wave events for very extreme, and super extreme classifications is significantly higher than SSP585 scenario. Our findings suggest the paramount necessity of adaptation strategies to address the adverse consequences of foreseen heat wave events.
引用
收藏
页码:331 / 351
页数:21
相关论文
共 50 条
  • [41] Regional climate projections of daily extreme temperatures in Argentina applying statistical downscaling to CMIP5 and CMIP6 models
    Balmaceda-Huarte, Rocio
    Olmo, Matias Ezequiel
    Bettolli, Maria Laura
    CLIMATE DYNAMICS, 2024, 62 (06) : 4997 - 5018
  • [42] A comparison of CMIP6 and CMIP5 projections for precipitation to observational data: the case of Northeastern Iran
    Yasin Zamani
    Seyed Arman Hashemi Monfared
    Mehdi Azhdari moghaddam
    Mohsen Hamidianpour
    Theoretical and Applied Climatology, 2020, 142 : 1613 - 1623
  • [43] An assessment of temperature simulations by CMIP6 climate models over the Tibetan Plateau and differences with CMIP5 climate models
    Hu, Qin
    Hua, Wei
    Yang, Kaiqing
    Ming, Jing
    Ma, Pan
    Zhao, Yong
    Fan, Guangzhou
    THEORETICAL AND APPLIED CLIMATOLOGY, 2022, 148 (1-2) : 223 - 236
  • [44] An assessment of temperature simulations by CMIP6 climate models over the Tibetan Plateau and differences with CMIP5 climate models
    Qin Hu
    Wei Hua
    Kaiqing Yang
    Jing Ming
    Pan Ma
    Yong Zhao
    Guangzhou Fan
    Theoretical and Applied Climatology, 2022, 148 : 223 - 236
  • [45] On the heat waves over India and their future projections under different SSP scenarios from CMIP6 models
    Norgate, Marc
    Tiwari, P. R.
    Das, Sushant
    Kumar, D.
    INTERNATIONAL JOURNAL OF CLIMATOLOGY, 2024, 44 (03) : 973 - 995
  • [46] Comparison of CMIP5 and CMIP6 GCM performance for flood projections in the Mekong River Basin
    Try, Sophal
    Tanaka, Shigenobu
    Tanaka, Kenji
    Sayama, Takahiro
    Khujanazarov, Temur
    Oeurng, Chantha
    JOURNAL OF HYDROLOGY-REGIONAL STUDIES, 2022, 40
  • [47] Differences between CMIP6 and CMIP5 Models in Simulating Climate over China and the East Asian Monsoon
    Dabang Jiang
    Dan Hu
    Zhiping Tian
    Xianmei Lang
    Advances in Atmospheric Sciences, 2020, 37 : 1102 - 1118
  • [48] A comparison of CMIP6 and CMIP5 projections for precipitation to observational data: the case of Northeastern Iran
    Zamani, Yasin
    Hashemi Monfared, Seyed Arman
    Azhdari Moghaddam, Mehdi
    Hamidianpour, Mohsen
    THEORETICAL AND APPLIED CLIMATOLOGY, 2020, 142 (3-4) : 1613 - 1623
  • [49] Extreme climate changes over three major river basins in China as seen in CMIP5 and CMIP6
    Xian Zhu
    Shao-Yi Lee
    Xiaohang Wen
    Zhenming Ji
    Lei Lin
    Zhigang Wei
    Zhiyuan Zheng
    Danya Xu
    Wenjie Dong
    Climate Dynamics, 2021, 57 : 1187 - 1205
  • [50] Emergent constraints on equilibrium climate sensitivity in CMIP5: do they mid for CMIP6?
    Schlund, Manuel
    Lauer, Axel
    Gentine, Pierre
    Sherwood, Steven C.
    Eyring, Veronika
    EARTH SYSTEM DYNAMICS, 2020, 11 (04) : 1233 - 1258