Potential changes in temperature extreme events under global warming at 1.5 °C and 2 °C over Cote d'Ivoire

被引:2
|
作者
N'Datchoh, E. T. [1 ]
Kouadio, K. [1 ,2 ]
Silue, S. [3 ]
Bamba, A. [1 ]
Naabil, E. [4 ]
Dje, K. B. [5 ]
Diedhiou, A. [1 ,6 ]
Sylla, M. B. [7 ]
Anquetin, S. [6 ]
Lennard, C. [8 ]
机构
[1] Univ Felix Houphouet Boigny, LASMES, 22 BP 582, Abidjan 22, Cote Ivoire
[2] Geophys Stn Lamto, BP 31, Ndouci, Cote Ivoire
[3] Univ Peleforo Gon Coulibaly Korhogo, BP 1328, Korhogo, Cote Ivoire
[4] Bolgatanga Tech Univ, Dept Agr Engn, Bolgatanga, Ghana
[5] SODEXAM Direct Meteorologie Natl, 15 BP 990, Abidjan 15, Cote Ivoire
[6] Univ Grenoble Alpes, CNRS, IRD, Grenoble INP,IGE, F-38000 Grenoble, France
[7] African Inst Math Sci AIMS, AIMS Rwanda Ctr, KN 3,POB 7150, Kigali, Rwanda
[8] Univ Cape Town, Dept Environm & Geograp Sci, Cape Town, South Africa
来源
ENVIRONMENTAL RESEARCH-CLIMATE | 2022年 / 1卷 / 01期
关键词
extreme event; temperature; climatic zones; Cote d'Ivoire; global warming level; CLIMATE-CHANGE; ANNUAL CYCLE; PRECIPITATION; AFRICA; RAINFALL;
D O I
10.1088/2752-5295/ac7acb
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
This work investigated the impact of 1.5 degrees C and 2 degrees C of global warming levels (GWLs) above pre-industrial levels on annual and seasonal mean changes in temperature extremes over C & ocirc;te d'Ivoire and its different climatic zones. We used the multi-model Coordinated Regional Climate Downscaling Experiment for Africa of 25 regional climate models under the RCP8.5 scenario. The changes in temperature are quantified relative to the period 1971-2000 based on five Expert Team on Climate Change Detection and Indices indexes namely for warm spells, hot nights, hot days, cold nights and cold days. We show that a global warming of 1.5 degrees C and 2 degrees C will lead to an increase in the frequency of warm days and warm nights and a decrease in the occurrence of cold days and cold nights across C & ocirc;te d'Ivoire in all climatic zones and seasons. More than 80% of the model ensemble members project this change at both GWLs. Moreover, the assessment of differences in GWLs highlights that the difference between the 1.5 degrees C and 2 degrees C thresholds may intensify the changes over all the country, climatic zones and seasons. Therefore this 0.5 degrees C difference in global warming is likely to impact upon energy demand and the agricultural system throughout the country and over all of the seasons. This study provides climate information for decision makers related to sectors such as agriculture, energy in their adaptation strategies.
引用
收藏
页数:11
相关论文
共 50 条
  • [31] Future Changes in Extreme High Temperature over China at 1.5°C–5°C Global Warming Based on CMIP6 Simulations
    Guwei Zhang
    Gang Zeng
    Xiaoye Yang
    Zhihong Jiang
    Advances in Atmospheric Sciences, 2021, 38 : 253 - 267
  • [32] Projected changes in population exposure to extreme precipitation events over Central Africa under the global warming levels of 1.5 °C and 2 °C: insights from CMIP6 simulations
    Ngavom, Zakariahou
    Fotso-Nguemo, Thierry C.
    Vondou, Derbetini A.
    Fotso-Kamga, Gabriel
    Zebaze, Sinclaire
    Yepdo, Zephirin D.
    Diedhiou, Arona
    MODELING EARTH SYSTEMS AND ENVIRONMENT, 2024, : 5753 - 5769
  • [33] Regional hotspots of temperature extremes under 1.5 °C and 2 °C of global mean warming
    Lewis, Sophie C.
    King, Andrew D.
    Perkins-Kirkpatrick, Sarah E.
    Mitchell, Daniel M.
    WEATHER AND CLIMATE EXTREMES, 2019, 26
  • [34] Extreme precipitation over East Asia under 1.5°C and 2°C global warming targets: a comparison of stabilized and overshoot projections
    Li, Donghuan
    Zhou, Tianjun
    Zhang, Wenxia
    ENVIRONMENTAL RESEARCH COMMUNICATIONS, 2019, 1 (08):
  • [35] Changes in mean and extreme climates over China with a 2°C global warming
    Lang XianMei
    Sui Yue
    CHINESE SCIENCE BULLETIN, 2013, 58 (12): : 1453 - 1461
  • [36] Changes in climate extremes over West and Central Africa at 1.5 °C and 2 °C global warming
    Diedhiou, Arona
    Bichet, Adeline
    Wartenburger, Richard
    Seneviratne, Sonia, I
    Rowell, David P.
    Sylla, Mouhamadou B.
    Diallo, Ismaila
    Todzo, Stella
    Toure, N'datchoh E.
    Camara, Moctar
    Ngatchah, Benjamin Ngounou
    Kane, Ndjido A.
    Tall, Laure
    Affholder, Francois
    ENVIRONMENTAL RESEARCH LETTERS, 2018, 13 (06):
  • [37] Projected climate over the Greater Horn of Africa under 1.5 °C and 2 °C global warming
    Osima, Sarah
    Indasi, Victor S.
    Zaroug, Modathir
    Endris, Hussen Seid
    Gudoshava, Masilin
    Misiani, Herbert O.
    Nimusiima, Alex
    Anyah, Richard O.
    Otieno, George
    Ogwang, Bob A.
    Jain, Suman
    Kondowe, Alfred L.
    Mwangi, Emmah
    Lennard, Chris
    Nikulin, Grigory
    Dosio, Alessandro
    ENVIRONMENTAL RESEARCH LETTERS, 2018, 13 (06):
  • [38] Future Changes in Extreme High Temperature over China at 1.5°C-5°C Global Warming Based on CMIP6 Simulations
    Zhang, Guwei
    Zeng, Gang
    Yang, Xiaoye
    Jiang, Zhihong
    ADVANCES IN ATMOSPHERIC SCIENCES, 2021, 38 (02) : 253 - 267
  • [39] Projected Changes in Snow Water Equivalent over the Tibetan Plateau under Global Warming of 1.5° and 2°C
    You, Qinglong
    Wu, Fangying
    Wang, Hongguo
    Jiang, Zhihong
    Pepin, Nick
    Kang, Shichang
    JOURNAL OF CLIMATE, 2020, 33 (12) : 5141 - 5154
  • [40] Hot spots of extreme precipitation change under 1.5 and 2 °C global warming scenarios
    Xu, Lianlian
    Wang, Aihui
    Yu, Wei
    Yang, Song
    WEATHER AND CLIMATE EXTREMES, 2021, 33