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Spatial modelling of summer climate indices based on local climate zones: expected changes in the future climate of Brno, Czech Republic

Identifikátory výsledku

  • Kód výsledku v IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F86652079%3A_____%2F19%3A00499866" target="_blank" >RIV/86652079:_____/19:00499866 - isvavai.cz</a>

  • Nalezeny alternativní kódy

    RIV/67985807:_____/19:00499866 RIV/00216224:14310/19:00109520 RIV/61989592:15310/19:73596809

  • Výsledek na webu

    <a href="http://dx.doi.org/10.1007/s10584-018-2353-5" target="_blank" >http://dx.doi.org/10.1007/s10584-018-2353-5</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1007/s10584-018-2353-5" target="_blank" >10.1007/s10584-018-2353-5</a>

Alternativní jazyky

  • Jazyk výsledku

    angličtina

  • Název v původním jazyce

    Spatial modelling of summer climate indices based on local climate zones: expected changes in the future climate of Brno, Czech Republic

  • Popis výsledku v původním jazyce

    With global climate change ongoing, there is growing concern about future living conditions in urban areas. This contribution presents the modelled spatial distribution of two daytime (summer days, hot days), and two night-time (warm nights and tropical nights) summer climate indices in the recent and future climate of the urban environment of Brno, Czech Republic, within the framework of local climate zones (LCZs). The thermodynamic MUKLIMO_3 model combined with the CUBOID method is used for spatial modelling. Climate indices are calculated from measurements over three periods (1961–1990, 1971–2000 and 1981–2010). The EURO-CORDEX database for two periods (2021–2050 and 2071–2100) and three representative concentration pathway (RCP) scenarios (2.6, 4.5 and 8.5) are employed to indicate future climate. The results show that the values of summer climate indices will significantly increase in the twenty-first century. In all LCZs, the increase per RCP 8.5 scenario is substantially more pronounced than scenarios per RCP 2.6 and 4.5. Our results indicate that a higher absolute increment in the number of hot days, warm nights and tropical nights is to be expected in already warmer, densely populated midrise and/or compact developments (LCZs 2, 3 and 5) in contrast to a substantially lower increment for forested areas (LCZ A). Considering the projected growth of summer climate indices and the profound differences that exist between LCZs, this study draws urgent attention to the importance of urban planning that works towards moderating the increasing heat stress in central European cities.

  • Název v anglickém jazyce

    Spatial modelling of summer climate indices based on local climate zones: expected changes in the future climate of Brno, Czech Republic

  • Popis výsledku anglicky

    With global climate change ongoing, there is growing concern about future living conditions in urban areas. This contribution presents the modelled spatial distribution of two daytime (summer days, hot days), and two night-time (warm nights and tropical nights) summer climate indices in the recent and future climate of the urban environment of Brno, Czech Republic, within the framework of local climate zones (LCZs). The thermodynamic MUKLIMO_3 model combined with the CUBOID method is used for spatial modelling. Climate indices are calculated from measurements over three periods (1961–1990, 1971–2000 and 1981–2010). The EURO-CORDEX database for two periods (2021–2050 and 2071–2100) and three representative concentration pathway (RCP) scenarios (2.6, 4.5 and 8.5) are employed to indicate future climate. The results show that the values of summer climate indices will significantly increase in the twenty-first century. In all LCZs, the increase per RCP 8.5 scenario is substantially more pronounced than scenarios per RCP 2.6 and 4.5. Our results indicate that a higher absolute increment in the number of hot days, warm nights and tropical nights is to be expected in already warmer, densely populated midrise and/or compact developments (LCZs 2, 3 and 5) in contrast to a substantially lower increment for forested areas (LCZ A). Considering the projected growth of summer climate indices and the profound differences that exist between LCZs, this study draws urgent attention to the importance of urban planning that works towards moderating the increasing heat stress in central European cities.

Klasifikace

  • Druh

    J<sub>imp</sub> - Článek v periodiku v databázi Web of Science

  • CEP obor

  • OECD FORD obor

    10509 - Meteorology and atmospheric sciences

Návaznosti výsledku

  • Projekt

    <a href="/cs/project/LO1415" target="_blank" >LO1415: CzechGlobe 2020 - Rozvoj Centra pro studium dopadů globální změny klimatu</a><br>

  • Návaznosti

    P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Ostatní

  • Rok uplatnění

    2019

  • Kód důvěrnosti údajů

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Údaje specifické pro druh výsledku

  • Název periodika

    Climatic Change

  • ISSN

    0165-0009

  • e-ISSN

  • Svazek periodika

    152

  • Číslo periodika v rámci svazku

    3-4

  • Stát vydavatele periodika

    NL - Nizozemsko

  • Počet stran výsledku

    16

  • Strana od-do

    487-502

  • Kód UT WoS článku

    000462907000011

  • EID výsledku v databázi Scopus

    2-s2.0-85059623227