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Temperature and precipitation variability in regional climate models and driving global climate models: Total variance and its temporal-scale components

Identifikátory výsledku

  • Kód výsledku v IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11320%2F19%3A10407375" target="_blank" >RIV/00216208:11320/19:10407375 - isvavai.cz</a>

  • Výsledek na webu

    <a href="https://verso.is.cuni.cz/pub/verso.fpl?fname=obd_publikace_handle&handle=zL5IdfG5rc" target="_blank" >https://verso.is.cuni.cz/pub/verso.fpl?fname=obd_publikace_handle&handle=zL5IdfG5rc</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1002/joc.5876" target="_blank" >10.1002/joc.5876</a>

Alternativní jazyky

  • Jazyk výsledku

    angličtina

  • Název v původním jazyce

    Temperature and precipitation variability in regional climate models and driving global climate models: Total variance and its temporal-scale components

  • Popis výsledku v původním jazyce

    This paper presents an evaluation of the variability and its temporal-scale components of daily air temperature and precipitation simulated by two regional climate models (RCMs) and two driving global climate models (GCMs) from the EURO-CORDEX and CMIP5 projects. The analysis was performed for eight geographical areas of central Europe for the period 1971-2000. After a brief evaluation of total variance, we focus on the ability of the simulations to represent short-term, seasonal and long-term variability components. This analysis was carried out for original time series as well as for series with the annual cycle removed. A fast Fourier transformation and a Kolmogorov-Zurbenko filter were used to separate the three temporal components. The two methods of time series decomposition generally agree, which confirms the robustness of the results. Although the observed total variability of daily air temperature and precipitation is not well represented in many cases and considerable differences among simulations exist, the separation of total variance into the three components is well represented. Regarding the air temperature, the results for the time series with the annual cycle removed are generally somewhat worse than for original series. The simulations tend to underestimate the short-term component of temperature variability, while the results for the other two components are inconclusive. Moreover, it was found that temperature variability caused by the annual cycle is overestimated by the simulation of HadGEM2 GCM and CCLM4-8-17 RCM driven by HadGEM2, which explains the relatively poor results of these simulations regarding air temperature total variance and short-term as well as seasonal components in the original temperature series. The RCMs provide better results than GCMs for temperature total variance but our results are rather inconclusive in the case of precipitation total variance and distribution of the variance of both studied variables into the three temporal components.

  • Název v anglickém jazyce

    Temperature and precipitation variability in regional climate models and driving global climate models: Total variance and its temporal-scale components

  • Popis výsledku anglicky

    This paper presents an evaluation of the variability and its temporal-scale components of daily air temperature and precipitation simulated by two regional climate models (RCMs) and two driving global climate models (GCMs) from the EURO-CORDEX and CMIP5 projects. The analysis was performed for eight geographical areas of central Europe for the period 1971-2000. After a brief evaluation of total variance, we focus on the ability of the simulations to represent short-term, seasonal and long-term variability components. This analysis was carried out for original time series as well as for series with the annual cycle removed. A fast Fourier transformation and a Kolmogorov-Zurbenko filter were used to separate the three temporal components. The two methods of time series decomposition generally agree, which confirms the robustness of the results. Although the observed total variability of daily air temperature and precipitation is not well represented in many cases and considerable differences among simulations exist, the separation of total variance into the three components is well represented. Regarding the air temperature, the results for the time series with the annual cycle removed are generally somewhat worse than for original series. The simulations tend to underestimate the short-term component of temperature variability, while the results for the other two components are inconclusive. Moreover, it was found that temperature variability caused by the annual cycle is overestimated by the simulation of HadGEM2 GCM and CCLM4-8-17 RCM driven by HadGEM2, which explains the relatively poor results of these simulations regarding air temperature total variance and short-term as well as seasonal components in the original temperature series. The RCMs provide better results than GCMs for temperature total variance but our results are rather inconclusive in the case of precipitation total variance and distribution of the variance of both studied variables into the three temporal components.

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

  • Návaznosti

    S - Specificky vyzkum na vysokych skolach<br>I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

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

    International Journal of Climatology

  • ISSN

    0899-8418

  • e-ISSN

  • Svazek periodika

    39

  • Číslo periodika v rámci svazku

    3

  • Stát vydavatele periodika

    GB - Spojené království Velké Británie a Severního Irska

  • Počet stran výsledku

    11

  • Strana od-do

    1276-1286

  • Kód UT WoS článku

    000461606600009

  • EID výsledku v databázi Scopus

    2-s2.0-85055262159