Počet záznamů: 1  

Effect of extreme precipitation event properties on the forecast skill

  1. 1.
    SYSNO ASEP0493446
    Druh ASEPA - Abstrakt
    Zařazení RIVZáznam nebyl označen do RIV
    Zařazení RIVNení vybrán druh dokumentu
    NázevEffect of extreme precipitation event properties on the forecast skill
    Tvůrce(i) Kašpar, Marek (UFA-U) RID, ORCID
    Bližňák, Vojtěch (UFA-U) RID, ORCID
    Müller, Miloslav (UFA-U) RID, ORCID
    Zacharov, Petr (UFA-U)
    Celkový počet autorů4
    Zdroj.dok.EMS Annual Meeting Abstracts, Vol. 15. - Berlín : European Meteorological Society, 2018
    Poč.str.1 s.
    Forma vydáníOnline - E
    AkceEMS Annual Meeting: European Conference for Applied Meteorology and Climatology 2018
    Datum konání03.09.2018 - 07.09.2018
    Místo konáníBudapest
    ZeměHU - Maďarsko
    Typ akceWRD
    Jazyk dok.eng - angličtina
    Země vyd.DE - Německo
    Klíč. slovaprecipitation climatology ; extreme precipitation ; forecast skill ; verification ; reanalysis
    Vědní obor RIVDG - Vědy o atmosféře, meteorologie
    Obor OECDMeteorology and atmospheric sciences
    Institucionální podporaUFA-U - RVO:68378289
    AnotacePrecipitation extremes naturally belong to the most studied meteorological and climatological hazards because of
    their impacts on the human society. The skill of the quantitative precipitation forecast is often insufficient to
    predict accurately and consistently their location, amount, type, and timing. We show the first
    results for the territory of the Czech Republic (CR) by presenting representative, mostly recent case studies where we analyze the dependence between the forecast skill and the extremeness characteristics of the events including accompanying circulation conditions.
    Extreme precipitation events (EPEs) is selected by the Weather Extremity Index (WEI), an advanced tool which
    combines the rarity of totals, extent and duration. The WEI is calculated from 1-day totals within the CR and separately within 11 catchments each covering the area of approximately 7000 km2. Selected EPEs are re-forecasted with the horizontal resolution of 2.8 km by the NWP model COSMO,the non-hydrostatic, compressible model which is able to resolve and explicitly simulate larger elements of organized convection. In order to evaluate the forecast skill, various spatial verification methods are used. Verification data comprise daily totals from rain gauge measurements from approximately 700 stations,precipitation intensities from a couple of pluviographs (since 1960) and radar measurements (since 2002).
    Next,accompanying circulation conditions are investigated by the method of anomalies, according to our experiences an appropriate approach using the NCEP/NCAR Reanalysis dataset. Frequency analysis of various thermodynamic variables is carried out in each grid box. An anomaly in a variable is determined as a contiguous space where probabilities of exceeding are nearing 0 or 1. The anomalies are characterized by their magnitude, extent, and duration. We assume that the conditional extremity of the circulation pattern will be the main explanatory variable of the forecast uncertainty.
    PracovištěÚstav fyziky atmosféry
    KontaktKateřina Adamovičová, adamovicova@ufa.cas.cz, Tel.: 272 016 012 ; Kateřina Potužníková, kaca@ufa.cas.cz, Tel.: 272 016 019
    Rok sběru2019
Počet záznamů: 1  

  Tyto stránky využívají soubory cookies, které usnadňují jejich prohlížení. Další informace o tom jak používáme cookies.