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Characteristics of rainfall events in regional climate model simulations for the Czech Republic

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00020711%3A_____%2F17%3A00004617" target="_blank" >RIV/00020711:_____/17:00004617 - isvavai.cz</a>

  • Alternative codes found

    RIV/68378289:_____/17:00471342 RIV/60460709:41330/17:73565

  • Result on the web

    <a href="https://www.hydrol-earth-syst-sci.net/21/963/2017/" target="_blank" >https://www.hydrol-earth-syst-sci.net/21/963/2017/</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.5194/hess-21-963-2017" target="_blank" >10.5194/hess-21-963-2017</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Characteristics of rainfall events in regional climate model simulations for the Czech Republic

  • Original language description

    Characteristics of rainfall events in an ensemble of 23 regional climate model (RCM) simulations are evaluated against observed data in the Czech Republic for the period 1981-2000. Individual rainfall events are identified using the concept of minimum inter-event time (MIT) and only heavy events (15 % of events with the largest event depths) during the warm season (May-September) are considered. . Inasmuch as an RCM grid box represents a spatial average, the effects of areal averaging of rainfall data on characteristics of events are investigated using the observed data. Rainfall events from the RCM simulations are then compared to those from the at-site and area-average observations. Simulated number of heavy events and seasonal total precipitation due to heavy events are on average represented relatively well despite the higher spatial variation compared to observations. RCM-simulated event depths are comparable to the area-average observations, while event durations are overestimated and other characteristics related to rainfall intensity are significantly underestimated. The differences between RCM-simulated and at-site observed rainfall event characteristics are in general dominated by the biases of the climate models rather than the areal-averaging effect. Most of the rainfall event characteristics in the majority of the RCM simulations show a similar altitude-dependence pattern as in the observed data. The number of heavy events and seasonal total precipitation due to heavy events increase with altitude, and this dependence is captured better by the RCM simulations with higher spatial resolution.

  • Czech name

  • Czech description

Classification

  • Type

    J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database

  • CEP classification

  • OECD FORD branch

    10500 - Earth and related environmental sciences

Result continuities

  • Project

    <a href="/en/project/VG20122015092" target="_blank" >VG20122015092: Erosion runoff - increased risk of the residents and the water quality exposure in the context of the expected climate change</a><br>

  • Continuities

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

Others

  • Publication year

    2017

  • Confidentiality

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

Data specific for result type

  • Name of the periodical

    Hydrology and Earth System Sciences

  • ISSN

    1027-5606

  • e-ISSN

    1607-7938

  • Volume of the periodical

    21

  • Issue of the periodical within the volume

    2

  • Country of publishing house

    DE - GERMANY

  • Number of pages

    18

  • Pages from-to

    963-980

  • UT code for WoS article

    000395162900003

  • EID of the result in the Scopus database