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

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...

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Main Authors: V. Svoboda, M. Hanel, P. Máca, J. Kyselý
Format: Article
Language:English
Published: Copernicus Publications 2017-02-01
Series:Hydrology and Earth System Sciences
Online Access:http://www.hydrol-earth-syst-sci.net/21/963/2017/hess-21-963-2017.pdf
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author V. Svoboda
M. Hanel
P. Máca
J. Kyselý
author_facet V. Svoboda
M. Hanel
P. Máca
J. Kyselý
author_sort V. Svoboda
collection DOAJ
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.
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spelling doaj.art-53b87e9732e14a64afbeb4cdc7ae711e2022-12-22T03:32:47ZengCopernicus PublicationsHydrology and Earth System Sciences1027-56061607-79382017-02-0121296398010.5194/hess-21-963-2017Characteristics of rainfall events in regional climate model simulations for the Czech RepublicV. Svoboda0M. Hanel1P. Máca2J. Kyselý3Faculty of Environmental Sciences, Czech University of Life Sciences Prague, Kamýcká 129, Praha 6 – Suchdol, 165 21, Czech RepublicFaculty of Environmental Sciences, Czech University of Life Sciences Prague, Kamýcká 129, Praha 6 – Suchdol, 165 21, Czech RepublicFaculty of Environmental Sciences, Czech University of Life Sciences Prague, Kamýcká 129, Praha 6 – Suchdol, 165 21, Czech RepublicFaculty of Environmental Sciences, Czech University of Life Sciences Prague, Kamýcká 129, Praha 6 – Suchdol, 165 21, Czech RepublicCharacteristics 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.http://www.hydrol-earth-syst-sci.net/21/963/2017/hess-21-963-2017.pdf
spellingShingle V. Svoboda
M. Hanel
P. Máca
J. Kyselý
Characteristics of rainfall events in regional climate model simulations for the Czech Republic
Hydrology and Earth System Sciences
title Characteristics of rainfall events in regional climate model simulations for the Czech Republic
title_full Characteristics of rainfall events in regional climate model simulations for the Czech Republic
title_fullStr Characteristics of rainfall events in regional climate model simulations for the Czech Republic
title_full_unstemmed Characteristics of rainfall events in regional climate model simulations for the Czech Republic
title_short Characteristics of rainfall events in regional climate model simulations for the Czech Republic
title_sort characteristics of rainfall events in regional climate model simulations for the czech republic
url http://www.hydrol-earth-syst-sci.net/21/963/2017/hess-21-963-2017.pdf
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