Počet záznamů: 1
Change in the distribution of heavy 1 h precipitation due to temperature changes in measured values, model reanalyses and model simulations of future climate
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SYSNO ASEP 0585124 Druh ASEP J - Článek v odborném periodiku Zařazení RIV J - Článek v odborném periodiku Poddruh J Článek ve WOS Název Change in the distribution of heavy 1 h precipitation due to temperature changes in measured values, model reanalyses and model simulations of future climate Tvůrce(i) Sokol, Zbyněk (UFA-U) RID, ORCID
Řezáčová, Daniela (UFA-U) RID, ORCID
Popová, Jana (UFA-U) RID, ORCIDCelkový počet autorů 3 Číslo článku 107395 Zdroj.dok. Atmospheric Research. - : Elsevier - ISSN 0169-8095
Roč. 304, July (2024)Poč.str. 12 s. Jazyk dok. eng - angličtina Země vyd. NL - Nizozemsko Klíč. slova Clausius Clapeyron scaling ; Scaling of precipitation percentile ; Time shift in temperature and precipitation measurement ; Climate Modelling ; Heavy very shortterm precipitation Vědní obor RIV DG - Vědy o atmosféře, meteorologie Obor OECD Meteorology and atmospheric sciences CEP SS02030040 GA TA ČR - Technologická agentura ČR Způsob publikování Open access Institucionální podpora UFA-U - RVO:68378289 UT WOS 001226124500001 EID SCOPUS 85189858021 DOI 10.1016/j.atmosres.2024.107395 Anotace This article presents main results on how the 1 h precipitation distribution changes, focused on high percentiles, with increasing air temperature based on the data from the Czech territory. The air temperature, the dew point temperature (both measured at 2 m above ground) and the temperature of lifting condensation level are used as temperature characteristics. The change in the distribution of 1 h precipitation measurements is compared with the results of reanalyses based on simulations of numerical weather prediction model ALADIN-CZ and with the results of future climate simulations by climate model ALADIN-CLIMAT-CZ. In general, the increase in precipitation appears clearly in the very upper part of precipitation distribution for high percentiles. Values of the upper percentiles of precipitation increase up to a certain threshold temperature and then decrease, which is also found in other studies. This also applies to the simulations of future climate. The main difference in measured and model results appears at the highest temperature values, which may be implied by the very different number of the model and the measured data. Pracoviště Ústav fyziky atmosféry Kontakt Kateřina Adamovičová, adamovicova@ufa.cas.cz, Tel.: 272 016 012 ; Kateřina Potužníková, kaca@ufa.cas.cz, Tel.: 272 016 019 Rok sběru 2025 Elektronická adresa https://www.sciencedirect.com/science/article/pii/S0169809524001777?via%3Dihub
Počet záznamů: 1