Comparison of extreme precipitation characteristics between the Ore Mountains and the Vosges Mountains (Europe)
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F68378289%3A_____%2F18%3A00479286" target="_blank" >RIV/68378289:_____/18:00479286 - isvavai.cz</a>
Výsledek na webu
<a href="http://dx.doi.org/10.1007/s00704-017-2247-x" target="_blank" >http://dx.doi.org/10.1007/s00704-017-2247-x</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1007/s00704-017-2247-x" target="_blank" >10.1007/s00704-017-2247-x</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Comparison of extreme precipitation characteristics between the Ore Mountains and the Vosges Mountains (Europe)
Popis výsledku v původním jazyce
Understanding the characteristics of extreme precipitation events (EPEs) not only helps in mitigating the hazards associated with it but will also reduce the risks by improved planning based on the detailed information, and provide basis for better engineering decisions which can withstand the recurring and likely more frequent events predicted in future in the context of global climate change. In this study, extremity, temporal and spatial characteristics, and synoptic situation of the 54 EPEs that occurred during 1960–2013 were compared between two low mountain ranges situated in Central Europe: the Ore Mountains (OM) and Vosges Mountains (VG). The EPEs were defined using the Weather Extremity Index, which quantifies the extremity, duration, and spatial extent of events. Comparative analysis of EPE characteristics showed that in both regions the EPEs were mostly short (lasted 1–2 days) and their seasonal occurrence significantly depended on the synoptic situation and duration of EPEs: the low was related to summer short EPEs, while zonal circulation to winter long EPEs. The EPEs were generally related to lows in OM and to troughs in VG. The lows often moved to OM from the Mediterranean area, i.e. along the Vb track. However, five EPEs in VG occurred during a low with Vb track significantly deflected westwards. The EPEs in VG affected smaller area as compared to that in OM. The comparison of EPEs between the two low mountain ranges is first of its kind and contributes to the understanding of EPE characteristics in the regions.
Název v anglickém jazyce
Comparison of extreme precipitation characteristics between the Ore Mountains and the Vosges Mountains (Europe)
Popis výsledku anglicky
Understanding the characteristics of extreme precipitation events (EPEs) not only helps in mitigating the hazards associated with it but will also reduce the risks by improved planning based on the detailed information, and provide basis for better engineering decisions which can withstand the recurring and likely more frequent events predicted in future in the context of global climate change. In this study, extremity, temporal and spatial characteristics, and synoptic situation of the 54 EPEs that occurred during 1960–2013 were compared between two low mountain ranges situated in Central Europe: the Ore Mountains (OM) and Vosges Mountains (VG). The EPEs were defined using the Weather Extremity Index, which quantifies the extremity, duration, and spatial extent of events. Comparative analysis of EPE characteristics showed that in both regions the EPEs were mostly short (lasted 1–2 days) and their seasonal occurrence significantly depended on the synoptic situation and duration of EPEs: the low was related to summer short EPEs, while zonal circulation to winter long EPEs. The EPEs were generally related to lows in OM and to troughs in VG. The lows often moved to OM from the Mediterranean area, i.e. along the Vb track. However, five EPEs in VG occurred during a low with Vb track significantly deflected westwards. The EPEs in VG affected smaller area as compared to that in OM. The comparison of EPEs between the two low mountain ranges is first of its kind and contributes to the understanding of EPE characteristics in the regions.
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
I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace
Ostatní
Rok uplatnění
2018
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
Theoretical and Applied Climatology
ISSN
0177-798X
e-ISSN
—
Svazek periodika
133
Číslo periodika v rámci svazku
3-4
Stát vydavatele periodika
AT - Rakouská republika
Počet stran výsledku
20
Strana od-do
1249-1268
Kód UT WoS článku
000438428600043
EID výsledku v databázi Scopus
2-s2.0-85028311966