2016
DOI: 10.26491/mhwm/63636
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Convective and non-convective wind gusts in Poland, 2001-2015

Abstract: The main aim of the article is to present the climatology of the peak wind gust frequency in poland caused by the impact of both atmospheric circulation and the presence of thunderstorm clouds. nine meteorological stations for the measurement period of 2001-2015 were taken into account. only sYnop reports with a peak wind gust higher or equal to 15 m s-1 in thunderstorm and non-thunderstorm days are considered in this study. The results indicate that the highest threat in terms of frequency and strength of pea… Show more

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Cited by 5 publications
(6 citation statements)
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“…(DeCosmo et al 1996;Smith et al 1996). In this way, air continuously exchanges and equilibrates water vapor partial pressures and relative humidity acts as an interactive factor controlling both upward and downward directed water vapor fluxes (Kraus 1972;Yu 2007;Kolendowicz et al 2016;Szwejkowski et al 2017).…”
Section: Water Vapor Impact On Airborne Eddiesmentioning
confidence: 99%
“…(DeCosmo et al 1996;Smith et al 1996). In this way, air continuously exchanges and equilibrates water vapor partial pressures and relative humidity acts as an interactive factor controlling both upward and downward directed water vapor fluxes (Kraus 1972;Yu 2007;Kolendowicz et al 2016;Szwejkowski et al 2017).…”
Section: Water Vapor Impact On Airborne Eddiesmentioning
confidence: 99%
“…Convective wind gusts (CGs) are nontronadic, straight-line winds (Mohr et al, 2017;Yu and Zheng, 2020). They predominantly occur in Eastern China in the warm summer months (Yang et al, 2017), and they are usually associated with thunderstorm clouds, in particular squall lines and supercells, which generate conditions conducive to the appearance of whirlwinds and squalls (Kolendowicz et al, 2016). Severe convective gusts are caused either by mesoscale cold pools associated with horizontal pressure gradients large enough to produce high wind speeds in the absence of strong downdrafts or by local-scale downbursts that create strong divergent horizontal winds near the ground (Wakimoto, 2001).…”
Section: Introductionmentioning
confidence: 99%
“…Convective wind gusts (CGs) are non-tornadic, straight-line winds (Mohr et al, 2017;Yu and Zheng, 2020). They predominantly occur in eastern China in the warm summer months (Yang et al, 2017), and they are usually associated with thunderstorm clouds, particularly squall lines and supercells, which generate conditions conducive to the appearance of whirlwinds and squalls (Kolendowicz et al, 2016). Severe convective gusts are caused either by mesoscale cold pools associated with horizontal pressure gradients large enough to produce high wind speeds in the absence of strong downdrafts or by local-scale downbursts that create strong divergent horizontal winds near the ground (Wakimoto, 2001).…”
Section: Introductionmentioning
confidence: 99%