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Downslope Windstorms in a Sheared Environmental Flow Having Density Decrease with Height
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Observations and modelling of downslope windstorm in Novorossiysk
Dynamics of Atmospheres and Oceans, 2018Abstract We present a comprehensive study of the three-dimensional structure of the Novorossiysk bora, a severe downslope windstorm on the north-eastern coast of the Black Sea. The analysis is based on observational data obtained from the Russian Hydrometeorological Service, automatic weather stations, sodar system, microwave temperature profiler and
Irina Repina +2 more
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Impact of land surface roughness on downslope windstorm modelling in the Arctic
Dynamics of Atmospheres and Oceans, 2021Abstract The article considers the reasons for the underestimation of the wind speed by the WRF-ARW model when simulating downslope windstorms in the Russian Arctic. Simulation results for the Tiksi windstorm, for which sensitivity tests were carried out, appeared to be weakly dependent on the initial and boundary conditions, topography resolution ...
Anna Shestakova
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Winter heat waves characteristics associated with downslope windstorm in south Brazil
International Journal of Climatology, 2023AbstractThe air temperature anomaly was analysed in 16 consecutive winters from 2004 to 2019 in southern Brazil using reanalysis data and hourly atmospheric observations. In this study, 13 heat wave (HW) episodes were identified using the percentile methodology.
Nicolle Cordero Simões Dos Reis +2 more
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A Severe Downslope Windstorm and Aircraft Turbulence Event Induced by a Mountain Wave
Journals of the Atmospheric Sciences, 1978Abstract A detailed analysis is presented of the large-scale, mesoscale and turbulent-scale features of a major downslope windstorm event in central Colorado on 11 January 1972. The storm is found to be associated with a moderate amplitude baroclinic disturbance moving across the northwestern United States within an intense zonal current.
D K Lilly
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An extreme clear air turbulence incidence associated with a strong downslope windstorm
24th Aerospace Sciences Meeting, 1986The meteorological conditions present during an occurrence of clear-air turbulence (CAT) associated with the presence of a mountain wave are documented. The incident caused severe vertical accelerations of two passenger aircraft travelling at 33,000 ft altitude.
R Bach
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Gravity waves induced by a downslope windstorm in modest terrain: a case study
Quarterly Journal of the Royal Meteorological SocietyAbstractThis study examines a typical episode of a downslope windstorm known as “Vento Norte” (VNOR; “North Wind” in Portuguese) in the state of Rio Grande do Sul, Brazil. The temporal and spatial evolution of the VNOR episode is analyzed by means of sonic anemometer data collected at 10 vertical levels on a 30 m tower, two automated weather stations ...
Michel Stefanello +2 more
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Unexpected High Winds in Northern New Jersey: A Downslope Windstorm in Modest Topography
Weather and Forecasting, 2011Abstract This study presents the first evidence for the occurrence of a downslope windstorm in New Jersey. During the early morning hours of 4 January 2009, an unanticipated strong wind event was observed. Despite a zone forecast calling for winds less than 4 m s−1 issued 4 h prior to the event, winds up to 23 m s−1 were reported at High
Steven Decker
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Pulsating Downslope Windstorms
Journal of the Atmospheric Sciences, 1989Abstract The flow configurations that obtain in several severe downslope windstorm events generated over isolated topography are studied using a two-dimensional nonlinear anelastic model. A new high resolution simulation of the 11 January 1972 windstorm in Boulder, Colorado, constructed using a very large model domain, is shown to qualitatively ...
J. F. Scinocca, W. R. Peltier
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The bimodal downslope windstorms at Kvísker
Meteorology and Atmospheric Physics, 2010Downslope windstorms at Kvisker in Southeast Iceland are explored using a mesoscale model, observations and numerical analysis of the atmosphere. Two different types of gravity-wave induced windstorms are identified. At the surface, their main difference is in the horizontal extent of the lee-side accelerated flow.
Hálfdán Ágústsson +1 more
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