2013
DOI: 10.3402/tellusa.v65i0.19206
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Simulations of the Bergen orographic wind shelter

Abstract: A B S T R A C T Even though the coast of western Norway is very windy, the centre of Bergen is rather calm. To gain further understanding of this wind shelter, we study the flow in the complex topography of Bergen during two southwesterly windstorms using surface observations and high-resolution numerical simulations. The results reveal large spatial variability in the local wind field. In some areas, there are periods of sustained winds of more than 25 m s At Florida, situated close to the city centre, both a… Show more

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Cited by 8 publications
(10 citation statements)
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“…This coastal city is located at 60.4 • N and 5.3 • E. The mountains around the city have peak elevations between 284 and 643 m a.s.l. They protect the valley from storms, significantly reducing the surface layer wind speed (Jonassen et al, 2013). The northern location with its weak solar irradiation during wintertime and cold air pooling in lower parts of the relief causes frequently observed but highly local temperature inversions during periods with persistently calm and clear weather.…”
Section: Site Descriptionmentioning
confidence: 99%
“…This coastal city is located at 60.4 • N and 5.3 • E. The mountains around the city have peak elevations between 284 and 643 m a.s.l. They protect the valley from storms, significantly reducing the surface layer wind speed (Jonassen et al, 2013). The northern location with its weak solar irradiation during wintertime and cold air pooling in lower parts of the relief causes frequently observed but highly local temperature inversions during periods with persistently calm and clear weather.…”
Section: Site Descriptionmentioning
confidence: 99%
“…The mean duration of such persistent inversions is 13.1 h. The height of their mean tops was around 220 m asl. The abrupt decrease of the number of inversion episodes with mean tops above 270 m asl might be connected to the local mountain shelter effect [Jonassen et al, 2013]. A few G-inversion episodes coincided with large-scale warm air advection, leading to unusually deep and strong G-inversions where the inversion tops reached levels of above 470 m asl.…”
Section: G-inversionsmentioning
confidence: 99%
“…This view motivated the present analysis of the data set obtained with the microwave temperature profiler MTP‐5HE from March 2011 through February 2013 in the central Bergen valley (60.4°N, 5.3°E), with a population of about 75,000. This rather complex area has been and still is subject to meteorological research [e.g., Jonassen et al ., , ; Valved , ]. The importance of the SBL temperature structure in the Bergen valley was realized decades ago.…”
Section: Introductionmentioning
confidence: 99%
“…While the valley shelters the city from extreme wind events from most directions (Jonassen et al, 2013), it also favours the existence of persistent ground-based temperature inversions during wintertime . In such conditions, the prolonged accumulation of NO 2 from road traffic as the largest source causes exceedances of legally regulated air quality thresholds.…”
Section: Area Of Interest and Local Air Quality Measurementsmentioning
confidence: 99%