Vertical profiles of wind speed over a mountain ridge

Measurements of vertical profiles of wind speed on the ridge of the Erz Mountains (Erzgebirge) were performed during the year 2000 with a Doppler sodar located near the village Dlouha´ Louka. The ridge is highly asymmetrical looking as a large escarpment. The vertical profile was studied for two cla...

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Main Authors: Jaroslav Svoboda, Jiří Čermák
Format: Article
Language:English
Published: Borntraeger 2002-10-01
Series:Meteorologische Zeitschrift
Online Access:http://dx.doi.org/10.1127/0941-2948/2002/0011-0361
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author Jaroslav Svoboda
Jiří Čermák
author_facet Jaroslav Svoboda
Jiří Čermák
author_sort Jaroslav Svoboda
collection DOAJ
description Measurements of vertical profiles of wind speed on the ridge of the Erz Mountains (Erzgebirge) were performed during the year 2000 with a Doppler sodar located near the village Dlouha´ Louka. The ridge is highly asymmetrical looking as a large escarpment. The vertical profile was studied for two classes of wind direction: airflow coming from the nearly flat top of the mountain ridge and airflow arising along the steep slope. The shape of the vertical profiles was analysed by statistical methods due to its great variability. Two typical vertical profiles were alternating in time: with and without a local wind speed maximum. The local wind maximum occurred most frequently at a height of 100200 m above terrain ground and was observed more intensively during the down-slope flow over the edge of the mountain ridge.
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spelling doaj.art-c0e3f59e8fd949d280f346946a662ace2024-02-08T08:39:43ZengBorntraegerMeteorologische Zeitschrift0941-29482002-10-0111536136610.1127/0941-2948/2002/0011-036150683Vertical profiles of wind speed over a mountain ridgeJaroslav SvobodaJiří ČermákMeasurements of vertical profiles of wind speed on the ridge of the Erz Mountains (Erzgebirge) were performed during the year 2000 with a Doppler sodar located near the village Dlouha´ Louka. The ridge is highly asymmetrical looking as a large escarpment. The vertical profile was studied for two classes of wind direction: airflow coming from the nearly flat top of the mountain ridge and airflow arising along the steep slope. The shape of the vertical profiles was analysed by statistical methods due to its great variability. Two typical vertical profiles were alternating in time: with and without a local wind speed maximum. The local wind maximum occurred most frequently at a height of 100200 m above terrain ground and was observed more intensively during the down-slope flow over the edge of the mountain ridge.http://dx.doi.org/10.1127/0941-2948/2002/0011-0361
spellingShingle Jaroslav Svoboda
Jiří Čermák
Vertical profiles of wind speed over a mountain ridge
Meteorologische Zeitschrift
title Vertical profiles of wind speed over a mountain ridge
title_full Vertical profiles of wind speed over a mountain ridge
title_fullStr Vertical profiles of wind speed over a mountain ridge
title_full_unstemmed Vertical profiles of wind speed over a mountain ridge
title_short Vertical profiles of wind speed over a mountain ridge
title_sort vertical profiles of wind speed over a mountain ridge
url http://dx.doi.org/10.1127/0941-2948/2002/0011-0361
work_keys_str_mv AT jaroslavsvoboda verticalprofilesofwindspeedoveramountainridge
AT jiricermak verticalprofilesofwindspeedoveramountainridge