Bora Flow Characteristics in a Complex Valley Environment

This paper complements the existing studies of Bora flow properties in the Vipava valley with the study of Bora turbulence in a lower region of the troposphere. The turbulence characteristics of Bora flow were derived from high resolution Doppler wind lidar measurements during eight Bora wind episod...

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Autores principales: Marija Bervida, Samo Stanič, Griša Močnik, Longlong Wang, Klemen Bergant, Xiaoquan Song
Formato: article
Lenguaje:EN
Publicado: MDPI AG 2021
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Acceso en línea:https://doaj.org/article/c37f597769d5439da34e528f709e1462
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spelling oai:doaj.org-article:c37f597769d5439da34e528f709e14622021-11-11T18:54:49ZBora Flow Characteristics in a Complex Valley Environment10.3390/rs132143632072-4292https://doaj.org/article/c37f597769d5439da34e528f709e14622021-10-01T00:00:00Zhttps://www.mdpi.com/2072-4292/13/21/4363https://doaj.org/toc/2072-4292This paper complements the existing studies of Bora flow properties in the Vipava valley with the study of Bora turbulence in a lower region of the troposphere. The turbulence characteristics of Bora flow were derived from high resolution Doppler wind lidar measurements during eight Bora wind episodes that occurred in November and December 2019. Based on the vertical profiles of wind velocity, from 80 to 180 m above the valley floor, the turbulence intensity related to all three spatial directions and the along-wind integral length scales related to three velocity components were evaluated and compared to the approximations given in international standards. The resulting turbulence characteristics of Bora flow in a deep mountain valley exhibited interesting behaviour, differing from the one expected and suggested by standards. The intensity of turbulence during Bora episodes was found to be quite strong, especially regarding the expected values for that particular category of terrain. The specific relationship between along-wind, lateral and vertical intensity was evaluated as well. The scales of turbulence in the along-wind direction were found to vary widely between different Bora episodes and were rather different from the approximations given by standards, with the most significant deviations observed for the along-wind length scale of the vertical velocity component. Finally, the periodicity of flow structures above the valley was assessed, yielding a wide range of possible periods between 1 and 10 min, thus confirming some of the previous observations from the studies of Bora in the Vipava valley.Marija BervidaSamo StaničGriša MočnikLonglong WangKlemen BergantXiaoquan SongMDPI AGarticleDoppler wind lidarBora windturbulence intensitycomplex terrainturbulence integral length scaleScienceQENRemote Sensing, Vol 13, Iss 4363, p 4363 (2021)
institution DOAJ
collection DOAJ
language EN
topic Doppler wind lidar
Bora wind
turbulence intensity
complex terrain
turbulence integral length scale
Science
Q
spellingShingle Doppler wind lidar
Bora wind
turbulence intensity
complex terrain
turbulence integral length scale
Science
Q
Marija Bervida
Samo Stanič
Griša Močnik
Longlong Wang
Klemen Bergant
Xiaoquan Song
Bora Flow Characteristics in a Complex Valley Environment
description This paper complements the existing studies of Bora flow properties in the Vipava valley with the study of Bora turbulence in a lower region of the troposphere. The turbulence characteristics of Bora flow were derived from high resolution Doppler wind lidar measurements during eight Bora wind episodes that occurred in November and December 2019. Based on the vertical profiles of wind velocity, from 80 to 180 m above the valley floor, the turbulence intensity related to all three spatial directions and the along-wind integral length scales related to three velocity components were evaluated and compared to the approximations given in international standards. The resulting turbulence characteristics of Bora flow in a deep mountain valley exhibited interesting behaviour, differing from the one expected and suggested by standards. The intensity of turbulence during Bora episodes was found to be quite strong, especially regarding the expected values for that particular category of terrain. The specific relationship between along-wind, lateral and vertical intensity was evaluated as well. The scales of turbulence in the along-wind direction were found to vary widely between different Bora episodes and were rather different from the approximations given by standards, with the most significant deviations observed for the along-wind length scale of the vertical velocity component. Finally, the periodicity of flow structures above the valley was assessed, yielding a wide range of possible periods between 1 and 10 min, thus confirming some of the previous observations from the studies of Bora in the Vipava valley.
format article
author Marija Bervida
Samo Stanič
Griša Močnik
Longlong Wang
Klemen Bergant
Xiaoquan Song
author_facet Marija Bervida
Samo Stanič
Griša Močnik
Longlong Wang
Klemen Bergant
Xiaoquan Song
author_sort Marija Bervida
title Bora Flow Characteristics in a Complex Valley Environment
title_short Bora Flow Characteristics in a Complex Valley Environment
title_full Bora Flow Characteristics in a Complex Valley Environment
title_fullStr Bora Flow Characteristics in a Complex Valley Environment
title_full_unstemmed Bora Flow Characteristics in a Complex Valley Environment
title_sort bora flow characteristics in a complex valley environment
publisher MDPI AG
publishDate 2021
url https://doaj.org/article/c37f597769d5439da34e528f709e1462
work_keys_str_mv AT marijabervida boraflowcharacteristicsinacomplexvalleyenvironment
AT samostanic boraflowcharacteristicsinacomplexvalleyenvironment
AT grisamocnik boraflowcharacteristicsinacomplexvalleyenvironment
AT longlongwang boraflowcharacteristicsinacomplexvalleyenvironment
AT klemenbergant boraflowcharacteristicsinacomplexvalleyenvironment
AT xiaoquansong boraflowcharacteristicsinacomplexvalleyenvironment
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