Experimental Investigation of the Near-Surface Flow Dynamics in Downburst-like Impinging Jets Immersed in ABL-like Winds

Downburst winds are strong downdrafts of cold air that embed into the atmospheric boundary layer (ABL) and produce intense horizontal outflow upon impingement on the ground. They are highly transient and three-dimensional extreme wind phenomena with a limited spatiotemporal structure that often make...

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Main Authors: Federico Canepa, Massimiliano Burlando, Horia Hangan, Djordje Romanic
Format: Article
Language:English
Published: MDPI AG 2022-04-01
Series:Atmosphere
Subjects:
Online Access:https://www.mdpi.com/2073-4433/13/4/621
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author Federico Canepa
Massimiliano Burlando
Horia Hangan
Djordje Romanic
author_facet Federico Canepa
Massimiliano Burlando
Horia Hangan
Djordje Romanic
author_sort Federico Canepa
collection DOAJ
description Downburst winds are strong downdrafts of cold air that embed into the atmospheric boundary layer (ABL) and produce intense horizontal outflow upon impingement on the ground. They are highly transient and three-dimensional extreme wind phenomena with a limited spatiotemporal structure that often makes the anemometric measurements in nature inadequate for reconstructing their complex flow fields. In the framework of the project THUNDERR, an experimental campaign on downburst outflows has been carried out at the WindEEE Dome at Western University, Canada. The present study analyzes the three-dimensional interaction between downburst (DB) outflows produced as large-scale impinging jets and ABL winds. Most experimental, numerical and analytical models in the literature neglect this flow interplay or treat it in an oversimplistic manner through a vector superposition. We found that the generated near-surface outflow is asymmetric, and a high-intensity wind zone develops at the interface between DB and ABL winds. The time variability of the leading edge of the outflow was investigated by synchronizing all wind measurements across the testing chamber. The three-dimensional flow structure was studied using a refined grid of Cobra probes that sampled the flow at high frequencies. The passage of the primary vortex produced a significant decrease in the height of maximum radial wind speed, predominantly in the ABL-streamwise direction. The turbulence intensity was the highest in the region where DB propagates into oppositely directed ABL winds.
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spelling doaj.art-4b3c67dff11b4718bed2e48f7536fa4e2023-12-01T00:47:36ZengMDPI AGAtmosphere2073-44332022-04-0113462110.3390/atmos13040621Experimental Investigation of the Near-Surface Flow Dynamics in Downburst-like Impinging Jets Immersed in ABL-like WindsFederico Canepa0Massimiliano Burlando1Horia Hangan2Djordje Romanic3Department of Civil, Chemical and Environmental Engineering (DICCA), Polytechnic School, University of Genoa, Via Montallegro 1, 16145 Genoa, ItalyDepartment of Civil, Chemical and Environmental Engineering (DICCA), Polytechnic School, University of Genoa, Via Montallegro 1, 16145 Genoa, ItalyWind Engineering, Energy and Environment (WindEEE) Research Institute, Western University, 2535 Advanced Avenue, London, ON N6M 0E2, CanadaWind Engineering, Energy and Environment (WindEEE) Research Institute, Western University, 2535 Advanced Avenue, London, ON N6M 0E2, CanadaDownburst winds are strong downdrafts of cold air that embed into the atmospheric boundary layer (ABL) and produce intense horizontal outflow upon impingement on the ground. They are highly transient and three-dimensional extreme wind phenomena with a limited spatiotemporal structure that often makes the anemometric measurements in nature inadequate for reconstructing their complex flow fields. In the framework of the project THUNDERR, an experimental campaign on downburst outflows has been carried out at the WindEEE Dome at Western University, Canada. The present study analyzes the three-dimensional interaction between downburst (DB) outflows produced as large-scale impinging jets and ABL winds. Most experimental, numerical and analytical models in the literature neglect this flow interplay or treat it in an oversimplistic manner through a vector superposition. We found that the generated near-surface outflow is asymmetric, and a high-intensity wind zone develops at the interface between DB and ABL winds. The time variability of the leading edge of the outflow was investigated by synchronizing all wind measurements across the testing chamber. The three-dimensional flow structure was studied using a refined grid of Cobra probes that sampled the flow at high frequencies. The passage of the primary vortex produced a significant decrease in the height of maximum radial wind speed, predominantly in the ABL-streamwise direction. The turbulence intensity was the highest in the region where DB propagates into oppositely directed ABL winds.https://www.mdpi.com/2073-4433/13/4/621downburst windimpinging jetABL windsbackground windflow interactionWindEEE Dome
spellingShingle Federico Canepa
Massimiliano Burlando
Horia Hangan
Djordje Romanic
Experimental Investigation of the Near-Surface Flow Dynamics in Downburst-like Impinging Jets Immersed in ABL-like Winds
Atmosphere
downburst wind
impinging jet
ABL winds
background wind
flow interaction
WindEEE Dome
title Experimental Investigation of the Near-Surface Flow Dynamics in Downburst-like Impinging Jets Immersed in ABL-like Winds
title_full Experimental Investigation of the Near-Surface Flow Dynamics in Downburst-like Impinging Jets Immersed in ABL-like Winds
title_fullStr Experimental Investigation of the Near-Surface Flow Dynamics in Downburst-like Impinging Jets Immersed in ABL-like Winds
title_full_unstemmed Experimental Investigation of the Near-Surface Flow Dynamics in Downburst-like Impinging Jets Immersed in ABL-like Winds
title_short Experimental Investigation of the Near-Surface Flow Dynamics in Downburst-like Impinging Jets Immersed in ABL-like Winds
title_sort experimental investigation of the near surface flow dynamics in downburst like impinging jets immersed in abl like winds
topic downburst wind
impinging jet
ABL winds
background wind
flow interaction
WindEEE Dome
url https://www.mdpi.com/2073-4433/13/4/621
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AT massimilianoburlando experimentalinvestigationofthenearsurfaceflowdynamicsindownburstlikeimpingingjetsimmersedinabllikewinds
AT horiahangan experimentalinvestigationofthenearsurfaceflowdynamicsindownburstlikeimpingingjetsimmersedinabllikewinds
AT djordjeromanic experimentalinvestigationofthenearsurfaceflowdynamicsindownburstlikeimpingingjetsimmersedinabllikewinds