Scaling for lobe and cleft patterns in particle-laden gravity currents
Lobe and cleft patterns are frequently observed at the leading edge of gravity currents, including non-Boussinesq particle-laden currents such as powder snow avalanches. Despite the importance of the instability in driving air entrainment, little is known about its origin or the mechanisms behind it...
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| Format: | Thesis (University of Nottingham only) |
| Language: | English |
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2014
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| Online Access: | https://eprints.nottingham.ac.uk/14237/ |
| _version_ | 1848791910440763392 |
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| author | Jackson, Andrew |
| author_facet | Jackson, Andrew |
| author_sort | Jackson, Andrew |
| building | Nottingham Research Data Repository |
| collection | Online Access |
| description | Lobe and cleft patterns are frequently observed at the leading edge of gravity currents, including non-Boussinesq particle-laden currents such as powder snow avalanches. Despite the importance of the instability in driving air entrainment, little is known about its origin or the mechanisms behind its development. In this work we seek to gain a better understanding of these mechanisms from a laboratory scale model of powder snow avalanches using lightweight granular material.
The instability mechanisms in these flows appear to be a combination of those found in both homogeneous Boussinesq gravity currents and unsuspended granular flows, with the size of the granular particles playing a central role in determining the wavelength of the lobe and cleft pattern. When scaled by particle diameter a relationship between Froude number and the wavelength of the lobe and cleft pattern is found, where the wavelength increases monotonically with Froude number. This relationship, in addition to Particle Image Velocimetry analysis, provides evidence for the existence of pairs of counter-rotating vortices at the leading edge of these currents, which play a key role in the development of the lobe and cleft pattern.
The internal pressure of these flows is found to scale with the dynamics of the large vortex-like structure that is observed within the head of the current. |
| first_indexed | 2025-11-14T18:36:01Z |
| format | Thesis (University of Nottingham only) |
| id | nottingham-14237 |
| institution | University of Nottingham Malaysia Campus |
| institution_category | Local University |
| language | English |
| last_indexed | 2025-11-14T18:36:01Z |
| publishDate | 2014 |
| recordtype | eprints |
| repository_type | Digital Repository |
| spelling | nottingham-142372025-02-28T11:29:33Z https://eprints.nottingham.ac.uk/14237/ Scaling for lobe and cleft patterns in particle-laden gravity currents Jackson, Andrew Lobe and cleft patterns are frequently observed at the leading edge of gravity currents, including non-Boussinesq particle-laden currents such as powder snow avalanches. Despite the importance of the instability in driving air entrainment, little is known about its origin or the mechanisms behind its development. In this work we seek to gain a better understanding of these mechanisms from a laboratory scale model of powder snow avalanches using lightweight granular material. The instability mechanisms in these flows appear to be a combination of those found in both homogeneous Boussinesq gravity currents and unsuspended granular flows, with the size of the granular particles playing a central role in determining the wavelength of the lobe and cleft pattern. When scaled by particle diameter a relationship between Froude number and the wavelength of the lobe and cleft pattern is found, where the wavelength increases monotonically with Froude number. This relationship, in addition to Particle Image Velocimetry analysis, provides evidence for the existence of pairs of counter-rotating vortices at the leading edge of these currents, which play a key role in the development of the lobe and cleft pattern. The internal pressure of these flows is found to scale with the dynamics of the large vortex-like structure that is observed within the head of the current. 2014-07-09 Thesis (University of Nottingham only) NonPeerReviewed application/pdf en arr https://eprints.nottingham.ac.uk/14237/1/thesisdone.pdf Jackson, Andrew (2014) Scaling for lobe and cleft patterns in particle-laden gravity currents. PhD thesis, University of Nottingham. Avalanches granular materials pattern formation (Physical sciences) |
| spellingShingle | Avalanches granular materials pattern formation (Physical sciences) Jackson, Andrew Scaling for lobe and cleft patterns in particle-laden gravity currents |
| title | Scaling for lobe and cleft patterns in particle-laden gravity currents |
| title_full | Scaling for lobe and cleft patterns in particle-laden gravity currents |
| title_fullStr | Scaling for lobe and cleft patterns in particle-laden gravity currents |
| title_full_unstemmed | Scaling for lobe and cleft patterns in particle-laden gravity currents |
| title_short | Scaling for lobe and cleft patterns in particle-laden gravity currents |
| title_sort | scaling for lobe and cleft patterns in particle-laden gravity currents |
| topic | Avalanches granular materials pattern formation (Physical sciences) |
| url | https://eprints.nottingham.ac.uk/14237/ |