Please use this identifier to cite or link to this item:
https://olympias.lib.uoi.gr/jspui/handle/123456789/17499Full metadata record
| DC Field | Value | Language |
|---|---|---|
| dc.contributor.author | Koletsis, I. | en |
| dc.contributor.author | Lagouvardos, K. | en |
| dc.contributor.author | Kotroni, V. | en |
| dc.contributor.author | Bartzokas, A. | en |
| dc.date.accessioned | 2015-11-24T18:39:49Z | - |
| dc.date.available | 2015-11-24T18:39:49Z | - |
| dc.identifier.issn | 0169-8095 | - |
| dc.identifier.uri | https://olympias.lib.uoi.gr/jspui/handle/123456789/17499 | - |
| dc.rights | Default Licence | - |
| dc.subject | windstorm | en |
| dc.subject | mountain wave breaking | en |
| dc.subject | downslope winds | en |
| dc.subject | amplitude mountain waves | en |
| dc.subject | cascade mountains | en |
| dc.subject | bora | en |
| dc.subject | model | en |
| dc.subject | flow | en |
| dc.subject | simulation | en |
| dc.subject | stability | en |
| dc.subject | evolution | en |
| dc.subject | forecasts | en |
| dc.subject | state | en |
| dc.title | Numerical study of a downslope windstorm in Northwestern Greece | en |
| heal.type | journalArticle | - |
| heal.type.en | Journal article | en |
| heal.type.el | Άρθρο Περιοδικού | el |
| heal.identifier.primary | DOI 10.1016/j.atmosres.2009.05.012 | - |
| heal.identifier.secondary | <Go to ISI>://000270119400004 | - |
| heal.identifier.secondary | http://ac.els-cdn.com/S0169809509001598/1-s2.0-S0169809509001598-main.pdf?_tid=2b27d81b3991d90a640d32494a50cda8&acdnat=1334218496_efc78cfc8028d1d878818c98af64f833 | - |
| heal.language | en | - |
| heal.access | campus | - |
| heal.recordProvider | Πανεπιστήμιο Ιωαννίνων. Σχολή Επιστημών και Τεχνολογιών. Τμήμα Βιολογικών Εφαρμογών και Τεχνολογιών | el |
| heal.publicationDate | 2009 | - |
| heal.abstract | This paper describes the leeside wind storm of 25-26 March 1998, the most intense wind storm of the last decade in Northwestern Greece. This wind storm produced wind gusts of similar to 30 m s(-1) that resulted in tree uprooting, roof damaging, electric power network disruption and flooding in the lake-side areas of Ioannina city in Northwestern Greece. With the aim to identify the role of Mountain Mitsikeli near the city of Ioannina on the windstorm and to investigate the physical mechanisms responsible for such orographically induced weather events, numerical simulations with MM5 model have been performed. The model results showed that a resolution of 2-km resolution is necessary in order to reproduce the localized character of the wind storm. The analysis revealed that a synergistic combination of the cross-barrier northeasterly flow, the stable layer above the mountain top and the presence of a critical level, led to the intensification of the lee side winds during the studied wind event. Sensitivity experiments with modified topography, further supported the important role of mountain Mitsikeli that stands as an isolated obstacle, on the modification of the wind field during the observed windstorm. (C) 2009 Elsevier B.V. All rights reserved. | en |
| heal.journalName | Atmospheric Research | en |
| heal.journalType | peer reviewed | - |
| heal.fullTextAvailability | TRUE | - |
| Appears in Collections: | Άρθρα σε επιστημονικά περιοδικά ( Ανοικτά) | |
Files in This Item:
| File | Description | Size | Format | |
|---|---|---|---|---|
| Koletsis-2009-Numerical study of a.pdf | 2.52 MB | Adobe PDF | View/Open Request a copy |
This item is licensed under a Creative Commons License
