Large-eddy simulation of foehn-cold pool interactions in the Inn Valley during PIANO IOP 2.

cold‐air pool complex terrain foehn heat budget large‐eddy simulation shear flow instability turbulent erosion

Journal

Quarterly journal of the Royal Meteorological Society. Royal Meteorological Society (Great Britain)
ISSN: 0035-9009
Titre abrégé: Q J R Meteorol Soc
Pays: England
ID NLM: 101661952

Informations de publication

Date de publication:
Jan 2021
Historique:
received: 20 06 2020
revised: 27 10 2020
accepted: 18 11 2020
entrez: 29 3 2021
pubmed: 30 3 2021
medline: 30 3 2021
Statut: ppublish

Résumé

Processes of cold-air pool (CAP) erosion in an Alpine valley during south foehn are investigated based on a real-case large-eddy simulation (LES). The event occurred during the second Intensive Observation Period (IOP 2) of the PIANO field experiment in the Inn Valley, Austria, near the city of Innsbruck. The goal is to clarify the role of advective versus turbulent heating, the latter often being misrepresented in mesoscale models. It was found that the LES of the first day of IOP 2 outperforms a mesoscale simulation, is not yet perfect, but is able to reproduce the CAP evolution and structure observed on the second day of IOP 2. The CAP exhibits strong heterogeneity in the along-valley direction. It is weaker in the east than in the west of the city with a local depression above the city. This heterogeneity results from different relative contributions and magnitudes of turbulent and advective heating/cooling, which mostly act against each other. Turbulent heating is important for faster CAP erosion in the east and advective cooling is important for CAP maintenance to the west of Innsbruck. The spatial heterogeneity in turbulent erosion is linked to splitting of the foehn into two branches at the mountain range north of the city, with a stronger eastward deflected branch. Intensification of the western branch at a later stage leads to complete CAP erosion also to the west of Innsbruck. Above the city centre, turbulent heating is strongest, and so is advective cooling by enhanced pre-foehn westerlies. These local winds are the result of CAP heterogeneity and gravity-wave asymmetry. This study emphasizes the importance of shear-flow instability for CAP erosion. It also highlights the large magnitudes of advective and turbulent heating compared to their net effect, which is even more pronounced for individual spatial components.

Identifiants

pubmed: 33776152
doi: 10.1002/qj.3954
pii: QJ3954
pmc: PMC7986625
doi:

Types de publication

Journal Article

Langues

eng

Pagination

944-982

Informations de copyright

© 2020 The Authors. Quarterly Journal of the Royal Meteorological Society published by John Wiley & Sons Ltd on behalf of the Royal Meteorological Society.

Références

Q J R Meteorol Soc. 2020 Apr;146(728):1232-1263
pubmed: 32612310

Auteurs

L Umek (L)

Department of Atmospheric and Cryospheric Sciences University of Innsbruck Innsbruck Austria.

A Gohm (A)

Department of Atmospheric and Cryospheric Sciences University of Innsbruck Innsbruck Austria.

M Haid (M)

Department of Atmospheric and Cryospheric Sciences University of Innsbruck Innsbruck Austria.

H C Ward (HC)

Department of Atmospheric and Cryospheric Sciences University of Innsbruck Innsbruck Austria.

M W Rotach (MW)

Department of Atmospheric and Cryospheric Sciences University of Innsbruck Innsbruck Austria.

Classifications MeSH