Foehn flow and stable air mass in the Rhine valley: The beginning of a MAP event
The foehn event of the 8th Intensive Observation Period (20-21 October 1999) of the Mesoscale Alpine Programme is examined at small scale with the help of both instrumental data (especially from a ground-based Doppler lidar) and of high-resolution simulation performed with the non-hydrostatic model...
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Published in | Quarterly journal of the Royal Meteorological Society Vol. 130; no. 597B; pp. 541 - 560 |
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Main Authors | , , |
Format | Journal Article |
Language | English |
Published |
01.01.2004
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Subjects | |
Online Access | Get full text |
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Summary: | The foehn event of the 8th Intensive Observation Period (20-21 October 1999) of the Mesoscale Alpine Programme is examined at small scale with the help of both instrumental data (especially from a ground-based Doppler lidar) and of high-resolution simulation performed with the non-hydrostatic model meso-NH. The three-dimensional characteristics of the flow in the Rhine valley at the beginning of the event are studied. Special attention is given to the interaction between the foehn and a stable air mass, whose presence drives the penetration of the warm and turbulent foehn air to the ground. A quantification of the simulated features of the flow is given in terms of mass budgets over the target area, and a three-dimensional picture representing the arrival of the foehn air. |
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Bibliography: | ObjectType-Article-1 SourceType-Scholarly Journals-1 content type line 23 ObjectType-Feature-2 |
ISSN: | 0035-9009 |
DOI: | 10.1256/qj.02.228 |