Mesoscale modelling of a flow modification caused by orography
Cases of orographically increased wind speed of SE directions over Moravia and Czech territory (an area of 250 x 100 km) are dealt with. The acceleration of the SE flow is characterized by presenting several examples and the typical synoptic situations are shown at which the phenomenon occurs with h...
| Main Authors: | , |
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| Format: | Article |
| Language: | English |
| Published: |
Borntraeger
1994-09-01
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| Series: | Meteorologische Zeitschrift |
| Subjects: | |
| Online Access: | http://dx.doi.org/10.1127/metz/3/1994/233 |
| _version_ | 1797320856400035840 |
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| author | J. Svoboda J. Štekl |
| author_facet | J. Svoboda J. Štekl |
| author_sort | J. Svoboda |
| collection | DOAJ |
| description | Cases of orographically increased wind speed of SE directions over Moravia and Czech territory (an area of 250 x 100 km) are dealt with. The acceleration of the SE flow is characterized by presenting several examples and the typical synoptic situations are shown at which the phenomenon occurs with high probability. A non-hydrostatic model with two horizontal grid steps (9.3 and 2 km) is used for a diagnostic simulation of the wind field at a level of 10 m above complex terrain. The model is able to modify the horizontally homogeneous flow so that the resultant flow is in accordance with the observed structure. |
| first_indexed | 2024-03-08T04:49:04Z |
| format | Article |
| id | doaj.art-dad4c65a71984ffbb869ec4892aa5896 |
| institution | Directory Open Access Journal |
| issn | 0941-2948 |
| language | English |
| last_indexed | 2024-03-08T04:49:04Z |
| publishDate | 1994-09-01 |
| publisher | Borntraeger |
| record_format | Article |
| series | Meteorologische Zeitschrift |
| spelling | doaj.art-dad4c65a71984ffbb869ec4892aa58962024-02-08T08:11:30ZengBorntraegerMeteorologische Zeitschrift0941-29481994-09-013423324110.1127/metz/3/1994/23389543Mesoscale modelling of a flow modification caused by orographyJ. SvobodaJ. ŠteklCases of orographically increased wind speed of SE directions over Moravia and Czech territory (an area of 250 x 100 km) are dealt with. The acceleration of the SE flow is characterized by presenting several examples and the typical synoptic situations are shown at which the phenomenon occurs with high probability. A non-hydrostatic model with two horizontal grid steps (9.3 and 2 km) is used for a diagnostic simulation of the wind field at a level of 10 m above complex terrain. The model is able to modify the horizontally homogeneous flow so that the resultant flow is in accordance with the observed structure.http://dx.doi.org/10.1127/metz/3/1994/233orographicallyse flownon-hydrostatichorizontal grid stepsorographischsüdostwindnicht hydrostatischhorizontale maschenweiten |
| spellingShingle | J. Svoboda J. Štekl Mesoscale modelling of a flow modification caused by orography Meteorologische Zeitschrift orographically se flow non-hydrostatic horizontal grid steps orographisch südostwind nicht hydrostatisch horizontale maschenweiten |
| title | Mesoscale modelling of a flow modification caused by orography |
| title_full | Mesoscale modelling of a flow modification caused by orography |
| title_fullStr | Mesoscale modelling of a flow modification caused by orography |
| title_full_unstemmed | Mesoscale modelling of a flow modification caused by orography |
| title_short | Mesoscale modelling of a flow modification caused by orography |
| title_sort | mesoscale modelling of a flow modification caused by orography |
| topic | orographically se flow non-hydrostatic horizontal grid steps orographisch südostwind nicht hydrostatisch horizontale maschenweiten |
| url | http://dx.doi.org/10.1127/metz/3/1994/233 |
| work_keys_str_mv | AT jsvoboda mesoscalemodellingofaflowmodificationcausedbyorography AT jstekl mesoscalemodellingofaflowmodificationcausedbyorography |