Mesoscale Bora flow and mountain pressure drag
The paper analyses the Bora periods on the basis of 10-minute microbarographic measurements (ALPEX 50P, March-April 1982) and the corresponding surface pressure drag values. In the cases with pressure drag with larger negative values than -1.3⋅10-3 Nm-3 the Bora was very strong over the entire North...
Main Authors: | , |
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Format: | Article |
Language: | English |
Published: |
Borntraeger
1995-07-01
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Series: | Meteorologische Zeitschrift |
Subjects: | |
Online Access: | http://dx.doi.org/10.1127/metz/4/1995/119 |
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author | Branka Ivančan-Picek V. Tutiš |
author_facet | Branka Ivančan-Picek V. Tutiš |
author_sort | Branka Ivančan-Picek |
collection | DOAJ |
description | The paper analyses the Bora periods on the basis of 10-minute microbarographic measurements (ALPEX 50P, March-April 1982) and the corresponding surface pressure drag values. In the cases with pressure drag with larger negative values than -1.3⋅10-3 Nm-3 the Bora was very strong over the entire Northern Adriatic coast. It is shown that pressure drag is highly correlated with the cross-mountain pressure differences which confirms the results from PYREX where such a simple relationship was found for the Pyrenees. The results suggest the possibility of application of the linear regression method in drag estimation for periods for which microbarographic data are not available. Mesoscale analysis of ALPEX Bora cases emphasize the large isentropic slope. The strongest gradient in the geopotential height field over the Dinaric Alps coincided with the strongest Bora. |
first_indexed | 2024-03-08T04:48:58Z |
format | Article |
id | doaj.art-c2f29168e583453280af7a95123ffed2 |
institution | Directory Open Access Journal |
issn | 0941-2948 |
language | English |
last_indexed | 2024-03-08T04:48:58Z |
publishDate | 1995-07-01 |
publisher | Borntraeger |
record_format | Article |
series | Meteorologische Zeitschrift |
spelling | doaj.art-c2f29168e583453280af7a95123ffed22024-02-08T08:12:19ZengBorntraegerMeteorologische Zeitschrift0941-29481995-07-014311912810.1127/metz/4/1995/11989184Mesoscale Bora flow and mountain pressure dragBranka Ivančan-PicekV. TutišThe paper analyses the Bora periods on the basis of 10-minute microbarographic measurements (ALPEX 50P, March-April 1982) and the corresponding surface pressure drag values. In the cases with pressure drag with larger negative values than -1.3⋅10-3 Nm-3 the Bora was very strong over the entire Northern Adriatic coast. It is shown that pressure drag is highly correlated with the cross-mountain pressure differences which confirms the results from PYREX where such a simple relationship was found for the Pyrenees. The results suggest the possibility of application of the linear regression method in drag estimation for periods for which microbarographic data are not available. Mesoscale analysis of ALPEX Bora cases emphasize the large isentropic slope. The strongest gradient in the geopotential height field over the Dinaric Alps coincided with the strongest Bora.http://dx.doi.org/10.1127/metz/4/1995/119microbarographic measurementspressure dragnorthern adriatic coastpyreneesmesoscale analysisdinaric alpsmikrobarographen-messungendruckwiderständeadria-küstepyrenäenisentropendinarische alpen |
spellingShingle | Branka Ivančan-Picek V. Tutiš Mesoscale Bora flow and mountain pressure drag Meteorologische Zeitschrift microbarographic measurements pressure drag northern adriatic coast pyrenees mesoscale analysis dinaric alps mikrobarographen-messungen druckwiderstände adria-küste pyrenäen isentropen dinarische alpen |
title | Mesoscale Bora flow and mountain pressure drag |
title_full | Mesoscale Bora flow and mountain pressure drag |
title_fullStr | Mesoscale Bora flow and mountain pressure drag |
title_full_unstemmed | Mesoscale Bora flow and mountain pressure drag |
title_short | Mesoscale Bora flow and mountain pressure drag |
title_sort | mesoscale bora flow and mountain pressure drag |
topic | microbarographic measurements pressure drag northern adriatic coast pyrenees mesoscale analysis dinaric alps mikrobarographen-messungen druckwiderstände adria-küste pyrenäen isentropen dinarische alpen |
url | http://dx.doi.org/10.1127/metz/4/1995/119 |
work_keys_str_mv | AT brankaivancanpicek mesoscaleboraflowandmountainpressuredrag AT vtutis mesoscaleboraflowandmountainpressuredrag |