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...

Full description

Bibliographic Details
Main Authors: Branka Ivančan-Picek, V. Tutiš
Format: Article
Language:English
Published: Borntraeger 1995-07-01
Series:Meteorologische Zeitschrift
Subjects:
Online Access:http://dx.doi.org/10.1127/metz/4/1995/119
_version_ 1827355827041730560
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