Rotation of sea/land breezes along the northeastern Adriatic coast

The diurnal evolution of the sea/land breeze hodographs over the northeastern Adriatic coast has been examined for several episodes, each lasting a few days. A limited set of observations, as well as the results of a three-dimensional nonhydrostatic mesoscale model are studied by applying a rota...

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Main Authors: M. T. Prtenjak, Z. Pasarić, M. Orlić, B. Grisogono
Format: Article
Language:English
Published: Copernicus Publications 2008-06-01
Series:Annales Geophysicae
Online Access:https://www.ann-geophys.net/26/1711/2008/angeo-26-1711-2008.pdf
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spelling doaj-3b0810775afa45a991c18931b00036032020-11-25T01:10:21ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05762008-06-01261711172410.5194/angeo-26-1711-2008Rotation of sea/land breezes along the northeastern Adriatic coastM. T. Prtenjak0Z. Pasarić1M. Orlić2B. Grisogono3Department of Geophysics, Faculty of Science, University of Zagreb, CroatiaDepartment of Geophysics, Faculty of Science, University of Zagreb, CroatiaDepartment of Geophysics, Faculty of Science, University of Zagreb, CroatiaDepartment of Geophysics, Faculty of Science, University of Zagreb, CroatiaThe diurnal evolution of the sea/land breeze hodographs over the northeastern Adriatic coast has been examined for several episodes, each lasting a few days. A limited set of observations, as well as the results of a three-dimensional nonhydrostatic mesoscale model are studied by applying a rotary-component method. This revealed a spatial distribution of the clockwise versus anti-clockwise rotation of the wind vectors for the sea/land breeze events. An application of the rotary-component method to the results of additional numerical sensitivity tests showed that the coastal topography height considerably influences both the shape of the wind hodographs and the sense of wind rotation. The method also displayed which areas are under a strong influence of the 24-h topographic forcing and which areas show a large wind consistency. A further analysis of the 24-h modeled wind hodographs at several selected stations has been performed, thus revealing the hodograph shapes and the reasons for them.https://www.ann-geophys.net/26/1711/2008/angeo-26-1711-2008.pdf
collection DOAJ
language English
format Article
sources DOAJ
author M. T. Prtenjak
Z. Pasarić
M. Orlić
B. Grisogono
spellingShingle M. T. Prtenjak
Z. Pasarić
M. Orlić
B. Grisogono
Rotation of sea/land breezes along the northeastern Adriatic coast
Annales Geophysicae
author_facet M. T. Prtenjak
Z. Pasarić
M. Orlić
B. Grisogono
author_sort M. T. Prtenjak
title Rotation of sea/land breezes along the northeastern Adriatic coast
title_short Rotation of sea/land breezes along the northeastern Adriatic coast
title_full Rotation of sea/land breezes along the northeastern Adriatic coast
title_fullStr Rotation of sea/land breezes along the northeastern Adriatic coast
title_full_unstemmed Rotation of sea/land breezes along the northeastern Adriatic coast
title_sort rotation of sea/land breezes along the northeastern adriatic coast
publisher Copernicus Publications
series Annales Geophysicae
issn 0992-7689
1432-0576
publishDate 2008-06-01
description The diurnal evolution of the sea/land breeze hodographs over the northeastern Adriatic coast has been examined for several episodes, each lasting a few days. A limited set of observations, as well as the results of a three-dimensional nonhydrostatic mesoscale model are studied by applying a rotary-component method. This revealed a spatial distribution of the clockwise versus anti-clockwise rotation of the wind vectors for the sea/land breeze events. An application of the rotary-component method to the results of additional numerical sensitivity tests showed that the coastal topography height considerably influences both the shape of the wind hodographs and the sense of wind rotation. The method also displayed which areas are under a strong influence of the 24-h topographic forcing and which areas show a large wind consistency. A further analysis of the 24-h modeled wind hodographs at several selected stations has been performed, thus revealing the hodograph shapes and the reasons for them.
url https://www.ann-geophys.net/26/1711/2008/angeo-26-1711-2008.pdf
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