Diurnal internal tides detected in the Adriatic

Strong diurnal oscillations, documented by temperature data that were collected along a submarine cliff on the Lastovo Island (southern Adriatic), are studied and compared with sea level and wind measurements at Dubrovnik and Komiža (island of Vis). Three thermistors were deployed at t...

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Main Authors: H. Mihanović, M. Orlić, Z. Pasarić
Format: Article
Language:English
Published: Copernicus Publications 2006-11-01
Series:Annales Geophysicae
Online Access:https://www.ann-geophys.net/24/2773/2006/angeo-24-2773-2006.pdf
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spelling doaj-7f8f46e956884911be6cbff0b6741b682020-11-24T22:58:21ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05762006-11-01242773278010.5194/angeo-24-2773-2006Diurnal internal tides detected in the AdriaticH. Mihanović0M. Orlić1Z. Pasarić2Hydrographic Institute of the Republic of Croatia, Zrinsko-Frankopanska 161, 21000 Split, CroatiaAndrija Mohorovičić Geophysical Institute, Faculty of Science, University of Zagreb, Horvatovac bb, 10000 Zagreb, CroatiaAndrija Mohorovičić Geophysical Institute, Faculty of Science, University of Zagreb, Horvatovac bb, 10000 Zagreb, CroatiaStrong diurnal oscillations, documented by temperature data that were collected along a submarine cliff on the Lastovo Island (southern Adriatic), are studied and compared with sea level and wind measurements at Dubrovnik and Komiža (island of Vis). Three thermistors were deployed at the depths of 15, 22 and 36 m between March 2001 and March 2002. Pronounced diurnal temperature oscillations were detected at 15 and 22 m during the stratified season. The correlation between the sea surface and thermocline displacements was highest in June 2001, when diurnal wind changes were not significant, while diurnal sea level oscillations achieved annual maxima. Thermocline oscillations were in phase with sea level changes. The range of diurnal sea surface variability was close to 19 cm, while the range of corresponding thermocline variability was about 5.4 m. The findings summarize the outcome of the first dedicated study of internal tides in the Adriatic.https://www.ann-geophys.net/24/2773/2006/angeo-24-2773-2006.pdf
collection DOAJ
language English
format Article
sources DOAJ
author H. Mihanović
M. Orlić
Z. Pasarić
spellingShingle H. Mihanović
M. Orlić
Z. Pasarić
Diurnal internal tides detected in the Adriatic
Annales Geophysicae
author_facet H. Mihanović
M. Orlić
Z. Pasarić
author_sort H. Mihanović
title Diurnal internal tides detected in the Adriatic
title_short Diurnal internal tides detected in the Adriatic
title_full Diurnal internal tides detected in the Adriatic
title_fullStr Diurnal internal tides detected in the Adriatic
title_full_unstemmed Diurnal internal tides detected in the Adriatic
title_sort diurnal internal tides detected in the adriatic
publisher Copernicus Publications
series Annales Geophysicae
issn 0992-7689
1432-0576
publishDate 2006-11-01
description Strong diurnal oscillations, documented by temperature data that were collected along a submarine cliff on the Lastovo Island (southern Adriatic), are studied and compared with sea level and wind measurements at Dubrovnik and Komiža (island of Vis). Three thermistors were deployed at the depths of 15, 22 and 36 m between March 2001 and March 2002. Pronounced diurnal temperature oscillations were detected at 15 and 22 m during the stratified season. The correlation between the sea surface and thermocline displacements was highest in June 2001, when diurnal wind changes were not significant, while diurnal sea level oscillations achieved annual maxima. Thermocline oscillations were in phase with sea level changes. The range of diurnal sea surface variability was close to 19 cm, while the range of corresponding thermocline variability was about 5.4 m. The findings summarize the outcome of the first dedicated study of internal tides in the Adriatic.
url https://www.ann-geophys.net/24/2773/2006/angeo-24-2773-2006.pdf
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AT morlic diurnalinternaltidesdetectedintheadriatic
AT zpasaric diurnalinternaltidesdetectedintheadriatic
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