Behavior of surges in Alexandria Eastern Harbor, Egypt

Alexandria Eastern Harbor (AEH) is constantly enduring the destructive problem of storm surges. Therefore, the investigation of the behavior of surges in the Harbor is crucial, and determining to which extent this is affected by the meteorological conditions is essential. We used hourly data of sea-...

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Main Authors: Tarek M. El-Geziry, Amna S. Dabbous
Format: Article
Language:English
Published: Elsevier 2021-06-01
Series:Egyptian Journal of Aquatic Research
Subjects:
Online Access:http://www.sciencedirect.com/science/article/pii/S1687428521000042
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spelling doaj-8668e6ff4a84426da3497fa73cf01d2f2021-06-25T04:47:10ZengElsevierEgyptian Journal of Aquatic Research1687-42852021-06-01472171178Behavior of surges in Alexandria Eastern Harbor, EgyptTarek M. El-Geziry0Amna S. Dabbous1Corresponding author.; Laboratory of Physical Oceanography, Division of Marine Environment, National Institute of Oceanography and Fisheries (NIOF), EgyptLaboratory of Physical Oceanography, Division of Marine Environment, National Institute of Oceanography and Fisheries (NIOF), EgyptAlexandria Eastern Harbor (AEH) is constantly enduring the destructive problem of storm surges. Therefore, the investigation of the behavior of surges in the Harbor is crucial, and determining to which extent this is affected by the meteorological conditions is essential. We used hourly data of sea-level, from 10.06.2018 to 15.06.2020, to calculate AEH surge heights. Simultaneous records of winds and sea-level pressure (SLP) were used to examine their impact on the calculated surges. Also, an empirical equation was derived to estimate the surge height in AEH by knowing the SLP and winds.Results revealed a 99% contribution of surges to the recorded sea-level. Surge heights exhibited a seasonal pattern with lower values in spring and higher ones in summer. While the positive surges dominated the Harbor all the year-round, the negative surges appeared only in 8 months: January-June, in addition to October and November.The total and the positive surges were directly proportional to all wind components but the negative parallel ones. Contrariwise, the negative surge associated the decrease of all wind components except the negative parallel and the negative normal components. There was an inverse relationship between the total, positive and negative surge heights and the SLP.http://www.sciencedirect.com/science/article/pii/S1687428521000042AlexandriaEastern HarborSurgesMeteorologySeasonalityRegression
collection DOAJ
language English
format Article
sources DOAJ
author Tarek M. El-Geziry
Amna S. Dabbous
spellingShingle Tarek M. El-Geziry
Amna S. Dabbous
Behavior of surges in Alexandria Eastern Harbor, Egypt
Egyptian Journal of Aquatic Research
Alexandria
Eastern Harbor
Surges
Meteorology
Seasonality
Regression
author_facet Tarek M. El-Geziry
Amna S. Dabbous
author_sort Tarek M. El-Geziry
title Behavior of surges in Alexandria Eastern Harbor, Egypt
title_short Behavior of surges in Alexandria Eastern Harbor, Egypt
title_full Behavior of surges in Alexandria Eastern Harbor, Egypt
title_fullStr Behavior of surges in Alexandria Eastern Harbor, Egypt
title_full_unstemmed Behavior of surges in Alexandria Eastern Harbor, Egypt
title_sort behavior of surges in alexandria eastern harbor, egypt
publisher Elsevier
series Egyptian Journal of Aquatic Research
issn 1687-4285
publishDate 2021-06-01
description Alexandria Eastern Harbor (AEH) is constantly enduring the destructive problem of storm surges. Therefore, the investigation of the behavior of surges in the Harbor is crucial, and determining to which extent this is affected by the meteorological conditions is essential. We used hourly data of sea-level, from 10.06.2018 to 15.06.2020, to calculate AEH surge heights. Simultaneous records of winds and sea-level pressure (SLP) were used to examine their impact on the calculated surges. Also, an empirical equation was derived to estimate the surge height in AEH by knowing the SLP and winds.Results revealed a 99% contribution of surges to the recorded sea-level. Surge heights exhibited a seasonal pattern with lower values in spring and higher ones in summer. While the positive surges dominated the Harbor all the year-round, the negative surges appeared only in 8 months: January-June, in addition to October and November.The total and the positive surges were directly proportional to all wind components but the negative parallel ones. Contrariwise, the negative surge associated the decrease of all wind components except the negative parallel and the negative normal components. There was an inverse relationship between the total, positive and negative surge heights and the SLP.
topic Alexandria
Eastern Harbor
Surges
Meteorology
Seasonality
Regression
url http://www.sciencedirect.com/science/article/pii/S1687428521000042
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