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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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 |
work_keys_str_mv |
AT tarekmelgeziry behaviorofsurgesinalexandriaeasternharboregypt AT amnasdabbous behaviorofsurgesinalexandriaeasternharboregypt |
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1721360765766598656 |