Remotely induced storm effects on the coastal flooding along the southwest coast of India

The southwest coast of India is exposed to long-period swells propagated from the South Indian Ocean during pre- and post-monsoon seasons. Although swells from the Southern Ocean and Atlantic Ocean were identified in the North Indian Ocean, their existence and impact along the southwest coast of Ind...

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Published in:Oceanologia
Main Authors: P.S. Swathy, Krishna, Valliyil Mohammed, Aboobacker, Madipally, Ramesh, L. Sheela, Nair
Format: Article in Journal/Newspaper
Language:English
Published: Elsevier
Subjects:
Online Access:http://hdl.handle.net/10576/54342
https://doi.org/10.1016/j.oceano.2023.03.003
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record_format openpolar
spelling ftqataruniv:oai:qspace.qu.edu.qa:10576/54342 2024-05-19T07:48:58+00:00 Remotely induced storm effects on the coastal flooding along the southwest coast of India P.S. Swathy, Krishna Valliyil Mohammed, Aboobacker Madipally, Ramesh L. Sheela, Nair application/pdf http://hdl.handle.net/10576/54342 https://doi.org/10.1016/j.oceano.2023.03.003 en eng Elsevier http://dx.doi.org/10.1016/j.oceano.2023.03.003 0078-3234 http://hdl.handle.net/10576/54342 503-516 3 65 2300-7370 IASO swells ERA5 winds Indian Ocean Kerala coast Coastal inundation Wave runup Article ftqataruniv https://doi.org/10.1016/j.oceano.2023.03.003 2024-04-30T23:40:38Z The southwest coast of India is exposed to long-period swells propagated from the South Indian Ocean during pre- and post-monsoon seasons. Although swells from the Southern Ocean and Atlantic Ocean were identified in the North Indian Ocean, their existence and impact along the southwest coast of India were not well investigated. On 19 March 2019, the Valiyathura-Shangumukham coastal stretch along the southwest coast of India experienced an unexpected coastal inundation without having a prompt forecast/warning, and not induced by a storm/cyclone in its vicinity. The present study investigates the causative forces of this inundation and estimates the wave runup and inundation. The study reveals that an unusual swell system was developed in the Indian-Atlantic-Southern Oceans (IASO) interface during 10–12 March and propagated towards the southwest coast of India. The measured wave spectra off Varkala clearly depicts the presence of long-period swells (Tp>18 s), which dominantly occurred as single-peaked. Wave modelling has been carried out to characterize the wave transformation associated with the “IASO interface swells” along the southern Kerala coast. A wave runup of up to 0.93 m height and a coastal inundation of up to 83 m onshore have been estimated during this event. UNESCO Chair in Marine Sciences at Qatar University, funded through the project, QUEX-ESC-QP-TM-18/19-01. Article in Journal/Newspaper Southern Ocean Qatar University: QU Institutional Repository Oceanologia 65 3 503 516
institution Open Polar
collection Qatar University: QU Institutional Repository
op_collection_id ftqataruniv
language English
topic IASO swells
ERA5 winds
Indian Ocean
Kerala coast
Coastal inundation
Wave runup
spellingShingle IASO swells
ERA5 winds
Indian Ocean
Kerala coast
Coastal inundation
Wave runup
P.S. Swathy, Krishna
Valliyil Mohammed, Aboobacker
Madipally, Ramesh
L. Sheela, Nair
Remotely induced storm effects on the coastal flooding along the southwest coast of India
topic_facet IASO swells
ERA5 winds
Indian Ocean
Kerala coast
Coastal inundation
Wave runup
description The southwest coast of India is exposed to long-period swells propagated from the South Indian Ocean during pre- and post-monsoon seasons. Although swells from the Southern Ocean and Atlantic Ocean were identified in the North Indian Ocean, their existence and impact along the southwest coast of India were not well investigated. On 19 March 2019, the Valiyathura-Shangumukham coastal stretch along the southwest coast of India experienced an unexpected coastal inundation without having a prompt forecast/warning, and not induced by a storm/cyclone in its vicinity. The present study investigates the causative forces of this inundation and estimates the wave runup and inundation. The study reveals that an unusual swell system was developed in the Indian-Atlantic-Southern Oceans (IASO) interface during 10–12 March and propagated towards the southwest coast of India. The measured wave spectra off Varkala clearly depicts the presence of long-period swells (Tp>18 s), which dominantly occurred as single-peaked. Wave modelling has been carried out to characterize the wave transformation associated with the “IASO interface swells” along the southern Kerala coast. A wave runup of up to 0.93 m height and a coastal inundation of up to 83 m onshore have been estimated during this event. UNESCO Chair in Marine Sciences at Qatar University, funded through the project, QUEX-ESC-QP-TM-18/19-01.
format Article in Journal/Newspaper
author P.S. Swathy, Krishna
Valliyil Mohammed, Aboobacker
Madipally, Ramesh
L. Sheela, Nair
author_facet P.S. Swathy, Krishna
Valliyil Mohammed, Aboobacker
Madipally, Ramesh
L. Sheela, Nair
author_sort P.S. Swathy, Krishna
title Remotely induced storm effects on the coastal flooding along the southwest coast of India
title_short Remotely induced storm effects on the coastal flooding along the southwest coast of India
title_full Remotely induced storm effects on the coastal flooding along the southwest coast of India
title_fullStr Remotely induced storm effects on the coastal flooding along the southwest coast of India
title_full_unstemmed Remotely induced storm effects on the coastal flooding along the southwest coast of India
title_sort remotely induced storm effects on the coastal flooding along the southwest coast of india
publisher Elsevier
url http://hdl.handle.net/10576/54342
https://doi.org/10.1016/j.oceano.2023.03.003
genre Southern Ocean
genre_facet Southern Ocean
op_relation http://dx.doi.org/10.1016/j.oceano.2023.03.003
0078-3234
http://hdl.handle.net/10576/54342
503-516
3
65
2300-7370
op_doi https://doi.org/10.1016/j.oceano.2023.03.003
container_title Oceanologia
container_volume 65
container_issue 3
container_start_page 503
op_container_end_page 516
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