Inter-annual variations in wave spectral characteristics at a location off the central west coast of India

The inter-annual variations in wave spectrum are examined based on the wave data measured at 9 m water depth off the central west coast of India from 2009 to 2012 using a wave rider buoy. The temporal variation of the spectral energy density over a calendar year indicates similar variation in all...

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Main Authors: V. Sanil Kumar, M. Anjali Nair
Format: Article
Language:English
Published: Copernicus Publications 2015-02-01
Series:Annales Geophysicae
Online Access:https://www.ann-geophys.net/33/159/2015/angeo-33-159-2015.pdf
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spelling doaj-1fff8991ef3a409f93509f96fa70a87a2020-11-25T00:11:58ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05762015-02-013315916710.5194/angeo-33-159-2015Inter-annual variations in wave spectral characteristics at a location off the central west coast of IndiaV. Sanil Kumar0M. Anjali Nair1Ocean Engineering, CSIR-National Institute of Oceanography (Council of Scientific & Industrial Research) Dona Paula, Goa 403 004, IndiaOcean Engineering, CSIR-National Institute of Oceanography (Council of Scientific & Industrial Research) Dona Paula, Goa 403 004, IndiaThe inter-annual variations in wave spectrum are examined based on the wave data measured at 9 m water depth off the central west coast of India from 2009 to 2012 using a wave rider buoy. The temporal variation of the spectral energy density over a calendar year indicates similar variation in all the four years studied. The inter-annual variations in wave spectrum are observed in all months with larger variations during January to February, May and October to November due to the changes in wind-sea. The seasonal average wave spectrum during the monsoon (June–September) is single-peaked and the swell component is high in 2011 compared to other years. The annual averaged wave spectrum had higher peak energy during 2011 due to the higher spectral energy present during the monsoon period. During the non-monsoon period, two peaks are predominantly observed in the wave spectra; with the average peak at 0.07 Hz corresponding to the swells from the Indian Ocean and another at 0.17 Hz due to the local wind field.https://www.ann-geophys.net/33/159/2015/angeo-33-159-2015.pdf
collection DOAJ
language English
format Article
sources DOAJ
author V. Sanil Kumar
M. Anjali Nair
spellingShingle V. Sanil Kumar
M. Anjali Nair
Inter-annual variations in wave spectral characteristics at a location off the central west coast of India
Annales Geophysicae
author_facet V. Sanil Kumar
M. Anjali Nair
author_sort V. Sanil Kumar
title Inter-annual variations in wave spectral characteristics at a location off the central west coast of India
title_short Inter-annual variations in wave spectral characteristics at a location off the central west coast of India
title_full Inter-annual variations in wave spectral characteristics at a location off the central west coast of India
title_fullStr Inter-annual variations in wave spectral characteristics at a location off the central west coast of India
title_full_unstemmed Inter-annual variations in wave spectral characteristics at a location off the central west coast of India
title_sort inter-annual variations in wave spectral characteristics at a location off the central west coast of india
publisher Copernicus Publications
series Annales Geophysicae
issn 0992-7689
1432-0576
publishDate 2015-02-01
description The inter-annual variations in wave spectrum are examined based on the wave data measured at 9 m water depth off the central west coast of India from 2009 to 2012 using a wave rider buoy. The temporal variation of the spectral energy density over a calendar year indicates similar variation in all the four years studied. The inter-annual variations in wave spectrum are observed in all months with larger variations during January to February, May and October to November due to the changes in wind-sea. The seasonal average wave spectrum during the monsoon (June–September) is single-peaked and the swell component is high in 2011 compared to other years. The annual averaged wave spectrum had higher peak energy during 2011 due to the higher spectral energy present during the monsoon period. During the non-monsoon period, two peaks are predominantly observed in the wave spectra; with the average peak at 0.07 Hz corresponding to the swells from the Indian Ocean and another at 0.17 Hz due to the local wind field.
url https://www.ann-geophys.net/33/159/2015/angeo-33-159-2015.pdf
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