Influence of winds on temporally varying short and long period gravity waves in the near shore regions of the eastern Arabian Sea

Wave data collected off Ratnagiri, west coast of India, during 1 May 2010 to 30 April 2012 are used in this study. Seasonal and annual variations in wave data controlled by the local wind system such as sea breeze and land breeze, and remote wind generated long period waves are also studied. The rol...
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Autor*in:	J. Glejin [verfasserIn] V. Sanil Kumar [verfasserIn] T. M. Balakrishnan Nair [verfasserIn] J. Singh [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2013

Übergeordnetes Werk:	In: Ocean Science - Copernicus Publications, 2004, 9(2013), 2, Seite 343-353
Übergeordnetes Werk:	volume:9 ; year:2013 ; number:2 ; pages:343-353

Links:	Link aufrufen Link aufrufen Link aufrufen Journal toc Journal toc

DOI / URN:	10.5194/os-9-343-2013

Katalog-ID:	DOAJ033057230

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allfieldsSound	10.5194/os-9-343-2013 doi (DE-627)DOAJ033057230 (DE-599)DOAJd8aad5a5657e46d89641bad74084986a DE-627 ger DE-627 rakwb eng GE1-350 J. Glejin verfasserin aut Influence of winds on temporally varying short and long period gravity waves in the near shore regions of the eastern Arabian Sea 2013 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Wave data collected off Ratnagiri, west coast of India, during 1 May 2010 to 30 April 2012 are used in this study. Seasonal and annual variations in wave data controlled by the local wind system such as sea breeze and land breeze, and remote wind generated long period waves are also studied. The role of sea breeze on the sea state during pre- and postmonsoon seasons is studied and it is found that the maximum wave height is observed at 15:00 UTC during the premonsoon season, with an estimated difference in time lag of 1–2 h in maximum wave height between premonsoon and postmonsoon seasons. Observed waves are classified in to (i) short waves (<i<T</i<<sub<p</sub< < 8 s), (ii) intermediate waves (8 < <i<T</i<<sub<p</sub< < 13 s), and (iii) long waves (<i<T</i<<sub<p</sub<< 13 s) based on peak period (<i<T</i<<sub<p</sub<) and the percentages of occurrence of each category are estimated. Long period waves are observed mainly during the pre- and the postmonsoon seasons. During the southwest monsoon period, the waves with period < 13 s are a minimum. An event during 2011 is identified as swells propagated from the Southern Ocean with an estimated travelling time of 5–6 days. The swells reaching the Arabian Sea from the south Indian Ocean and Southern Ocean, due to storms during the pre- and postmonsoon periods, modify the near surface winds due to higher phase wave celerity than the wind speed. Estimation of inverse wave age using large-scale winds such as NCEP (National Centers for Environmental Prediction) reflects the presence of cyclonic activity during pre- and postmonsoon seasons but not the effect of the local sea breeze/land breeze wind system. Geography. Anthropology. Recreation G Environmental sciences V. Sanil Kumar verfasserin aut T. M. Balakrishnan Nair verfasserin aut J. Singh verfasserin aut In Ocean Science Copernicus Publications, 2004 9(2013), 2, Seite 343-353 (DE-627)483612820 (DE-600)2183769-7 18120792 nnns volume:9 year:2013 number:2 pages:343-353 https://doi.org/10.5194/os-9-343-2013 kostenfrei https://doaj.org/article/d8aad5a5657e46d89641bad74084986a kostenfrei http://www.ocean-sci.net/9/343/2013/os-9-343-2013.pdf kostenfrei https://doaj.org/toc/1812-0784 Journal toc kostenfrei https://doaj.org/toc/1812-0792 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_213 GBV_ILN_230 GBV_ILN_267 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2003 GBV_ILN_2014 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 9 2013 2 343-353
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topic_title	GE1-350 Influence of winds on temporally varying short and long period gravity waves in the near shore regions of the eastern Arabian Sea
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title	Influence of winds on temporally varying short and long period gravity waves in the near shore regions of the eastern Arabian Sea
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title_full	Influence of winds on temporally varying short and long period gravity waves in the near shore regions of the eastern Arabian Sea
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title_sort	influence of winds on temporally varying short and long period gravity waves in the near shore regions of the eastern arabian sea
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title_auth	Influence of winds on temporally varying short and long period gravity waves in the near shore regions of the eastern Arabian Sea
abstract	Wave data collected off Ratnagiri, west coast of India, during 1 May 2010 to 30 April 2012 are used in this study. Seasonal and annual variations in wave data controlled by the local wind system such as sea breeze and land breeze, and remote wind generated long period waves are also studied. The role of sea breeze on the sea state during pre- and postmonsoon seasons is studied and it is found that the maximum wave height is observed at 15:00 UTC during the premonsoon season, with an estimated difference in time lag of 1–2 h in maximum wave height between premonsoon and postmonsoon seasons. Observed waves are classified in to (i) short waves (<i<T</i<<sub<p</sub< < 8 s), (ii) intermediate waves (8 < <i<T</i<<sub<p</sub< < 13 s), and (iii) long waves (<i<T</i<<sub<p</sub<< 13 s) based on peak period (<i<T</i<<sub<p</sub<) and the percentages of occurrence of each category are estimated. Long period waves are observed mainly during the pre- and the postmonsoon seasons. During the southwest monsoon period, the waves with period < 13 s are a minimum. An event during 2011 is identified as swells propagated from the Southern Ocean with an estimated travelling time of 5–6 days. The swells reaching the Arabian Sea from the south Indian Ocean and Southern Ocean, due to storms during the pre- and postmonsoon periods, modify the near surface winds due to higher phase wave celerity than the wind speed. Estimation of inverse wave age using large-scale winds such as NCEP (National Centers for Environmental Prediction) reflects the presence of cyclonic activity during pre- and postmonsoon seasons but not the effect of the local sea breeze/land breeze wind system.
abstractGer	Wave data collected off Ratnagiri, west coast of India, during 1 May 2010 to 30 April 2012 are used in this study. Seasonal and annual variations in wave data controlled by the local wind system such as sea breeze and land breeze, and remote wind generated long period waves are also studied. The role of sea breeze on the sea state during pre- and postmonsoon seasons is studied and it is found that the maximum wave height is observed at 15:00 UTC during the premonsoon season, with an estimated difference in time lag of 1–2 h in maximum wave height between premonsoon and postmonsoon seasons. Observed waves are classified in to (i) short waves (<i<T</i<<sub<p</sub< < 8 s), (ii) intermediate waves (8 < <i<T</i<<sub<p</sub< < 13 s), and (iii) long waves (<i<T</i<<sub<p</sub<< 13 s) based on peak period (<i<T</i<<sub<p</sub<) and the percentages of occurrence of each category are estimated. Long period waves are observed mainly during the pre- and the postmonsoon seasons. During the southwest monsoon period, the waves with period < 13 s are a minimum. An event during 2011 is identified as swells propagated from the Southern Ocean with an estimated travelling time of 5–6 days. The swells reaching the Arabian Sea from the south Indian Ocean and Southern Ocean, due to storms during the pre- and postmonsoon periods, modify the near surface winds due to higher phase wave celerity than the wind speed. Estimation of inverse wave age using large-scale winds such as NCEP (National Centers for Environmental Prediction) reflects the presence of cyclonic activity during pre- and postmonsoon seasons but not the effect of the local sea breeze/land breeze wind system.
abstract_unstemmed	Wave data collected off Ratnagiri, west coast of India, during 1 May 2010 to 30 April 2012 are used in this study. Seasonal and annual variations in wave data controlled by the local wind system such as sea breeze and land breeze, and remote wind generated long period waves are also studied. The role of sea breeze on the sea state during pre- and postmonsoon seasons is studied and it is found that the maximum wave height is observed at 15:00 UTC during the premonsoon season, with an estimated difference in time lag of 1–2 h in maximum wave height between premonsoon and postmonsoon seasons. Observed waves are classified in to (i) short waves (<i<T</i<<sub<p</sub< < 8 s), (ii) intermediate waves (8 < <i<T</i<<sub<p</sub< < 13 s), and (iii) long waves (<i<T</i<<sub<p</sub<< 13 s) based on peak period (<i<T</i<<sub<p</sub<) and the percentages of occurrence of each category are estimated. Long period waves are observed mainly during the pre- and the postmonsoon seasons. During the southwest monsoon period, the waves with period < 13 s are a minimum. An event during 2011 is identified as swells propagated from the Southern Ocean with an estimated travelling time of 5–6 days. The swells reaching the Arabian Sea from the south Indian Ocean and Southern Ocean, due to storms during the pre- and postmonsoon periods, modify the near surface winds due to higher phase wave celerity than the wind speed. Estimation of inverse wave age using large-scale winds such as NCEP (National Centers for Environmental Prediction) reflects the presence of cyclonic activity during pre- and postmonsoon seasons but not the effect of the local sea breeze/land breeze wind system.
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title_short	Influence of winds on temporally varying short and long period gravity waves in the near shore regions of the eastern Arabian Sea
url	https://doi.org/10.5194/os-9-343-2013 https://doaj.org/article/d8aad5a5657e46d89641bad74084986a http://www.ocean-sci.net/9/343/2013/os-9-343-2013.pdf https://doaj.org/toc/1812-0784 https://doaj.org/toc/1812-0792
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An event during 2011 is identified as swells propagated from the Southern Ocean with an estimated travelling time of 5–6 days. The swells reaching the Arabian Sea from the south Indian Ocean and Southern Ocean, due to storms during the pre- and postmonsoon periods, modify the near surface winds due to higher phase wave celerity than the wind speed. Estimation of inverse wave age using large-scale winds such as NCEP (National Centers for Environmental Prediction) reflects the presence of cyclonic activity during pre- and postmonsoon seasons but not the effect of the local sea breeze/land breeze wind system.</subfield></datafield><datafield tag="653" ind1=" " ind2="0"><subfield code="a">Geography. Anthropology. Recreation</subfield></datafield><datafield tag="653" ind1=" " ind2="0"><subfield code="a">G</subfield></datafield><datafield tag="653" ind1=" " ind2="0"><subfield code="a">Environmental sciences</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">V. 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Influence of winds on temporally varying short and long period gravity waves in the near shore regions of the eastern Arabian Sea

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