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Perian data11/15/2023 ![]() Renew Energy 114:46–58Īnoop TR, Sanil Kumar V, Shanas PR, Johnson G (2015) Surface wave climatology and its variability in the North Indian Ocean based on ERA-Interim reanalysis. Ocean Eng 84:20–28Īboobacker VM, Shanas PR, Alsaafani MA, Albarakaati AMA (2017) Wave energy resource assessment for Red Sea. Geophys Res Lett 38(3):L03608Īboobacker VM, Seemanth M, Samiksha SV, Sudheesh K, Kerkar J, Vethamony P (2014) Sea breeze-induced wind sea growth in the central west coast of India. Cont Shelf Res 31(16):1701–1712Īboobacker VM, Vethamony P, Rashmi R (2011b) “Shamal” swells in the Arabian Sea and their influence along the west coast of India. Int J climatology 38:4417–4430Īboobacker VM, Rashmi R, Vethamony P, Menon HB (2011a) On the dominance of pre-existing swells over wind seas along the west coast of India. Int J Climatol 38:4405–4416Īboobacker VM, Shanas PR (2018b) The climatology of shamals in the Arabian Sea-part 2: surface waves. J Clim 28:819–837Īboobacker VM, Shanas PR (2018a) The climatology of shamals in the Arabian Sea-part 1: surface winds. Distinct features identified in the climate and trends of northerly winds and waves are further discussed.Īarnes OJ, Abdalla S, Bidlot JR, Breivik Ø (2015) Marine wind and wave height trends at different ERA-interim forecast ranges. The northern Arabian Sea including the Sea of Oman exhibits significant decreasing trend in northerly maximum wind speed (− 1.4 cm/s/year) and H s (− 0.67 cm/year), while the Gulf and the Red Sea exhibit sectorial contrasting trend, indicating the dominance of localized effects in modifying the regional climate. ![]() The study brings out an increasing trend in the northerly maximum wind speed (0.8–1.2 cm/s/year) and H s (0.42–0.88 cm/year) in the southern and central Arabian Sea, which is consistent with the global trend in extreme wind speed and H s. ![]() We have analyzed climatology and trends of northerly maximum wind speed and significant wave height (H s) in the Arabian Sea and the connected marginal seas, Arabian/Persian Gulf and the Red Sea, during non-monsoon season derived from 40 years of ERA5 wind and wave data, and estimated monthly, annual and decadal extreme climate and their trends. Recent studies point out the importance of northerly winds and waves in the Arabian Sea, especially those due to shamal and makran events in addition to the northeast monsoon system. ![]()
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