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Spectral wave characteristics off Gangavaram, Bay of Bengal

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Abstract

Spectral wave characteristics were studied based on waves measured for 1 year during 2010 off Gangavaram, Bay of Bengal. Maximum wave height of 5.2 m was observed on 19 May 2010 due to the influence of cyclonic storm LAILA. The wave spectrum was single-peaked during 57 % of the time and the double-peaked spectrum observed was mainly swell-dominated. Low-frequency waves (0.05–0.15 Hz) were predominantly from 150° to 180°, whereas high-frequency waves (>0.15 Hz) during November–January were mainly from 90° to 120°, and during July and August from 180° to 210°. Annual average significant wave height was similar to the value (1 m) observed in the eastern Arabian Sea.

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References

  • Aranuvachapun S (1987) Parameters of JONSWAP spectral model for surface gravity waves—I. Monte Carlo simulation study. Ocean Eng 14:89–115

    Article  Google Scholar 

  • Baba M, Dattatri J, Abraham S (1989) Ocean wave spectra off Cochin, west coast of India. Indian J Mar Sci 18:106–112

    Google Scholar 

  • Barstow SB, Kollstad T (1991) Field trials of the directional waverider. In: Proceedings of the first international offshore and polar engineering conference III, pp 55–63

  • Chakrabarti SK (2005) Handbook of offshore engineering, vol 1., Ocean Engineering Series. Elsevier, Amsterdam

    Google Scholar 

  • Chen G, Chapron B, Ezraty R, Vandemark D (2002) A global view of swell and wind sea climate in the ocean by satellite altimeter and scatterometer. J Atmos Ocean Tech 19:1849–1859

    Article  Google Scholar 

  • Datawell (2009) Datawell Waverider Reference Manual. Datawell BV oceanographic instruments, The Netherlands

  • Dattatri J, Jothi Shankar N, Raman H (1977) Comparison of Scott spectra with ocean wave spectra. J Waterways Port Coastal Ocean Eng ASCE 103:375–378

    Google Scholar 

  • Donelan MA, Dobsen F, Smith S, Anderson R (1993) On the dependence of sea surface roughness on wave development. J Phys Oceanogr 23:2143–2149

    Article  Google Scholar 

  • Drennan WM, Graber HC, Hauser D, Quentin C (2003) On the wave age dependence of wind stress over pure wind seas. J Geophys Res 108:8062. doi:10.1029/2000JC000715

    Article  Google Scholar 

  • Dube SK, Rao AD, Sinha PC, Murty TS, Bahulayan N (1997) Storm surge in the Bay of Bengal and Arabian Sea: the problem and its prediction. Mausam 48:283–304

    Google Scholar 

  • Glejin J, Kumar VS, Philip CS, Singh J, Pednekar P, Kumar KA, Dora UG, Gowthaman R (2012) Variations in swells along eastern Arabian Sea during the summer monsoon. Open J Mar Sci 2:43–50

    Article  Google Scholar 

  • Glejin J, Kumar VS, Nair TMB, Singh J (2013) Influence of winds on temporally varying short and long period gravity waves in the near shore regions of eastern Arabian Sea. Ocean Sci 9:343–353

    Article  Google Scholar 

  • Goda Y (1970) Numerical experiments on wave statistics with spectral simulation. In: Report Port and Harbour Research Institute, vol 9, Japan, pp 3–57

  • Goda Y (1976) “On Wave Groups”. Proc Conf Behav Offshore Struct Trondheim 1:115–128

    Google Scholar 

  • Goda Y (1983) Analysis of wave grouping and spectra of long-travelled swell. Japan. Rep Port Harb Res Inst 22:3–41

    Google Scholar 

  • Hanley KE, Belcher SE, Sullivan PP (2010) A global climatology of wind–wave interaction. J Phys Oceanogr 40:1263–1282

    Article  Google Scholar 

  • Hanson JL, Phillips OM (1999) Wind sea growth and dissipation in the open ocean. J Phys Oceanogr 29:1633–1648

    Article  Google Scholar 

  • Harish CM, Baba M (1986) Spectral and statistical properties of shallow water waves. Ocean Eng 13:239–248

    Article  Google Scholar 

  • Hasselmann K, Barnett TP, Bouws E, Carlson H, Cartwright DE, Enke K, Ewing JA, Gienapp H, Hasselmann DE, Kruseman P, Meerburg A, Muller P, Olbers DJ, Richter K, Sell W, Walden H (1973) Measurements of wind-wave growth and swell decay during the Joint North Sea Wave Project (JONSWAP). Deutsche Hydrograph Z A 12:95

    Google Scholar 

  • Haver S (1980) Analysis of uncertainties related to the stochastic modelling of ocean waves. Division of Marine structures, The Norwegian Institute of Technology, Norway, Report No. UR-80-09, p 187

  • Kalnay E, Kanamitsu M, Kistler R, Collins W, Deaven D, Gandin L, Iredell M, Saha S, White G, Woollen J, Zhu Y, Leetmaa A, Reynolds B, Chelliah M, Ebisuzaki W, Higgins W, Janowiak J, Mo KC, Ropelewski C, Wang J, Jenne Roy, Joseph D (1996) The NCEP/NCAR 40-year reanalysis project. Bull Am Meteorol Soc 77:437–471

    Article  Google Scholar 

  • Kitaigordskii SA, Krasitskii VP, Zaslavskii MM (1975) On Phillips theory of equilibrium range in the spectra of wind generated gravity waves. J Phys Oceanogr 5:410–420

    Article  Google Scholar 

  • Kuik AJ, Vledder G, Holthuijsen LH (1988) A method for the routine analysis of pitch and roll buoy wave data. J Phys Oceanogr 18:1020–1034

    Article  Google Scholar 

  • Kumar VS, Kumar KA (2008) Spectral representation of high shallow water waves. Ocean Eng 35:900–911

    Article  Google Scholar 

  • Kumar VS, Sajiv P (2010) Variations in long term wind speed during different decades in Arabian Sea and Bay of Bengal. J Earth Syst Sci 119(5):639–653

    Article  Google Scholar 

  • Kumar VS, Mandal S, Anand NM, Nayak BU (1994) Spectral representation of measured shallow water waves. In: Proceedings of Indian national conference on harbour and ocean engineering (INCHOE-94), vol 1. CWPRS, Pune, pp 23–32

  • Kumar VS, Anand NM, Kumar KA, Mandal S (2003) Multipeakedness and groupiness of shallow water waves along Indian coast. J Coastal Res 19:1052–1065

    Google Scholar 

  • Kumar VS, Kumar KA, Raju NSN (2004) Wave characteristics off Visakhapatnam coast during a cyclone. Curr Sci 86(11):1524–1529

    Google Scholar 

  • Kumar VS, Philip S, Nair TNB (2010) Waves in shallow water off west coast of India during the onset of summer monsoon. Ann Geophys 28:817–824

    Google Scholar 

  • Kumar VS, Shanas PR, Dubhashi KK (2014) Shallow water wave spectral characteristics along the eastern Arabian Sea. Nat Hazards 70:377–394. doi:10.1007/s11069-013-0815-7

    Article  Google Scholar 

  • Myrhaug D, Slaattelid OH (1999) Statistical properties of successive wave periods. J Offshore Mech Arctic Eng 121:166–177

    Article  Google Scholar 

  • Narasimhan S, Deo MC (1979) Spectral analysis of ocean waves—a study. In: Proceedings of the conference on civil engineering in oceans, ASCE, pp 877–892

  • Ochi MK, Hubble EN (1976) On six parameter wave spectra. In: Proceedings of the 15th coastal engineering conference, ASCE, pp 321–328

  • Pierson WJ, Moskowitz L (1964) A proposed form for fully developed seas based on the similarity theory of S.A.Kitaigorodski. J Geophys Res 69:5181–5190

    Article  Google Scholar 

  • Portilla J, Ocampo-Torres FJ, Monbaliu J (2009) Spectral partitioning and identification of wind sea and swell. J Atmos Ocean Tech 26:117–122

    Article  Google Scholar 

  • Rao CVKP, Baba M (1996) Observed wave characteristics during growth and decay: a case study. Cont Shelf Res 16(12):1509–1520

    Article  Google Scholar 

  • Sajiv PC, Kumar VS, Johnson G, Dora GU, Vinayaraj P (2012) Interannual and seasonal variations in nearshore wave characteristics off Honnavar, west coast of India. Curr Sci 103(3):286–292

    Google Scholar 

  • Scott JR (1965) A sea spectrum for model test and long-term ship prediction. J Ship Res 9:145–152

    Google Scholar 

  • Soares CG (1991) On the occurrence of double peaked wave spectra. Ocean Eng 18(1/2):167–171

    Article  Google Scholar 

  • Suresh RRV, Annapurnaiah K, Reddy KG, Lakshmi TN, Balakrishnan Nair TM (2010) Wind sea and swell characteristics off east coast of India during southwest monsoon. Int J Oceans Oceanogr 4:35–44

    Google Scholar 

  • Thompson TS, Nelson AR, Sedivy DG (1984) Wave group anatomy. In: Proceeding of 19th conference on coastal engineering, vol 1. American Society of Civil Engineers, pp 661–677

  • Wolf J, Brown JM, Howarth MJ (2011) The wave climate of Liverpool Bay—observations and modelling. Ocean Dyn 61:639–655

    Article  Google Scholar 

Download references

Acknowledgments

The authors gratefully acknowledge the financial support given by the Earth System Science Organization, Ministry of Earth Sciences, Government of India, to conduct this research. The directors of CSIR-NIO, Goa, and INCOIS, Hyderabad, provided encouragement to carry out the study. We thank Mr. Arun Nherakkol, Scientist, INCOIS, and NIO colleagues Dr. B.P. Rao, Mr. N.S.N. Raju and Mr. Jai Singh for their help during data collection. Mr. Glejin Johnson, Research Scholar, CSIR-NIO, prepared Fig. 1. Gangavaram Port officials and Andhra University provided the logistics during the data collection period. We thank the two anonymous reviewers for critical comments and suggestions which improved the quality of the paper. This work is NIO contribution No. 5532.

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Correspondence to V. Sanil Kumar.

Appendix: Definition of wave parameters used in the study

Appendix: Definition of wave parameters used in the study

$$ {\text{Significant wave height }}\left( {H_{\text{s}} } \right) = 4 { }\sqrt {m_{o} } $$
(A1)
$$ {\text{Mean wave period }}(T_{{{\text{m}}_{02} }} ) = \sqrt {m_{0} /m_{2} } $$
(A2)
$$ {\text{Spectral narrowness parameter }}(\nu ) = \sqrt {\frac{{m_{0} \;m_{2} }}{{m_{1}^{2} }} - 1} $$
(A3)
$$ {\text{Spectral peakedness parameter (}}Q_{\text{p}} )= \frac{2}{{m_{0}^{2} }}\int\limits_{0}^{\infty } {fS^{2} (f)\;{\text{d}}f} $$
(A4)

where m n is the nth order spectral moment and is given by,

$$ m_{n} = \int\limits_{0}^{\infty } {f^{n} S(f)\;{\text{d}}f,\quad n = 0,1,2{\text{ and }}4} $$

S(f) is the spectral energy density at frequency f.

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Kumar, V.S., Dubhashi, K.K. & Nair, T.M.B. Spectral wave characteristics off Gangavaram, Bay of Bengal. J Oceanogr 70, 307–321 (2014). https://doi.org/10.1007/s10872-014-0223-y

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