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AbstractThe wave climate off northern Norway is considered and the investigation is based on wave measurements made at Tromsøflaket by means of a waverider buoy during the years 1977–1981. Data quality of waverider measurements is briefly commented upon; however, more emphasis is given to an evaluation of the long-term representativity of the actual measuring period and to a procedure accounting approximately for a lack of representativity. The wave climate is presented in terms of a smoothed joint probability density function of the significant wave height, Hs, and the spectral peak period, Tp. Based on this distribution a consistent design curve in the Hs, Tp space is established.
AbstractThe wave climate off northern Norway is considered and the investigation is based on wave measurements made at Tromsøflaket by means of a waverider buoy during the years 1977–1981. Data quality of waverider measurements is briefly commented upon; however, more emphasis is given to an evaluation of the long-term representativity of the actual measuring period and to a procedure accounting approximately for a lack of representativity. The wave climate is presented in terms of a smoothed joint probability density function of the significant wave height, Hs, and the spectral peak period, Tp. Based on this distribution a consistent design curve in the Hs, Tp space is established.
Wave climate off northern Norway
Haver, Sverre (author)
Applied Ocean Research ; 7 ; 85-92
1985-01-01
8 pages
Article (Journal)
Electronic Resource
English
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