Laboratory of Wave Engineering, Department of Cybernetics, School of
Science, Tallinn University of Technology, Akadeemia tee 21, Tallinn, 12618,
Estonia
Estonian Academy of Sciences, Kohtu 6, Tallinn, 10130, Estonia
Katri Pindsoo
Laboratory of Wave Engineering, Department of Cybernetics, School of
Science, Tallinn University of Technology, Akadeemia tee 21, Tallinn, 12618,
Estonia
Laboratory of Wave Engineering, Department of Cybernetics, School of
Science, Tallinn University of Technology, Akadeemia tee 21, Tallinn, 12618,
Estonia
Maris Eelsalu
Laboratory of Wave Engineering, Department of Cybernetics, School of
Science, Tallinn University of Technology, Akadeemia tee 21, Tallinn, 12618,
Estonia
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Total article views: 2,043 (including HTML, PDF, and XML)
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Total article views: 1,310 (including HTML, PDF, and XML)
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Total article views: 733 (including HTML, PDF, and XML)
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Extreme water levels are often created by several drivers with different properties. For example, the contribution from the water volume of the Baltic Sea follows a Gaussian distribution, but storm surges represent a Poisson process. We show that wave set-up heights (the third major component of high water levels) usually follow an exponential distribution and thus also represent a Poisson process. However, at some locations set-up heights better match an inverse Gaussian (Wald) distribution.
Extreme water levels are often created by several drivers with different properties. For...
