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Open AccessJournal ArticleDOI

Wave Directions in a Narrow Bay

TLDR
In this paper, three models with different assumptions on the directional coupling between the wave components were used to analyze the physics responsible for the directional behavior of the waves in the Baltic Sea.
Abstract
In slanting fetch conditions the direction of actively growing waves is strongly controlled by the fetch geometry. The effect was found to be pronounced in the long and narrow Gulf of Finland in the Baltic Sea, where it significantly modifies the directional wave climate. Three models with different assumptions on the directional coupling between the wave components were used to analyze the physics responsible for the directional behavior of the waves in the gulf. The directionally decoupled model produced the direction at the spectral peak correctly when the slanting fetch geometry was narrow but gave a weaker steering than observed when the fetch geometry was broader. The method of Donelan estimated well the direction at the spectral peak in well-defined slanting fetch conditions, but overestimated the longer fetch components during wave growth from a more complex shoreline. Neither the decoupled nor the Donelan model reproduced the observed shifting of direction with the frequency. The perform...

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Citations
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Journal Article

Wave hindcast statistics in the seasonally ice-covered Baltic Sea

TL;DR: Six years of wave hindcasts, calculated by the wave model WAM, are used to compile wave statistics for the Baltic Sea, finding the severest wave climate is in the Baltic Proper and the wave climate in the other basins is considerably less severe.
Book ChapterDOI

Recent Change—Sea Level and Wind Waves

TL;DR: In this paper, the authors describe observed changes in sea level and wind waves in the Baltic Sea basin over the past 200 years and the main climate drivers of this change, and the datasets available for studying these are described in detail.
Journal ArticleDOI

Spatial patterns of the wave climate in the Baltic Proper and the Gulf of Finland

TL;DR: In this article, a large part of the mismatches between long-term changes to wave properties at selected sites can be explained by the rich spatial patterns in changes to the Baltic Sea wave fields that are not resolved by the existing wave observation network.
Journal Article

Coastal erosion processes in the eastern Gulf of Finland and their links with geological and hydrometeorological factors

TL;DR: It is demonstrated that the most extreme erosion events occur when high waves excited by long-lasting western or south-western storms attack the coast during very high storm surges in the absence of stable sea ice.
References
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Journal ArticleDOI

High-resolution frequency-wavenumber spectrum analysis

TL;DR: In this article, a high-resolution frequency-wavenumber power spectral density estimation method was proposed, which employs a wavenumber window whose shape changes and is a function of the wave height at which an estimate is obtained.

Measurements of wind-wave growth and swell decay during the Joint North Sea Wave Project (JONSWAP)

TL;DR: In this article, wave spectra were measured along a profile extending 160 kilometers into the North Sea westward from Sylt for a period of two weeks in 1968 and 1969, with particular emphasis on wave growth under stationary offshore wind conditions and the attenuation of swell in water of finite depth.
Journal ArticleDOI

A proposed spectral form for fully developed wind seas based on the similarity theory of S. A. Kitaigorodskii

TL;DR: In this article, the authors used the data for the spectra of fully developed seas obtained for wind speeds from 20 to 40 knots as measured by anemometers on two weather ships.
Book

Dynamics and Modelling of Ocean Waves

TL;DR: The Wave Modelling Group (WAM) model as mentioned in this paper is based on a detailed physical description of air/sea interactions and is widely used for wave forecasting for meteorological and oceanographic purposes.
Journal ArticleDOI

Directional spectra of wind-generated waves

TL;DR: In this paper, the directional spectrum of wind-generated waves on deep water is determined by using a modification of Barber's (1963) method, and the results reveal that the frequency spectrum in the rear face is inversely proportional to the fourth power of the frequency.
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