Steepness of Surface Wind Waves in the Black Sea

Within the statistical description of wind waves, the steepness of individual waves, as well as their crests and troughs, is analyzed. The analysis was performed using data obtained in field conditions via an equipment with a high spatial and temporal resolution, which made it possible to consider short-period waves in a frequency range with an upper limit of 0.5 Hz. It has been shown that the steepness of individual waves can be several times greater than the spectral steepness calculated from spectral moments. The values of average horizontal asymmetry, which is defined as the ratio of the steepness of the leading and trailing fronts, and the average vertical asymmetry, which is defined as the ratio of the steepness of the crest and trough, are greater than 1. At the same time, individual waves are often observed whose horizontal and/or vertical asymmetry is less than 1. Empirical distributions have been constructed for the steepness of waves, their crests and troughs.

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Publication Details

Journal
Russian Meteorology and Hydrology
Published
2025-12-01
DOI
https://doi.org/10.3103/s1068373925120040
Primary Topic
Ocean Waves and Remote Sensing
Type
article
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article

Steepness of Surface Wind Waves in the Black Sea

A. S. Knyazkov, A. S. Zapevalov
Russian Meteorology and Hydrology
Ocean Waves and Remote Sensing
article

Steepness of Surface Wind Waves in the Black Sea

A. S. Knyazkov, A. S. Zapevalov
article en

Abstract

Within the statistical description of wind waves, the steepness of individual waves, as well as their crests and troughs, is analyzed. The analysis was performed using data obtained in field conditions via an equipment with a high spatial and temporal resolution, which made it possible to consider short-period waves in a frequency range with an upper limit of 0.5 Hz. It has been shown that the steepness of individual waves can be several times greater than the spectral steepness calculated from spectral moments. The values of average horizontal asymmetry, which is defined as the ratio of the steepness of the leading and trailing fronts, and the average vertical asymmetry, which is defined as the ratio of the steepness of the crest and trough, are greater than 1. At the same time, individual waves are often observed whose horizontal and/or vertical asymmetry is less than 1. Empirical distributions have been constructed for the steepness of waves, their crests and troughs.

Russian Meteorology and HydrologyVol. 50(12)
Russian Academy of Sciences (RU), Marine Hydrophysical Institute (RU)
Life below water
Openalex Percentile: Top 25%
Ocean Waves and Remote Sensing
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