Feedback

Anomalous dispersion of fourier components of surface gravity waves in the near shore area

ORCID
0000-0002-6673-8273
Affiliation/Institute
Leichtweiß-Institut
Büsching, Fritz

Water level deflections eta(t) have been measured synchronously at some positions in a beach profile on the isle of SYLT/North Sea during severe storm surge conditions as well as at attenuating wave action. A steadily increasing wave period T in the upbeach direction, turning out z from strip chart evaluations, is in accordance with the result of FOURIER syntheses. Near shore wave deformation is explained by ANOMALOUS dispersion of the frequency components.

Cite

Citation style:
Could not load citation form.

Access Statistic

Total:
Downloads:
Abtractviews:
Last 12 Month:
Downloads:
Abtractviews:

Rights

Use and reproduction:
All rights reserved