Abstract

The third generation wind-wave model Mike21-SW was used to study spectral characteristics of waves generated by the historical Cyclone Gonu in June 2007 along and off the Iranian coasts on the northern Oman Sea. The model was forced with the cyclone wind field generated using a Holland (1980) model based on cyclone data obtained from the Joint Typhon Warning Center (JTWC). The wave model was calibrated for the northern Oman Sea using bulk and spectral wave data at a station out of the Chabahar Bay. Evolution of directional-frequency spectra during the cyclone was investigated for two locations near the entrance and off the Chabahar Bay. At the offshore station, energy was contributed to the spectrum over an approximately 180 degree directional span that included different local and remotely generated waves. As the cyclone proceeded northwestward, all spectral directions continuously rotated in the clockwise direction at both locations. Frequency spectra at these locations were investigated for four different times corresponding to different locations of Cyclone’s eye and were justified using the sea growth parameter of the Joint North Sea Wave Project (JONSWAP) experiment. Using the modified JONSWAP parameters for hurricane conditions resulted in a frequency spectrum consistent with simulation results.

Highlights

  • The overarching aim of this study is to describe peaks of frequency spectra induced by Cyclone Gonu using traditional Joint North Sea Wave Project (JONSWAP) parameters, and examining the consistency between the simulated spectra and a modified representation of the JONSWAP spectrum for hurricane conditions

  • Since the focus of this paper is, studying wave spectra characteristics in the northern Oman Sea, simulated wave fields are investigated from 5 - 7 June 2007, when the eye was located between the Oman and Iranian coasts

  • Wave fields generated by Cyclone Gonu in the Arabian Sea and the northern Oman Sea were simulated using Mike21-SW, which was forced by a cyclone wind field generated using the approach of Holland [25]

Read more

Summary

Introduction

Tropical cyclones are energetic atmospheric phenomena with complex spatial. The response is always associated with extreme wave heights, large current velocities, and substantial water level variations (Allahdadi et al [1]). Tropical cyclones substantially contribute to transport of sediments and biogeochemical substances over oceanic and shelf waters (D’Sa et al [2]; Tehrani et al [3]; Chiaichtehrani [4]). Wave characteristics are among the most relevant oceanic responses of these storms, due to their destructive effects on structures and coastal communities as well as their substantial effects on transport phenomena in the shelf waters. Extreme wave heights generated by Cyclones are used as the main parameter for designing offshore and coastal structures. The wave height is used for studying beach erosion which is a common phenomenon during severe storms

Objectives
Results
Conclusion
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call