Abstract

Over the past several decades, an increasing number of studies have focused on the global view of swell and wind sea climate. However, our understanding of wind sea and swell is still incomplete as is the lack of an integrated description for all the wave components. In this paper, the European Centre for Medium-Range Weather Forecasts (ECMWF) Era-medium wind data is used to run the WAVEWATCH III model and the global wave fields in 2010 are reproduced. Using the spectra energy partition (SEP) method, two-dimensional wave spectra were separated and detailed information for the components of wind sea and swell was obtained. We found that the highest seasonal mean energy of swell and wind sea are distributed in the respective winter hemispheres. In most seas, swell carries a large part of the wave energy withWsbeing higher than 50%. Compared to swell, the global distribution of wind sea energy is highly affected by the seasons. We also established a link between inverse wave age and the ratio of swell energy to total wave energy. This study aims to improve our understanding of surface wave energy composition and thus the parameterization of global-scale wind-wave interaction and air-sea momentum flux.

Highlights

  • Ocean surface gravity waves are the medium that transfers energy across the air-sea surface

  • The significant wave height (SWH) of total waves obtained from the WAVEWATCH III model output were compared against the NDBC buoy data using temporal correlation analyses

  • After separating wind sea and swell from mixed waves, we studied the spatial and seasonal distribution of swell and wind sea energy

Read more

Summary

Introduction

Ocean surface gravity waves are the medium that transfers energy across the air-sea surface. It was estimated by Wang and Huang [1] that the global wind energy input for the formation of surface waves is 60 TW. Some portion is even transported back to the atmosphere through air-sea interaction. From results obtained during several sea expeditions, Grachev and Fairall (2001) [3] found that, in the equatorial west Pacific Ocean, upward energy and momentum transfer occurs about 10% of the time

Objectives
Results
Conclusion
Full Text
Paper version not known

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