Comparative Study of the Aladin and Arome Wind Effect on Waves Characteristics: Application on the International Port of Algiers

Authors

  • Sara Chikhi Department of Energetic and Fluid Mechanics, faculty of physics, University of Science and Technology Houari Boumedienne (USTHB), 16111 Algiers, Algeria
  • Mohamed El-Amine Slimani Department of Energetic and Fluid Mechanics, faculty of physics, University of Science and Technology Houari Boumedienne (USTHB), 16111 Algiers, Algeria;Numerical Weather Forecast, National Center for Meteorology, Avenue Mohamed Khemisti BP 153 Dar el Beida,16011 Algiers, Algeria

DOI:

https://doi.org/10.30564/jasr.v2i3.708

Abstract

The sea states numerical modeling has been developed for years, it used for very varied fields such as the sizing of coastal work, the safety of navigation, the study of the stability of the beaches or the water leisure.  The spectral third-generation ocean wind-wave model WAVEWATCH III (WW3) software was adopted and developed for simulating wave propagation in the Mediterranean basin.  In this study, a more detailed study was carried out on the port of Algiers. Two different atmospheric models have been used to get the wind forcing: ALADIN (Area Limited Dynamic Adaptation Inter National Development) with an 8 km resolution. And AROME (Application to Operational Research at Meso-scale) with a 3 km resolution. The results obtained using both of the atmospheric models have been compared and analyzed.

Keywords:

Wind-Waves; Wave propagation; Mediterranean basin; WAVEWATCH; Wave-characteristics

References

[1] Ardhuin, F., Jenkins, A. D., & Belibassakis, K. A.. Comments on “The Three-Dimensional Current and Surface Wave Equations.” Journal of Physical Oceanography, 2008a, 38(6): 1340–1350. https://doi.org/10.1175/2007jpo3670.1

[2] Ardhuin, F., Marié, L., Rascle, N., Forget, P., & Roland, A.. Observation and estimation of Lagrangian, Stokes and Eulerian currents induced by wind and waves at the sea surface, 2008b: 2820–2838. https://doi.org/10.1175/2009JPO4169.1

[3] Benassai, G., & Ascione, I.. Implementation and Validation of Wave Watch III Model Offshore the Coastlines of Southern Italy, 2008: 553–560. https://doi.org/10.1115/omae2006-92555

[4] Bouws, E., Günther, H., Rosenthal, W., & Vincent, C. L.. Similarity of the wind-wave spectrum in finite depth water. Spectral Form. J. Geophys. Res, 1985, 90(C1): 975–986.

[5] Chen, Q., Zhao, H., Hu, K., & Douglass, S. L.. Prediction of Wind Waves in a Shallow Estuary. Journal of Waterway, Port, Coastal, and Ocean Engineering, 2005, 131(4): 137–148. https://doi.org/10.1061/(asce)0733-950x(2005)131:4(137)

[6] Mentaschi, L., Besio, G., Cassola, F., & Mazzino, A.. Performance evaluation of Wavewatch III in the Mediterranean Sea. Ocean Modelling, 2015, 90: 82–94. https://doi.org/10.1016/j.ocemod.2015.04.003

[7] Okihiro, M., Guza, R. T., & Seymour, R. J.. Excitation of Seiche Observed in a Small Harbor which are sheltered frequency The oscillatory outside the harbor at swell frequencies -2 Hz ). 1993, 98.

[8] Rascle, N., & Ardhuin, F.. Drift and mixing under the ocean surface revisited: Stratified conditions and model-data comparisons. Journal of Geophysical Research: Oceans, 2009, 114(2): 1–17. https://doi.org/10.1029/2007JC004466

[9] Zijlema, M., Van Vledder, G. P., & Holthuijsen, L. H.. Bottom friction and wind drag for wave models. Coastal Engineering, 2012, 65: 19–26. https://doi.org/10.1016/j.coastaleng.2012.03.002

[10] Zodiatis, G., Galanis, G., Nikolaidis, A., Kalogeri, C., Hayes, D., Georgiou, G. C., … Kallos, G.. Wave energy potential in the Eastern Mediterranean Levantine Basin. An integrated 10-year study. Renewable Energy, 2014, 69: 311–323. https://doi.org/10.1016/j.renene.2014.03.051

Downloads

How to Cite

Chikhi, S., & Slimani, M. E.-A. (2019). Comparative Study of the Aladin and Arome Wind Effect on Waves Characteristics: Application on the International Port of Algiers. Journal of Atmospheric Science Research, 2(3), 1–5. https://doi.org/10.30564/jasr.v2i3.708

Issue

Article Type

Article