4.7 Article

Propagation and attenuation of swell energy in the Pacific Ocean

期刊

RENEWABLE ENERGY
卷 188, 期 -, 页码 750-764

出版社

PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.renene.2022.02.071

关键词

Swell energy; Propagation characteristics; Attenuation rate; Intraseasonal oscillation

资金

  1. developing projection of Dalian Naval Academy
  2. open fund project of Shandong Provincial Key Laboratory of Ocean Engineering, Ocean University of China [kloe201901]
  3. National Key R&D Program of China (Technologyand application of wind power/photovoltaic power prediction for promoting renewable energy consumption) [2018YFB0904200]
  4. eponymous Complement S&T Program of State Grid Corporation of China [SGLNDKOOKJJS1800266]
  5. Major International (Regional) Joint Research Project of National Science Foundation of China [42120104001, .41520104008]
  6. [41520104008]

向作者/读者索取更多资源

This study analyzes the propagation, attenuation, and intraseasonal oscillation characteristics of swell energy in the Pacific Ocean. The results show that swells from the North and South Pacific typically propagate to low latitude waters and experience significant energy attenuation during the process.
Understanding the characteristics of swell propagation is practical for swell monitoring, early warning and wave power generation. In this study, the attenuation rate of swell energy during the propagation process is defined. Then, the propagation, attenuation and intraseasonal oscillation characteristics of swell energy in the Pacific Ocean are analyzed based on the 40-year European Centre for Medium-Range Weather Forecasts (ECMWF) reanalysis (ERA-40). Results show that (1) The swells generated from the North Pacific Ocean westerlies (NPOW) and the South Pacific Ocean westerlies (SPOW) usually propagate to the low latitude waters of the Pacific Ocean. (2) Swells in Hawaiian waters, Cologne Islands waters and Iquique waters mainly originate from the winter hemisphere. (3) It takes approximately 8 days for the swell to propagate from the SPOW to Cologne Islands waters. It takes approximately 7.5 days for the swell to travel from the NPOW to Cologne Islands waters. (4) An obvious attenuation of swell energy of 60%-90% occurs during the propagation process. (5) Swell energies in the SPOW, NPOW, Hawaiian waters, Cologne Islands waters and Iquique waters share a common quasi-biweekly oscillation. The attenuation rate of the swell energy has a significant quasi-weekly or quasi-biweekly oscillation.(c) 2022 Elsevier Ltd. All rights reserved.

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