Improved Prediction of Local Significant Wave Height by Considering the Memory of Past Winds

Author:

Zhang Shaotong1ORCID,Yang Zhen2,Zhang Yaqi1,Zhao Shangrui2,Wu Jinran3,Wang Chenghao4ORCID,Wang You‐Gan3ORCID,Jeng Dong‐Sheng5,Nielsen Peter6ORCID,Li Guangxue1,Li Sanzhong1

Affiliation:

1. Frontiers Science Center for Deep Ocean Multispheres and Earth System Key Lab of Submarine Geosciences and Prospecting Techniques, MOE College of Marine Geosciences Ocean University of China Qingdao China

2. School of Science Wuhan University of Technology Wuhan China

3. Institute for Learning Sciences & Teacher Education Australian Catholic University Brisbane QLD Australia

4. National Engineering Research Center of Port Hydraulic Construction Technology Tianjin Research Institute for Water Transport Engineering, M.O.T. Tianjin China

5. School of Engineering and Built Environments Griffith University Gold Coast Campus Southport QLD Australia

6. School of Civil Engineering The University of Queensland‐St. Lucia Campus St. Lucia QLD Australia

Abstract

AbstractWave and water depth were measured with an instrumented tripod in the Yellow River Delta from 9 December 2014 to 29 April 2015. Concurrent wind data were also collected from a nearby wind station. A high‐precision model for predicting local significant wave height (Hs) with wind speed (vw) is constructed using an improved data‐driven approach. The proposed model realized high accuracy as it solves the problem that the Hs falls too fast during the wind‐decreasing periods. It was tackled by considering the remaining influence of historical vw on the present Hs via incorporating a memory curve of the past wind effect. This innovative approach significantly improves the prediction (R2 from 0.60 to 0.83). The winds in the past 24 hr still left an influence on the waves at the observation site although the influence decreases with time. Physically, it is an implicit but simpler consideration of wind fetch/duration. Further data modeling experiments indicated that the decisive factor for the Hs at the site is the wind speed. Wind directions slightly improve the prediction, indicating that waves are slightly affected by the underwater seabed slope along different wind directions, and northwest winds cause the strongest waves at the site. Adding atmospheric pressure or water depth even reduces the accuracy, which indicated that storm surges and wave deformations under different tide levels have a weak impact on Hs. The proposed local wave model can be easily constructed with available wind and wave data, making it expandable to other regions dominated by wind waves.

Funder

National Natural Science Foundation of China

Publisher

American Geophysical Union (AGU)

Subject

Water Science and Technology

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