4.3 Article

Evaluating the Accuracy of ERA5 Wave Reanalysis in the Water Around China

Journal

JOURNAL OF OCEAN UNIVERSITY OF CHINA
Volume 20, Issue 1, Pages 1-9

Publisher

OCEAN UNIV CHINA
DOI: 10.1007/s11802-021-4496-7

Keywords

wave hindcasting; reanalysis; ERA5; wave height; wave period

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Wave parameters are crucial for human activities, and in this study, the quality of wave height and wave period in ERA5 reanalysis was evaluated using data from six buoys near Chinese waters. The ERA5 data overestimated significant wave height, with large underestimation during tropical cyclones. The differences in annual wave period between ERA5 and buoys ranged from -1.31s to 0.4s, with better simulation effect in deep water areas.
Wave parameters, such as wave height and wave period, are important for human activities, such as navigation, ocean engineering and sediment transport, etc. In this study, wave data from six buoys around Chinese waters, are used to assess the quality of wave height and wave period in the ERA5 reanalysis of the European Centre for Medium-Range Weather Forecasts. Annual hourly data with temporal resolution are used. The difference between the significant wave height (SWH) of ERA 5 and that of the buoy varies from -0.35 m to 0.30 m for the three shallow locations; for the three deep locations, the variation ranges from -0.09 m to 0.09 m. The ERA5 SWH data show positive biases, indicating an overall overestimation for all locations, except for E2 and S1 where underestimation is observed. During the tropical cyclone period, a large (about 32%) underestimation of the maximum SWH in the ERA5 data is observed. Hence, the ERA5 SWH data cannot be used for design applications without site-specific validation. The difference between the annual wave period from ERA5 and the mean wave period from the buoys varies from -1.31s to 0.4s. Inter-comparisons suggest that the ERA5 dataset is consistent with the annual mean SWH. However, for the average period, the performance is not good, and half of the correlation coefficients in the four points are less 50%. Overall, the deep water area simulation effect is better than that in the shallow water.

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