Predictability of storm wave heights in the ice-free Beaufort Sea |
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| Authors: | Takehiko Nose Adrean Webb Takuji Waseda Jun Inoue Kazutoshi Sato |
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| Institution: | 1.Department of Ocean Technology, Policy, and Environment,The University of Tokyo,Kashiwa,Japan;2.Disaster Prevention Research Institute,Kyoto University,Kyoto,Japan;3.National Institute for Polar Research,Tachikawa,Japan;4.Application Laboratory,Japan Agency for Marine-Earth Science and Technology,Yokohama,Japan;5.Kitami Institute of Technology,Kitami,Japan |
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| Abstract: | A predictability study on wave forecast of the Arctic Ocean is necessary to help identify hazardous areas and ensure sustainable shipping along the trans-Arctic routes. To assist with validation of the Arctic Ocean wave model, two drifting wave buoys were deployed off Point Barrow, Alaska for two months in September 2016. Both buoys measured significant wave heights exceeding 4 m during two different storm events on 19 September and 22 October. The NOAA-WAVEWATCH III? model with 16-km resolution was forced using wind and sea ice reanalysis data and obtained general agreement with the observation. The September storm was reproduced well; however, model accuracy deteriorated in October with a negative wave height bias of around 1 m during the October storm. Utilising reanalysis data, including the most up-to-date ERA5, this study investigated the cause: grid resolution, wind and ice forcing, and in situ sea level pressure observations assimilated for reanalysis. The analysis has found that there is a 20% reduction of in situ SLP observations in the area of interest, presumably due to fewer ships and deployment options during the sea ice advance period. The 63-member atmospheric ensemble reanalysis, ALERA2, has shown that this led to a larger ensemble spread in the October monthly mean wind field compared to September. Since atmospheric physics is complex during sea ice advance, it is speculated that the elevated uncertainty of synoptic-scale wind caused the negative wave model bias. This has implications for wave hindcasts and forecasts in the Arctic Ocean. |
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