Additionally, on comparing the model simulations with original sea ice data (daily or hourly data) and climatological sea ice data, a positive trend of \documentclass[12pt]{minimal} \usepackage{amsmath} \usepackage{wasysym} \usepackage{amsfonts} \usepackage{amssymb} \usepackage{amsbsy} \usepackage{mathrsfs} \usepackage{upgreek} \setlength{\oddsidemargin}{-69pt} \begin{document}$${P}_{\mathrm{w}}$$\end{document} P w was found to be enhanced by the reduction in the sea ice (reduction of direct wave attenuation due to the sea ice) and the increase in the surface wind.
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Increase in the wave power caused by decreasing sea ice over the Sea of Okhotsk in winter.
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