Forecasting of Surface Currents via Correcting Wind Stress with Assimilation of High-Frequency Radar Data in a Three-Dimensional Model

<table class="table-group" id="tab3"><tr><td><table class="table"><tr><td class="thead-hr" colspan="3"><hr/></td></tr><tr class="thead"><td class="align_left">Time/model</td><td class="align_center">BG</td><td class="align_center">DA5</td></tr><tr><td class="thead-hr" colspan="3"><hr/></td></tr><tr><td class="align_left">03:00</td><td class="align_center">39.4507</td><td class="align_center">33.5558</td></tr><tr><td class="align_left">06:00</td><td class="align_center">49.4637</td><td class="align_center">42.9707</td></tr><tr><td class="align_left">09:00</td><td class="align_center">23.9298</td><td class="align_center">23.1958</td></tr><tr><td class="align_left">12:00</td><td class="align_center">52.729</td><td class="align_center">51.7525</td></tr><tr class="table-tr"><td colspan="3"><hr class="tbody-hr"/></td></tr></table></td></tr></table>

Advances in Meteorology

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Table 3

Table 3: Forecasting of Surface Currents via Correcting Wind Stress with Assimilation of High-Frequency Radar Data in a Three-Dimensional Model 