Santiago T. Martin
A storm surge numerical model was developed to compute storm surges induced by a typhoon crossing Manila Bay. The linearized form of the vertically integrated equations of motion for shallow water were used. Five experiments were performed for each of the four cases of typhoon track. Results showed that for a typhoon crossing any point of the bay at any direction from the eastern side, the peak surge occurs at the northern portion of the bay. The highest value is generated by a typhoon moving westward and crosses the center of the bay.