Abstract
On 26 August 2011, the merger of two misocyclones was accompanied by surface wind gusts in western Tokyo, within the Tokyo Metropolitan Area Convective Study region. In this study, using data from a high-density ground weather observation network stations and the Doppler Radar for Airport Weather system at Haneda Airport, we clarified the merging process of the two misocyclones and the structure of the resulting vortex.
