This paper reports finely resolved radar signatures of tornadogenesis associated with a typhoon and elucidates how a small-scale tornadic vortex emerged on the ground in relation to the parent storm structure. Approximately 5 min before producing JEF-2 damage, a counterrotating vortex pair appeared above the rear-flank outflow region. The vortex pair developed upward, and its counterclockwise vortex approached a preexisting mesocyclone located aloft. At their closest approach, an abrupt intensification of the counterclockwise vortex occurred in the upper part and propagated downward. Meanwhile, significant vortex shrinking occurred at low levels. As a result, a small-scale tornadic vortex emerged over the damaged area. We suggest that coupling of the vortex pair with a mesocyclone and near-surface vorticity stretching played crucial roles in tornadogenesis. Since the coupling occurred on a minute scale and was affected by subtle spatial change on a scale of hundreds of meters, the tornado occurred in highly sensitive conditions. Plain Language Summary A tropical cyclone-tornado, which is a major subset of damaging tornadoes that is not well understood as yet, was finely resolved by a rapid-scan radar at an extremely close range. We found that a vertical coupling between a transiently generated smaller-scale vortex and a preexisting larger-scale vortex played a crucial role in producing the tornado. The exceptionally small spatiotemporal scale of the coupling process suggests a highly sensitive nature of tornadogenesis.