A very interesting excerpt from a very interesting paper:
Lander (1994b) defined the evolution of the monsoon trough into a large cyclonic vortex that became nearly circular with a radius of 2500 km in the sea-level pressure field (Fig. 8). The circulation takes on the character of a large monsoon depression such that the strongest winds are located at large distances from the center. Convection is concentrated in a large cyclonically-curved band that extends along the southern and eastern periphery of the circulation. Once the monsoon gyre has formed it tends to persist for a period of weeks.
Often, the convection along the eastern periphery of the gyre is the source for many MCSs that may form into small tropical cyclones. Harr et al. (1996a) define the formation of Tropical Storm Ofelia from MCS activity associated with an active monsoon gyre.
Lander (1994b) defines two distinct modes of a monsoon gyre life cycle. The first is the production of a small tropical cyclone from the periphery convection to the east of the gyre center. The second mode is the acceleration of the peripheral winds around the gyre such that the gyre itself becomes a large tropical cyclone (Fig. 9). Chen et al. (2004) indicate that nearly 70% of western North Pacific tropical cyclone formations are associated with a monsoon gyre, which is a much higher percentage than defined by Lander (1994b).
http://www.weather.nps.navy.mil/~cpchang/IWM-III/R10-B3e-Tropical%20Cyclones.pdf