The dissipating stage of the tropical cyclone where the surface pressure rises and the area affected by the cyclones diminishes in size as it recurves or dissipate due to friction and lack of moisture over continents or when colder and drier air enters through when they go poleward.
Land masses weaken typhoons, causing them to dissipate if the land mass is large. ... If a typhoon moves over land, this supply of warm ocean water is cut off, and the typhoon dissipates.
