Tropical Storm Patricia was a short-lived tropical cyclone that briefly affected parts of Baja California Sur before rapidly degenerating over water. Developing from a tropical wave that traversed the Atlantic Ocean during September 2009, Patricia was first classified as a tropical depression on October 11 several hundred miles south of the Baja California Peninsula. The system quickly intensified into a tropical storm as it tracked in a general northward direction. By October 12, Patricia attained its peak intensity with winds of 60 mph (95 km/h) and a minimum barometric pressure of 996 mbar (hPa; 29.41 inHg). The following day, increasing wind shear and unfavorable conditions caused the storm to rapidly weaken. By the morning of October 14, Patricia had degenerated into a non-convective remnant low near the southern coastline of Baja California Sur. The remnants of the storm persisted until October 15, at which time they dissipated over open waters. Although the center of Patricia did not impact land, the outer bands caused significant rainfall in portions of western Mexico. In Sonora, up to of rain fell, leading to significant flooding that left 600 people homeless. Other Mexican states received similar impact. Overall, the effects of Patricia were minor and resulted in no loss of life. Meteorological history Tropical Storm Patricia originated from a tropical wave that moved off the west coast of Africa on September 23. Two days later, Tropical Depression Eight developed from the wave over the eastern Atlantic Ocean. The depression tracked northwestward, while the wave continued a steady westward track. By October 6, the system crossed Central America and entered the eastern Pacific Ocean. Gradual development took place over the following several days with widespread, scattered convection consolidating around a developing area of low pressure. On October 11, a well-defined circulation had formed and the National Hurricane Center (NHC) estimated that it developed into a tropical depression roughly 405 mi (650 km) south-southeast of the southern tip of Baja California Sur. Several hours later, the system further strengthened into a tropical storm and was named Patricia. The low-level circulation became embedded within very deep convection and further intensification was anticipated. Patricia tracked north-northwest in a region of low to moderate wind shear, under the steering currents of a strong ridge of high pressure to the east and a trough located northwest. Although over warm sea surface temperatures, relatively stable air aloft prevented substantial intensification. By the