The origins of Hurricane Dora can be traced back to a tropical wave that emerged off the western African coast on July 7.
The disturbance tracked into the Caribbean Sea seven days later without any signs of development.
However, the system encountered an enhanced flow of moisture in the southwestern Caribbean, allowing for organization and the formation of a broad low-pressure area on July 15.
Upon tracking into the eastern Pacific, the National Hurricane Center (NHC) judged the storm to have had a low chance developing into a tropical cyclone.
The next day, thunderstorm activity erupted around the system, and at 1500 UTC on July 18, the NHC declared the vigorous disturbance to have reached tropical depression status; in post-season analysis, the NHC found that Dora was already a tropical storm by this point after developing six hours earlier.

After development, Dora was steered towards the northwest by a ridge over the Southwestern United States.
Situated in an area of favorable atmospheric conditions and warm sea surface temperatures, the tropical cyclone quickly strengthened, developing an intermittent eye before being classified as a hurricane at 1800 UTC on July 19.
At the time, the storm was roughly 245 mi (400 km) south-southwest of Puerto Escondido, Oaxaca.
Upon reaching hurricane status, Dora began an episode of rapid intensification as its inner structure became more well-defined and its eye more permanent.
At the same time, mesovorticies within the eye—often indicators of intense tropical cyclones—were noted on satellite imagery.
By 1800 UTC on July 20, Dora had attained the threshold for major hurricane status.
After acquiring some characteristics of an annular hurricane early on July 21, Dora reached its peak intensity at 1200 UTC that day with a minimum barometric pressure of 929 mbar (hPa; 27.43 inHg) and maximum sustained winds of 155 mph (250 km/h), making it a high-end Category 4 on the Saffir–Simpson hurricane wind scale.

Dora held its peak strength for just six hours before it began to weaken due to cooler waters and the presence of wind shear.
Although the hurricane's initial weakening phase was gradual, the overall structure of Dora quickly deteriorated in response to increasingly hostile wind shear around the storm.
The storm's eye abruptly dissipated less than 12 hours after Dora's peak intensity, By 1800 UTC on July 22, the tropical cyclone had weakened to tropical storm intensity, undergoing an 80 mph (130 km/h) decrease in winds in just 24 hours.
Continued weakening prompted the NHC to downgrade Dora to a tropical depression two days later at 1200 UTC as the system curved west of the Baja California Peninsula.
Twelve hours later, the system degenerated into a remnant low pressure area devoid of any thunderstorm activity.
The low persisted for a day as it tracked north-northwestward, eventually dissipating 70 mi (110 km) south-southwest of Bahía Asunción on July 26.
The origins of Hurricane Dora can be traced back to a tropical wave that emerged off the western African coast on July 7. The disturbance tracked into the Caribbean Sea seven days later without any signs of development. However, the system encountered an enhanced flow of moisture in the southwestern Caribbean, allowing for organization and the formation of a broad low-pressure area on July 15. Upon tracking into the eastern Pacific, the National Hurricane Center (NHC) judged the storm to have had a low chance developing into a tropical cyclone. The next day, thunderstorm activity erupted around the system, and at 1500 UTC on July 18, the NHC declared the vigorous disturbance to have reached tropical depression status; in post-season analysis, the NHC found that Dora was already a tropical storm by this point after developing six hours earlier.
After development, Dora was steered towards the northwest by a ridge over the Southwestern United States. Situated in an area of favorable atmospheric conditions and warm sea surface temperatures, the tropical cyclone quickly strengthened, developing an intermittent eye before being classified as a hurricane at 1800 UTC on July 19. At the time, the storm was roughly 245 mi (400 km) south-southwest of Puerto Escondido, Oaxaca. Upon reaching hurricane status, Dora began an episode of rapid intensification as its inner structure became more well-defined and its eye more permanent. At the same time, mesovorticies within the eye—often indicators of intense tropical cyclones—were noted on satellite imagery. By 1800 UTC on July 20, Dora had attained the threshold for major hurricane status. After acquiring some characteristics of an annular hurricane early on July 21, Dora reached its peak intensity at 1200 UTC that day with a minimum barometric pressure of 929 mbar (hPa; 27.43 inHg) and maximum sustained winds of 155 mph (250 km/h), making it a high-end Category 4 on the Saffir–Simpson hurricane wind scale.
Dora held its peak strength for just six hours before it began to weaken due to cooler waters and the presence of wind shear. Although the hurricane's initial weakening phase was gradual, the overall structure of Dora quickly deteriorated in response to increasingly hostile wind shear around the storm. The storm's eye abruptly dissipated less than 12 hours after Dora's peak intensity, By 1800 UTC on July 22, the tropical cyclone had weakened to tropical storm intensity, undergoing an 80 mph (130 km/h) decrease in winds in just 24 hours. Continued weakening prompted the NHC to downgrade Dora to a tropical depression two days later at 1200 UTC as the system curved west of the Baja California Peninsula. Twelve hours later, the system degenerated into a remnant low pressure area devoid of any thunderstorm activity. The low persisted for a day as it tracked north-northwestward, eventually dissipating 70 mi (110 km) south-southwest of Bahía Asunción on July 26.
Hurricane Dora (2011)