page_title: Hurricane Nora (2003)
section_title: Meteorological history
hierarchical_section_title: Hurricane Nora (2003) / Meteorological history
caption_attribution_description: The MODIS instrument onboard NASA’s Aqua satellite captured this true-color image of two tropical systems in the eastern Pacific Ocean: Tropical Storm Nora (upper left) and Tropical Storm Olaf (bottom right). At the this image was taken Nora had maximum sustained winds of 46 mph while Olaf had sustained winds of 50 mph and was forecast to slightly strengthen before making landfall near Manzanillo.
context_page_description: Hurricane Nora was the final of five tropical cyclones to make landfall in the 2003 Pacific hurricane season. The fourteenth named storm and fifth hurricane of the season, Nora developed on October 1 from a tropical wave. It slowly intensified as it moved northwestward, intensifying into a hurricane on October 4. That day, Nora rapidly intensified to its peak of 100 mph, but the larger Hurricane Olaf to its east prevented further strengthening. An approaching trough turned the rapidly weakening system to the east toward Mexico. By October 7, it was downgraded to a tropical depression. Although it no longer met the criteria for being a tropical cyclone, the National Hurricane Center continued issuing advisories due to the cyclone's proximity with land. Nora unexpectedly redeveloped an area of thunderstorms and moved ashore near Mazatlán, Sinaloa on October 9 before dissipating. The depression dropped locally heavy rainfall in western Mexico, but there were no reports of damage. Later, the remnants combined with Olaf and an upper-level low to produce flooding and a tornado in central Texas.
context_section_description: The origins of Nora were from a tropical wave that exited the west coast of Africa on September 13. It moved westward across the Atlantic Ocean and Caribbean Sea without developing. The wave axis crossed Central America on September 25, with its convection tracking westward along the southern Mexican coastline. On September 29, the system became better organized when it reached a position about 100 mi (160 km) south of Acapulco. Although upper-level wind shear was only marginally favorable, the National Hurricane Center first noted the potential for tropical cyclogenesis on September 30 over the subsequent few days. This verified on October 1 after the thunderstorms organized enough for the system to be classified as Tropical Depression Fourteen-E. At the time, it was located about 600 mi (975 km) south of the southern tip of the Baja California peninsula.
  Upon developing, the depression had a well-defined low-level circulation, and with a ridge to the north, it moved south of due west. Conditions favored further development, including low wind shear and warm water temperatures. The convection gradually organized, and the depression intensified into Tropical Storm Nora early on October 2. Its motion briefly became nearly stationary as Nora rounded the furthest extent of the ridge, although a steady motion to the northwest began on October 3. That day, an eye feature developed in the center of the deep convection, and Nora attained hurricane status early on October 4. Steady intensification continued to winds of 100 mph (160 km/h) by later that day, and favorable conditions were expected to allow the hurricane to reach major hurricane status, or winds of 115 mph (185 km/h). However, Nora did not intensify further, due to unfavorable increased wind shear from the developing Tropical Storm Olaf to its east.
  By October 5, the eye of Nora was no longer evident on satellite imagery, which indicated the beginning of a weakening trend. However, a Special Sensor Microwave/Imager observed a small eye that was open to the northwest. The convection became ragged, and on October 6 the winds decreased below hurricane-force. Around the same time, a strong approaching mid-level trough caused Nora to slow and turn to the east. Continued wind shear and the presence of dry air stripped the thunderstorms away from the center, and by October 7 all of the deep convection had dissipated. As a result, it was downgraded to a tropical depression, and Nora weakened to the extent that it barely met the criteria for being a tropical cyclone. The NHC maintained advisories due to the circulation's proximity to western Mexico, as well as the unlikely potential for redeveloping thunderstorms due to its movement over warmer waters. Nora accelerated to the east-northeast and later to the northeast due to the advancing trough. As it approached western Mexico, an area of curved convection unexpectedly developed over the center. Without additional redevelopment, the poorly defined circulation of Nora made landfall near Mazatlán, Sinaloa early on October 9. It dissipated shortly thereafter over the high terrain of western Mexico.
caption: Nora (left) and Olaf (right) both approaching Mexico on October 6
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