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Typhoon Nina (1975)

Pacific typhoon

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Through China and Lake


Meteorological history

A well defined trough line extending southeastward into the Philippine Sea spawned a disturbance on July 29. After its initial status as a disturbance, Tropical Depression 04W was designated and moved southwestward for 36 hours as the structure of the system began to organize. On July 31, the depression slowed and began to rapidly intensify, becoming a tropical storm and was named "Nina". It began to turn to the northwest afterward. A subtropical ridge prevented Nina from turning further north and it began to track west-northwest just before reaching typhoon intensity.

Nina underwent explosive development in the late hours of August 1. Aircraft reconnaissance reported a 65 hPa drop of pressure, with winds increasing from a mere 65 to 130 knots (75 to 150 mph; 120 to 241 km/h) the day after. During that period, it attained its peak intensity of 135 knots (155 mph; 250 km/h). The typhoon began to weaken as it approached Taiwan, making landfall near the coastal city of Hualien as a Category 3 storm with 100 kn (120 mph; 190 km/h) winds.

The storm began to weaken as it went across the island's central mountain range, sparing the most populated areas from the eyewall. It entered the Formosa Straits as a weak typhoon, making another landfall near Jinjiang, Fujian. After moving northwest and crossing Jiangxi, it turned north on the night of August 5 near Changde, Hunan. A day later, the storm moved over Xinyang, Henan, and was later blocked by a cold front near Zhumadian, Henan for three days. The stationary thunderstorm system brought heavy rainfall, causing the infamous collapse of the Banqiao Dam. The storm moved southwest on August 8, and dissipated soon afterwards.

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