Tropical Storm Brenda (1960)
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 Weather map of Brenda | |
| Meteorological history | |
|---|---|
| Formed | July 28, 1960 |
| Extratropical | July 31 |
| Dissipated | August 1, 1960 |
| Tropical storm | |
| 1-minute sustained (SSHWS/NWS) | |
| Highest winds | 70 mph (110 km/h) |
| Lowest pressure | 991 mbar (hPa); 29.26 inHg |
| Overall effects | |
| Fatalities | ≥1 indirect |
| Damage | $5 million (1960 USD) |
| Areas affected | Gulf Coast of the United States, East Coast of the United States, Eastern Canada |
| IBTrACS | |
Part of the 1960 Atlantic hurricane season | |
Tropical Storm Brenda was the second named storm of the 1960 Atlantic hurricane season. It developed in the northeastern Gulf of Mexico on July 28, and after moving ashore over the Florida Peninsula, it attained tropical storm status. It accelerated northeast along the U.S. East Coast, ultimately peaking as a moderate storm with winds of 60 mph (97 km/h) before crossing the Mid-Atlantic states and New England; it dissipated on July 31 over southern Canada. It inflicted moderate damage in Florida, the worst since Hurricane Easy of 1950, and dropped heavy rainfall as far north as New York City. Its total damage was estimated at US$5 million, and only indirect deaths were blamed on it.
Tropical storm (39–73 mph, 63–118 km/h)
Category 1 (74–95 mph, 119–153 km/h)
Category 2 (96–110 mph, 154–177 km/h)
Category 3 (111–129 mph, 178–208 km/h)
Category 4 (130–156 mph, 209–251 km/h)
Category 5 (≥157 mph, ≥252 km/h)
Unknown
Extratropical cyclone, remnant low, tropical disturbance, or monsoon depressionA weak low-pressure area that organized in the northeast Gulf of Mexico began to intensify on July 28, while located west of the Tampa Bay.[1] Early in its life, the system had a broad circulation with primarily light winds, similar to that of a subtropical storm.[2] The storm is estimated to have become a tropical depression earlier the previous day as it moved toward the northeast.[3] It made landfall along the Florida coast near Cross City and continued inland, gradually accelerating.[1] It likely attained tropical storm status at around 1200 UTC on July 28 while its center was situated west of Tampa.[3] The cyclone was named Brenda after reconnaissance aircraft confirmed that it had reached tropical storm strength.[1]
Brenda tracked northward, hugging the Georgia and South Carolina coasts before moving inland over North Carolina on July 29. It attained its peak winds of 60 mph (97 km/h) late that evening, while situated south of Wilmington.[3] The next morning, the storm emerged over the Chesapeake Bay moving northeast at about 30 mph (48 km/h).[4] Brenda crossed the Delmarva Peninsula and rapidly tracked into southern New Jersey. The storm crossed the state and eventually made another landfall in Brooklyn, New York before making yet another landfall in coastal Connecticut.[3]
At around 0000 UTC on July 31, Brenda moved into Massachusetts. Shortly thereafter, it lost its tropical characteristics and transitioned into an extratropical cyclone.[3] It dissipated by August 1 over southern Canada. Because Brenda was in the vicinity of land for most of its course, it was not able to intensify beyond tropical storm status.[1]
