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Hurricane Agnes

Category 1 Atlantic hurricane in 1972

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Hurricane Agnes near peak intensity while in the Gulf of Mexico on June 18, 1972.
NOAA · Public domain

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Through Cuba, Atlantic Ocean and Atmospheric pressure

Though it moved slowly across the Yucatán Peninsula, the damage Agnes caused in Mexico is unknown. Although the storm bypassed the tip of Cuba, heavy rainfall occurred, killing seven people. In Florida, Agnes caused a significant tornado outbreak, with at least 26 confirmed twisters, two of which were spawned in Georgia. The tornadoes and two initially unconfirmed tornadoes in Florida alone resulted in over $4.5 million (1972 USD) in damage and six fatalities. At least 2,082 structures in Florida suffered either major damage or were destroyed. About 1,355 other dwellings experienced minor losses. Though Agnes made landfall as a hurricane, no hurricane-force winds were reported. Along the coast abnormally high tides resulted in extensive damage, especially between Apalachicola and Cedar Key. Light to moderate rainfall was reported in Florida, though no significant flooding occurred. In Georgia, damage was limited to two tornadoes, which caused approximately $275,000 in losses. Minimal effects were also recorded in Alabama, Connecticut, Delaware, Rhode Island, South Carolina, and Tennessee; though one fatality was reported in Delaware. The most significant effects, by far, occurred in Pennsylvania, mostly due to intense flooding. The tropical storm severely flooded the Susquehanna River and the Lackawanna River, causing major damage to the Wilkes-Barre/Scranton metropolitan area. In both Pennsylvania and New Jersey combined, about 43,594 structures were either destroyed or significantly damaged. In Canada, a mobile home was toppled, killing two people.

Agnes was the costliest hurricane to hit the United States at the time, causing an estimated $2.1 billion in damage. The hurricane's death toll was 128. The effects of Agnes were widespread, from the Caribbean to Canada, with much of the east coast of the United States affected. Damage was heaviest in Pennsylvania, where Agnes was the state's wettest tropical cyclone. Due to the significant effects, the name Agnes was retired in the spring of 1973.

Meteorological history

In early-mid June 1972, atmospheric conditions favored tropical cyclogenesis in the Caribbean Sea. Banded convection developed in the northwestern Caribbean Sea by June 11, though the system did not significantly organize. After an upper trough moved east, wind shear decreased, causing lower atmospheric pressures observations in Cozumel, Quintana Roo, Mexico. It is estimated that a tropical depression developed by 1200 UTC on June 14, while centered over the Yucatán Peninsula, about 78 miles (126 km) southeast of Mérida, Yucatán. The depression tracked eastward and entered the western Caribbean Sea on June 15. Operationally, the National Hurricane Center did not initiate advisories on the depression until 1500 UTC on June 15. Early on June 16 at 0000 UTC, the depression strengthened into Tropical Storm Agnes. However, the depression was not operationally upgraded until sixteen hours later. After becoming a tropical storm on June 16, Agnes slowly curved northward and approached the Yucatán Channel. Late on June 17, it was noted that projected path indicated the possibly of landfall in western Cuba. However, the storm remained offshore, though it closely brushed the western tip of Cuba. At 1200 UTC on June 18, Agnes intensified into a hurricane while in the southeastern Gulf of Mexico.

Prematurely, the National Hurricane Center operationally upgraded Agnes to a hurricane at 0200 UTC on that day. Upon becoming a hurricane, Agnes attained its maximum sustained winds of 85 mph (140 km/h), though it had not reached its minimum atmospheric pressure. Due to unfavorable conditions, Agnes leveled-off slightly in intensity and weakened to a minimal hurricane while approaching the Gulf Coast of the United States. Shortly before 2200 UTC on June 19, Agnes made landfall near Cape San Blas, Florida with winds of 75 mph (120 km/h). At 0000 UTC on June 20, only a few hours after moving inland, Agnes weakened to a tropical storm. After crossing the Florida/Alabama/Georgia stateline, Agnes rapidly weakened to a tropical depression. While over Georgia, the depression curved northeastward and eventually to the east-northeast after entering South Carolina. Though the storm had not dissipated, the National Hurricane Center issued its final bulletin on Agnes at 1600 UTC on June 20. By early on June 21, a large extratropical trough spawned a low pressure area, which resulted in baroclinic activity. As a result, Agnes restrengthened into a tropical storm at 1800 UTC on June 21, while centered over eastern North Carolina.

Three hours later, the National Hurricane Center noted decreasing atmospheric pressures, and indicated that winds had reached gale-force winds and once again upgraded Agnes to a tropical storm. By early on June 22, Agnes emerged into the northwestern Atlantic Ocean, where it continued to re-intensify. At 1200 UTC, Agnes reached its minimum atmospheric pressure of 977 mbar (28.9 inHg), as reported by a reconnaissance aircraft. However, maximum sustained winds were at only 70 mph (110 km/h). Late on June 22, Agnes made its final landfall on Long Beach, New York, on Long Island, with winds of 65 mph (100 km/h).

Agnes changed into an extratropical cyclone once cold air invaded its circulation late on June 22, completing its extratropical transition on the next day. The system looped across south-central Pennsylvania on June 23 and then looped across southern Ontario on June 25. It spawned a tornado in Maniwaki, Québec, early that day, which killed two and injured 11 people. The cyclone sped east-northeast, reaching Cape Breton Island on June 27 before intensifying as it re-entered the North Atlantic. After moving as far north as the 61st parallel while crossing the 25th meridian west on the morning of June 29, Agnes turned southeastward. Its central pressure bottomed out near 980 millibars (29 inHg) towards 0000 UTC on June 30. Between July 1 and July 3, the long-lived system looped between Ireland and Iceland while weakening once more. The system turned northeast, strengthening one more time while accelerating across the Hebrides on July 4 through 5. A stronger system moving in from the west finally absorbed Agnes on July 6, while located to the southeast of Iceland.

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