Tropical Storm Carrie (1972)  Tropical Storm Carrie was a strong tropical storm that affected the East Coast of the United States in early September 1972. The third tropical cyclone of the 1972 Atlantic hurricane season, Carrie formed on August 29 from a complex sequence of meteorological events starting with the emergence of a tropical wave into the Atlantic in the middle of August. Tracking generally northward throughout its life, Carrie reached an initial peak intensity as a moderate tropical storm before nearly weakening back into tropical depression status. The storm began to reintensify in a baroclinic environment after turning toward the northwest; its winds of as it was transitioning into an extratropical system eclipsed the cyclone's previous maximum strength. The extratropical remnants of Carrie skirted eastern New England before making landfall in Maine on September 4 and dissipating over the Gulf of Saint Lawrence during the next two days. Carrie had a minimal impact on the East Coast south of New England, limited to increased swells, gusty winds, and light rainfall. The worst conditions occurred over southeastern New England, where wind gusts reached and rainfall exceeded . Damage was most severe along and slightly inland from the coast. Thousands of people became stranded on offshore islands of Massachusetts after dangerous conditions created by the storm prompted the suspension of steamship service. Overall damage was generally light, with total monetary losses valued at $1,780,000, and four deaths are blamed on the storm. The origins of Tropical Storm Carrie are traced back to a tropical wave—an elongated area of low atmospheric air pressure—that emerged from the western coast of Africa on August 15, 1972. A relatively strong weather system, the wave progressed westward, but by the time it had reached the Leeward Islands ten days later, it had degenerated substantially. The influence of a nearby upper-level low pressure system caused the disturbance to further deteriorate, and the resultant remnant circulation drifted toward the northwest; by August 28, it was situated at a position just offshore southeastern Florida. The low pressure system maintained a cold core and had not yet established itself at the surface. On August 29, the low began moving northward in response to an approaching trough. For the first time, a low-level circulation center had been identified in association with the system, and the storm became a tropical depression at 1200 UTC while located east of the central Florida peninsula. The depression tracked steadily northeastward as it gradually intensified. On August 31, reconnaissance aircraft flying into the cyclone reported maximum sustained winds of up to around .