and subtropical systems are either at or above sustained wind speeds of , which is the threshold for tropical storm intensity. Thus, tropical depressions are not included here. Systems Tropical Storm One On May 13, a tropical depression formed about south of Trinidad, Cuba. It quickly crossed the island and moved over the Straits of Florida. The cyclone strengthened to a minimal tropical storm on May 14 and soon made landfall near Key Vaca, Florida, with winds of . Around 06:00 UTC the storm struck the Florida mainland near Cape Sable and initially moved north-northwestward across the state. Based on observations from Tampa late on May 14, the storm's minimum barometric pressure is estimated at . The cyclone turned northeastward on May 15. It transitioned to an extratropical cyclone over eastern Virginia on the following day. The remnants briefly re-emerged over the Atlantic, before striking New England and dissipating over Maine on May 17. Initially, the cyclone was not included in the Atlantic hurricane database. The tropical storm ended a significant drought in Florida, producing the state's first widespread rainfall event in several months. Parched crops and vegetation were rejuvenated by the well-timed rains. Lakeland, Florida, recorded of rain in a 24-hour period. Strong, albeit non-damaging winds, were felt across the Florida coasts, with a peak gust of documented in Jacksonville. Moderate gales were produced by the storm's extratropical stages in the Mid-Atlantic states and New England. Widespread rainfall in southwestern Maine and southeastern New Hampshire from the storm's remnants peaked at in Durham, Maine, and damaged roads. The cost of damaged infrastructure in southwestern Maine was estimated at $150,000. Hurricane Two The Gulf Coast Hurricane of 1916 A tropical disturbance organized into a tropical depression over the southwestern Caribbean on June 28. Little intensification occurred for several days as the depression moved westward and eventually northwestward, brushing the coasts of Nicaragua and Honduras late on June 30 and early on July 1. The cyclone finally strengthened into a tropical storm early the next day and reached hurricane status late on July 3 as it neared the Yucatán Channel. Further intensification occurred in the Gulf of Mexico, and at around 18:00 UTC on July 5, the storm peaked as a Category 3 hurricane with maximum sustained winds of and a minimum barometric pressure of , with the latter being derived from the former. About three hours later, the hurricane made