The 1902 Atlantic hurricane season featured five known tropical cyclones, three of which made landfall in the United States. The first system was initially observed in the northwestern Caribbean on June 12. The last system dissipated on November 6 while located well southeast of Newfoundland. These dates fall within the period with the most tropical cyclone activity in the Atlantic. None of the systems existed simultaneously. Of the season's five tropical cyclones, three reached hurricane status. However, none of them strengthened into major hurricanes, which are Category 3 or higher on the modern-day Saffir–Simpson hurricane wind scale. Along with 1901, this was the first time that two consecutive seasons lacked a major hurricane since 1864 and 1865. Only one storm left significant impact, which was the second hurricane. It brought flooding and strong winds to Texas, resulting in severe damage in some areas. A tornado spawned by the storm also caused five fatalities. The season's activity was reflected with an accumulated cyclone energy (ACE) rating of 28, the lowest value since 1890. ACE is a metric used to express the energy used by a tropical cyclone during its lifetime. Therefore, a storm with a longer duration will have high values of ACE. It is only calculated at six-hour increments in which specific tropical and subtropical systems are either at or above sustained wind speeds of 39 mph (63 km/h), which is the threshold for tropical storm intensity. Thus, tropical depressions are not included here. Timeline Systems Tropical Storm One In June, a low-pressure area was observed over the western Caribbean. At 12:00 UTC on June 12, a tropical depression developed about north of Swan Island, Honduras. The depression moved north-northeastward and intensified into a tropical storm early the next day. Later on June 13, the storm made landfall in modern-day Artemisa Province of Cuba with winds of . After reaching the Gulf of Mexico late on June 13, the system continued to strengthen and peaked with maximum sustained winds of . Around 23:00 UTC, it made landfall near Steinhatchee, Florida, at the same intensity. After moving inland, the storm moved northeastward and slowly weakened. Around midday on June 16, the system became extratropical over southeastern Virginia and then accelerated northeastward, before dissipating near Anticosti Island, Quebec, late on the following day. Some locations in Florida observed tropical storm force winds. In Virginia, the steamer Falcon sank southeast of False Cape.