a subtropical storm on January 18. It dissipated about five days later. However, the next tropical cyclone, an unnumbered depression, did not develop until June 21. In July, there were two systems, including an unnumbered tropical depression and Tropical Storm Amelia. Seven tropical cyclones formed in August, including Tropical Depression Four, tropical storms Bess and Debra and hurricanes Cora and Ella. There were also seven systems in September – tropical depressions Eight, Nine, and Twelve, Tropical Storm Hope, and hurricanes Flossie and Greta. During the month of October, there were five tropical cyclones, with two unnumbered tropical depressions, tropical storms Irma and Juliet, and Hurricane Kendra. There was another unnumbered tropical depression in November, which dissipated on November 5. The season's activity was reflected with an accumulated cyclone energy (ACE) rating of 63. 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. Systems Subtropical Storm One In the middle of January, an upper-level trough in the westerlies spawned a surface low-pressure area to the east-northeast of the Lesser Antilles and to the south of a subtropical ridge. Isolated from the detrimental effects of the westerlies, it was initially non-tropical in nature and intensified through a baroclinic energy source, or one that derives energy from the interaction of cold and warm air. Convection increased slightly despite cool sea surface temperatures of around . At 1200 UTC on January 18, it organized into a subtropical depression about east-northeast of Puerto Rico while moving in a general westward track, which it would maintain for much of its duration. The National Hurricane Center (NHC) initiated Dvorak classifications on the cyclone at 0000 UTC on January 19, assessing a Dvorak number of T2.5, suggesting both tropical and subtropical characteristics. On the same day, the pressure gradient between the storm and the ridge produced gale-force winds. By early on January 20, the storm maintained minimal convection near its center, with its primary rainband revolved in a cyclonic formation around its well-defined center. Later that day, the storm strengthened into a subtropical storm and attained peak winds of , supported by