Tropical Storm Andrea was a short-lived weather system in the central Atlantic, spanning from June 23 to June 24. The National Hurricane Center (NHC) began observing a trough of low pressure on June 22, located east-southeast of Bermuda. This low pressure was on a weakening stationary front, but it exhibited signs of increased deep convection and organization. As a result, a tropical depression formed early on June 23, approximately 490 miles east of Bermuda. By noon the same day, Andrea reached its peak intensity with maximum sustained winds of 40 mph. Due to the high-pressure environment surrounding Andrea, it had an unusually high central pressure for a tropical storm, recorded at 1014 mbar.
Despite its short lifespan, Andrea showcased typical characteristics of a tropical storm but failed to intensify significantly. The deep convection that initially characterized the storm collapsed by the afternoon of June 24. By 6 PM UTC on June 24, Andrea had transitioned into an extratropical low, effectively marking the end of its tropical phase. The storm fully dissipated by the following day, June 25. Overall, Andrea's development, dissipation, and relatively high central pressure underscore the complexities of tropical systems, particularly in their formation and progression within different environmental conditions.