and storm-force winds were only recorded over a small area on the Texas coastline. The storm produced minor rainfall over south Texas with Brownsville recording and Corpus Christi recording 0.95 in (24.1 in). Winds up to were reported in Brownsville around 1 am CST (0800 UTC) on September 7. Tropical depression In late September, a low-pressure area detached from a dissipating frontal system and gradually organized into a tropical system over warm sea surface temperatures in the central Atlantic. A tropical depression formed by late on September 29. However, the depression transitioned into an extratropical cyclone on October 1 as it merged with another frontal system. Tropical Storm Four A tropical depression developed near the Yucatan Peninsula early on November 27. The depression drifted southeastward and gradually strengthened into a tropical storm. Once in the gulf, it accelerated and intensified to winds of . Early on December 1, the storm made landfall near Fort Myers, Florida, at the same intensity. The system weakened and soon became extratropical. The extratropical cyclone emerged over the eastern Atlantic several hours later and regained hurricane-force winds. By 0000 UTC, the extratropical system peaked with winds of and a minimum pressure of . Around this time, the U. S. S. Patoka, which was in the vicinity of the storm, recorded a pressure of . The northeastward movement slowed shortly after crossing Florida. Around 2300 UTC, it made landfall between Wilmington and Cape Hatteras with winds equivalent to a minimal hurricane. Shortly after landfall, maximum sustained winds in the storm dropped below . A strong area of high pressure located over the Canadian Maritimes caused the system to turn east-southeastward. On December 5, the storm weakened further to the equivalent of a tropical depression as the system began to move towards the south. The remnants of the storm continued eastward, passing several hundred miles north of Bermuda later that day. The cyclone was reported near the Azores on December 9, before finally merging with another cyclone over the North Atlantic. The storm caused significant property and crop damage along the Gulf Coast of Florida. Trees, power lines, and telegraph wires were uprooted or knocked down by high winds along the Suwannee River. Structures which were previously considered to be safe from storms, being over inland, sustained significant damage from what was likely storm surge. The beaches along the Atlantic coast also sustained considerable damages from the