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The 1913 Atlantic hurricane season was the third consecutive year with a tropical cyclone developing before June. The first system, a tropical depression, developed on May&nbsp;5 while the last transitioned into an extratropical cyclone on October&nbsp;30. Of note, the seventh and eighth cyclones existed simultaneously from August&nbsp;30 to September&nbsp;4.

Of the season's ten tropical cyclones, six became tropical storms and four strengthened into hurricanes. Furthermore, none of these strengthened into a major hurricane—Category&nbsp;3 or higher on the modern-day Saffir–Simpson hurricane wind scale—marking the sixth such occurrence since 1900. 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 , which is the threshold for tropical storm intensity. Thus, tropical depressions are not included here.

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Timeline

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Systems

Hurricane One

Weather maps and ship data indicate the development of a tropical depression in the southwestern Caribbean Sea around 06:00&nbsp;UTC on June&nbsp;21. Moving north-northwestward, the depression accelerated and intensified into a tropical storm on the following day. Early on June&nbsp;23, the storm made landfall near the Honduras–Nicaragua border with winds of . Thereafter, it continued north-northwestward and oscillated slightly in strength. The system made another landfall near Cancún, Quintana Roo, with winds of late on June&nbsp;25. After briefly crossing the Yucatan Peninsula, the cyclone emerged into the Gulf of Mexico and eventually began moving more to the west-northwest. Early on June&nbsp;27, it deepened into a Category&nbsp;1 hurricane and peaked with maximum sustained winds of . The hurricane then curved northwestward and made landfall in Padre Island, Texas, at the same intensity around 01:00&nbsp;UTC on June&nbsp;28. After moving inland, the storm quickly weakened and dissipated over Val Verde County just under 24&nbsp;hours later.

Impact in Central America and Mexico is unknown. The storm brought heavy rainfall to portions of South Texas. At Montell, of precipitation fell in about 19&nbsp;hours, while Uvalde observed of rain in approximately 17&nbsp;hours. The resultant flooding caused considerable damage to lowlands, houses, and stock. Additionally, communication by telegraph and telephone were cut-off for several days and traffic was interrupted due to inundated streets. One person drowned in Montell. Strong winds were also reported, with winds of over Central Padre Island. Along the coast, storm surge peaked at in Galveston. In Farmville, a warehouse collapsed, killing two people inside while three deaths occurred elsewhere in the state. Precipitation led to minor crop damage, totaling approximately $75,000.