The effects of the 1919 Florida Keys hurricane in Texas were the deadliest of any tropical cyclone in the Texas Coastal Bend, killing at least 284 people. The hurricane produced a widespread swath of devastation across the region, exacerbated by the large extent of its winds. The city of Corpus Christi bore the brunt of the hurricane's impacts, contributing to the largest portion of the damage toll in Texas; nearly all of the confirmed fatalities were residents of the city. The storm originated from the Leeward Islands early in September 1919 and took a generally west-northwestward course, devastating the Florida Keys en route to the Gulf of Mexico. On the afternoon of September 14, the center of the hurricane made landfall upon the Texas coast at Baffin Bay. The storm's winds were estimated at at landfall, making it a Category 3 hurricane on the Saffir–Simpson hurricane wind scale. After slowly moving ashore, it weakened and straddled the Rio Grande before dissipating on September 16 over West Texas.

Background

Between its establishment in 1839 and the hurricane of 1919, the city of Corpus Christi, Texas, had developed into a major regional port, bolstered heavily during the Gilded Age by the connection of a railway to the city following investments by wealthy South Texas businessmen Richard King and Mifflin Kenedy. There were over 200 buildings between Corpus Christi Bay and Nueces Bay by 1919, with a burgeoning network of railways linking the city to inland locales. Among Texas ports, Corpus Christi trailed only Galveston by total commercial volume; the Corpus Christi Caller, a Corpus Christi newspaper, considered Galveston a rival port city and often derided it in print. In the four years prior to 1919, two Category 4 hurricanes threatened Corpus Christi, but struck elsewhere along the Texas coast; the first made landfall near Galveston in August 1915 while the second moved ashore near Baffin Bay in August 1916. In response to these two near-misses, the Caller published a headline stating that "[Corpus Christi] is Practically Storm Proof." While a seawall was erected in Galveston following a devastating hurricane in 1900, civic leaders did not believe such a structure was necessary for Corpus Christi; the Caller surmised in a July 1901 article that "such a tidal wave and destruction of life and property as occurred at Galveston September 8, 1900, is an utter impossibility." Some residents of the city believed that the outlying barrier islands sufficiently protected the city from storm surge. George Reeder, the bureau chief of the Corpus Christi division of the United States Weather Bureau, penned an article in the Caller in 1900, testifying to the immunity of the city from tropical storms by virtue of Corpus Christi's location, topography, and barrier islands. Brochures from the Texas Mexican Railway described Corpus Christi as "the only coast city of the Gulf of Mexico, between Veracruz and Florida, that is absolutely secure against inundation." Other publications also asserted Corpus Christi's invulnerability using similar arguments.

One of the highest priorities of the Corpus Christi government in the years leading up to the 1919 hurricane was to establish a deep-water port; maritime commerce had been hamstrung by the inability of large ships to enter the Corpus Christi Bay. U.S. Representative John Nance Garner brought forth a proposal to the Army Corps of Engineers to survey and dredge a channel from Aransas Pass to Corpus Christi's wharves. A bayfront improvement plan was developed to meet government mandates for protection of the city's populace in order to proceed with the deep-water port's development, including a possible seawall. However, the high costs involved and political divisions prevented the project from proceeding promptly; by August 1919, only property valuation of lands near the proposed seawall had been conducted.

The 1919 hurricane began as a tropical depression over the Leeward Islands on September 2, 1919. It traveled on a west-northwestward path, crossing the Mona Passage as a tropical storm before intensifying into a hurricane. The U.S. Weather Bureau did not anticipate its eventual track into the Gulf of Mexico. However, the Azores High, a steering influence on tropical cyclones, was unusually expansive in the summer of 1919. This caused the hurricane to track west across the Bahamas, towards the Florida Straits, and eventually into the Gulf of Mexico. It struck the Dry Tortugas of Florida on September 10 with maximum sustained winds of , ranking it as a Category 4 hurricane on the modern-day Saffir–Simpson scale. At Key West, Florida, the storm likely damaged all structures; property loss there was estimated at $2 million. The storm was particularly impactful at sea: the Spanish steamship Valbanera, with 488 passengers and crew, and the Ward Line steamship Corydon, with 37 crew, sank in the hurricane's wrath. In total, the storm sank at least 10 large ships and 25 smaller vessels between the Bahamas and Texas. With the storm bearing down on South Florida, Major Allen Buell of the Weather Bureau predicted that San Antonio, Texas, would not experience any inclement effects.

Due to a lack of weather observations over the Gulf of Mexico, the Weather Bureau had difficulty locating and forecasting the hurricane as it approached Texas. H. C. Frankenfield, a supervising forecaster with the bureau, would later write in the Monthly Weather Review that it was "absolutely impossible to forecast the intensity and progress of the storm, and the coast stations, far from the center of the storm, afforded but meager information." Bulletins from the regional Weather Bureau center in New Orleans, Louisiana, conveyed these uncertainties as the hurricane traversed the gulf. Storm warnings were issued for the coast of East Texas between Port Arthur and Corpus Christi by the agency on September 11, but were discontinued after the Weather Bureau erroneously suspected that the storm made landfall in Louisiana and Mississippi. Acknowledging that knowledge of the storm's location was "conjectural", the Weather Bureau transmitted the following message to telegraph offices along the coast:

Despite showers reaching the Texas Coastal Bend on September 12, Corpus Christi officials ordered the lowering of storm warning flags along the city's beaches and wharves the following day. With the storm appearing to have passed harmlessly, residents were outdoors enjoying the cool northerly winds afforded by the nearby hurricane. At Galveston, the night sky was clear and tides were normal, albeit suffused with heavy surf. The air pressure at Galveston and Port Arthur rose on September 12; this temporary rise was later attributed to an area of high pressure moving southeast across the region. The next day, the Weather Bureau stated that the hurricane would be smaller and weaker than the 1916 Texas hurricane, with winds forecast to reach . However, on September 13 the northerly winds in Corpus Christi became increasingly violent and coastal swells became indicative of an approaching storm surge. Observations taken along the Texas coast on the afternoon of September 13 documented a gradual decrease in air pressure, with Galveston also reporting an increase in ocean swells. The Houston Weather Bureau office relayed a message to Corpus Christi locating the storm south of Galveston, Texas, and urging the Corpus Christi Weather Bureau to monitor the air pressure and to "take all possible precautions against rising winds and higher tides" if the pressure were to fall. Hurricane warnings were reinstated on September 14 as the storm's effects continued to escalate along the Texas coast. The hurricane made landfall south of Corpus Christi that afternoon with sustained winds of and an air pressure of 950 mbar (hPa; 28.05 inHg).

Preparations Falling pressures in Houston—indicative of the storm's proximity—prompted an evacuation of railroad cars from Galveston Island to the mainland via the use of switch engines on September 12. These cars carried some 3 million bushels of grain along with other perishable cargo.p. 1 p. 2 Ships at the Port of Galveston remained at port with the storm looming to the east. Galveston residents concurrently took refuge at hotels in Houston, with interurban service allotting additional cars hourly to facilitate their evacuation. At 10:30 a.m. CDT on September 14, Charles Heckathorn, a meteorologist for Corpus Christi's Weather Bureau office, issued a warning to "direct people in exposed places to seek places of safety." City police dispatched messengers to disseminate this alert for residents north of Corpus Christi. However, not every resident received warning; communications to Incarnate Word were disrupted before warnings could be delivered. People began to flee their homes in earnest as the sea began to rise and inundate dry ground ahead of the hurricane's arrival.

Impact The 1919 hurricane caused at least $20 million in damage and 284 deaths in Texas. The official death total only incorporated bodies that could be identified; many of those who perished in Nueces Bay were covered in crude oil following breaches of oil tanks at Port Aransas and could not be identified. According to the National Weather Service office in Corpus Christi, as many as 600–1000 people may have been killed. A relief committee organized in Corpus Christi after the storm reported over 400 fatalities and over 100 missing. However, the Caller downplayed the city's death toll to bolster the city's appeal for the development of a deep-water port. The storm produced an extended swath of rainfall over much of South and West Texas. Rainfall totals of at least spanned westward towards the Pecos River valley into Hudspeth County and northward into the Texas Panhandle towards the Oklahoma border. Between September 14–16, several cities set 24-hour rainfall records; single-day totals reached as high as in George West on September 15. Throughout the state in September 1919, 80 weather stations recorded a 24-hour period with more than of rain.

Southeast Texas

The hurricane caused approximately $272,000 in damage within the Galveston district of the U.S. Weather Bureau. Along the Texas coast from Matagorda Bay to the Texas border with Louisiana, storm surge heights ranged from at Orange to at Port O'Connor, where some homes were wrecked by heavy seas; damage in Port O'Connor and Seadrift amounted to $40,000. Sabine Pass along the Louisiana border experienced an surge. "A few buildings" were destroyed in Seabrook along the coast of Galveston Bay, with total property damage valued at $2,000. A bulkhead in Trinity Bay off Anahuac was damaged, but Anahuac itself suffered little damage from a storm tide due to its elevated position relative to the bay. Washouts occurred on segments of the Gulf and Interstate Railroad near Caplen, causing an estimated $20,000 in damage.