A tropical wave moved off the African coast on August 16th and traveled westward across theAtlantic Ocean. As it neared the Caribbean Sea, the track became more west-northwest. On the23rd, it moved under an upper-level cold low. By the 27th, the associated weather moved north of the upper cyclone, which had spread across the Bahamas and Florida. On the 28th, the disturbance moved into the eastern Gulf of Mexico, and organized into a tropical depression on the 29th about 200 nautical miles south-southwest of New Orleans, a tropical storm on the morning of the 30th,and a hurricane that night. Its track was west-southwest through much of the Gulf of Mexico with some minor fluctuations in track, until Anita made landfall as a strong category 4 urricane along the coast of east-central Mexico 80 nautical miles north of Tampico, Mexico near the town of Soto La Marina around dawn on September 2nd, which received 15.20″ of rain. The system emerged into the eastern Pacific and was redesignated Tropical Depression 11. The depression moved quickly westward and dissipated after passing south of Baja California on the 4th.

The graphics below show the storm total rainfall for Anita. Rainfall information from the United States was obtained from the National Climatic Data enter. Rainfall information from Mexico was obtained from the Comision Nacional del Agua, the parent agency of their national weather service. Note the maxima lie on either side of its track across northeast Mexico.

<<Retired Hurricane

Hurricane Andrew was a small but powerful storm that caused massive destruction along a path through southern Florida and south-central Louisiana in late August 1992. Rainfall associated with Andrew was light for a hurricane because of the small size and rapid forward movement of the storm. However, rainfall totals of more than 7 inches were recorded for the storm period in southeastern Florida and Louisiana; a high of 11.9 inches was recorded in Hammond, La. (Rappaport, 1992). Maximum sustained windspeeds of 141 mph (miles per hour), with gusts of 169 mph, were recorded on August 24, just before landfall in Florida (Rappaport, 1992). A storm surge of about 17 feet above sea level was recorded at Biscayne Bay, Fla. and about 9 feet near Terrebonne Bay in south-central Louisiana.

Hurricane Andrew originated in the North Atlantic Ocean,moved westward over the Bahamas, and made landfall near the southern tip of Florida on the morning of August 24. After passing over the Florida Everglades, the storm proceeded in a northwesterly direction across the Gulf of Mexico and made landfall in south-central Louisiana at Point Chevreuil on the morning of August 26. Andrew deteriorated rapidly after landfall in Louisiana and was downgraded to a tropical depression on August 27. The remnants of Andrew proceeded on a northeasterly path, producing severe weather throughout the Southeastern States (Rappaport, 1992).

Hurricane Andrew moved across southern Florida at an average forward speed of 18 mph (National Oceanic and Atmospheric Administration, 1992). As it crossed southern Florida, Andrew left a path of destruction 25 miles wide and 60 miles long (Gore, 1993).

<<Retired Hurricane