Millions of people across the northern Gulf Coast braced Tuesday for a rare winter storm that’s expected to scatter heavy snow, sleet and freezing rain around the Deep South as a blast of Arctic air plunges much of the eastern U.S. into a deep freeze.

A winter storm dumped snow from Texas into Louisiana, Mississippi, Alabama and even Florida Tuesday. More of the South is up next.

A historic winter storm is expected to bring rare heavy snowfall and ice to states along the Gulf Coast and could impact as many as 55 million people through midweek, according to national

A significant portion of I-10 is closed in both directions in Louisiana west of Baton Rouge to the Texas border.

As Florida faces an intense cold snap, complete with freeze warnings and cold-weather advisories, one unique hazard stands out—falling iguanas.

Snow totals in Louisiana have broken records. Parts of Florida, Texas and Georgia have also accumulated several inches of snow.

The first-ever blizzard warning has been issued for parts of the Texas and Louisiana coast as a historic snowstorm hits the South. One hypothermia-related death has been reported in Georgia, according to James Stallings,

Millions of people living along the Gulf Coast and into the Southeast are bracing for a rare, significant winter storm that’s expected to significantly impact travel and lead to power outages due to heavy snow and ice starting Monday evening.

A winter storm pummeled the southern United States with ice and snow Tuesday. Here's how much snow fell in Florida, Texas, Alabama and more.

As heavy snow, sleet and freezing rain hit parts of the Deep South, a blast of Arctic air plunged much of the Midwest and the eastern U.S. into a deep freeze.

according to meteorologist Hayley Adams at the NWS in Houston. Florida state offices in the affected counties closed at 1 p.m., with offices closing even earlier in Pensacola. All non-essential ...

Winter Storm Enzo was not your typical winter storm, but its rain and snow were caused by a classic setup. Enzo never truly had a robust low pressure system, but instead was a large overlap between the coldest air of the season, abundant moisture and the tail end of a deep upper-level trough.