USA TODAY US Edition

Dust from the Sahara darkens Texas skies

- Doyle Rice

Sure, it’s always hot in Texas in July, but this week, a new ingredient from an ocean away adds to the heat misery: Plumes of dust from the Sahara Desert bring hazy skies to the Lone Star State.

“The haze is due to dust from the Sahara Desert being blown thousands of miles to the west,” AccuWeathe­r meteorolog­ist Dean DeVore said.

The National Weather Service office in Fort Worth said Monday, “The combinatio­n of the Sahara dust plume ... and pollutants within immediate urban areas is already resulting in hazy conditions across parts of the area.”

Air quality will also be a concern. “Combined with oppressive heat, the air quality will be like experienci­ng the desert itself,” tweeted meteorolog­ist Ryan Maue of weather.us.

AirNow warned that “people with heart or lung disease, older adults and children should reduce prolonged or heavy exertion.”

Temperatur­es could reach record levels this week. “This heat will reach far and wide with the majority of Texas, Oklahoma and eastern New Mexico seeing temperatur­es above 100 degrees all week,” the weather service office in Midland, Texas, said. “Many record highs could be in jeopardy.”

Night will not offer much relief from the oppressive conditions as overnight lows dip only into the middle 70s to lower 80s, AccuWeathe­r said.

Hundreds of millions of tons of soil are lifted from the Sahara every year, the National Oceanic and Atmospheri­c Administra­tion said. This recent event is on the larger side.

Dust from Africa is more common in the Caribbean islands, but occasional­ly, it can make its way into Mexico and parts of the Florida Peninsula and Texas. When it’s over the Atlantic Ocean, the extremely dry, dusty air from the Sahara can prevent hurricanes from forming, NASA said.

A good amount of this dust can trace its origins back to a dry lake bed in north-central Chad, known as the Bodele depression, NOAA said.

The dust is made up of the “skeletons” of diatoms, micro-organisms that trace their origin back to when the Bodele depression was full of water. These diatoms are picked up by winds that are naturally accelerate­d through a gap in the mountains upwind of the depression.

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