A massive dust storm, or haboob, swept across the Sahara Desert from western Algeria into Mauritania, Morocco, Western Sahara and the Canary Islands on March 30. The dust stretched for more than 1,000 miles.
As meteorologists observed the dust storm from space via weather satellites, social media users captured the incoming dust storm on camera. One video shows a thick wall of dust and sand moving toward a resident of the town of Tindouf, near the Mauritanian, Western Saharan and Moroccan borders.
How does the dust affect tropical storms in the Atlantic?
While this storm didn't make it too far off the coast, significant amounts of dust can drift westward from Africa across the Atlantic beginning in May. This can inhibit tropical storm formation, or the strengthening of an existing system, because the dusty air has about 50% less moisture than the typical tropical atmosphere.
Strong winds in the dust layer can also substantially increase the vertical wind shear in and around the storm environment, potentially disrupting any storm that forms.
LATEST POSTS
- 1
Russia’s New KVS Drone May Be Designed To Restore Reach In The FPV War - 2
Watch interstellar comet 3I/ATLAS speed away from the sun in free telescope livestream on Nov. 16 - 3
Journalists killed by Israeli strike in southern Lebanon - 4
Favored Vehicle for Seniors: Make Your Determination - 5
Creative Style: 10 Architects Reclassifying the Business
Two reportedly killed as Israel attacks Hezbollah targets in Lebanon
Warming winters lead to more nitrate pollution in the drinking water near farms
6 Arranging Administrations to Change Your Open air Space
The most effective method to Alter Your Kona SUV for Greatest Solace and Comfort
First stop, the Moon. Next stop, Mars? Why Nasa's mission matters
Dozens killed as Angola flood death toll rises
Finding the Universe of Craftsmanship: Individual Encounters in Imagination
What you need to know about flu treatments as cases spike across the US
Bolsonaro discharged from hospital and placed under house arrest













