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
Manual for Tracking down Spending plan Agreeable Travel Objections - 2
Islamic State group militants claim capture and execution of a Nigerian brigadier general - 3
Spotify Wrapped and Apple Music Replay are here: Top songs, albums and artists of 2025 - 4
Bestselling author Colleen Hoover reveals cancer journey - 5
Foreign journalist kidnapped in Iraq: Interior Ministry
European nations criticise Israel’s death penalty plans
Israel Police decry online defamation campaign against female officer in Jerusalem
Early Thanksgiving week forecast: Where Americans can expect cold, rain and snow for the holiday
Pfizer says patient dies after receiving hemophilia drug in trial
Scientists are getting our robotic explorers ready to help send humans to Mars
Manual for 6 Hot Brilliant Beds
This Huge Ocean Beast Shifts Sharks’ Evolutionary Timeline
Proficient Cultivating Devices for a Lovely and Useful Nursery in 2024
A definitive Manual for the 5 Off-road Bicycles Available











