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
Experience Is standing by: History's Most noteworthy Travelers - 2
Figure out How to Plan for Your Web-based Degree monetarily - 3
Kids may be more likely to get the new ‘Cicada’ variant of Covid-19, scientists say. Here’s what to know about BA.3.2 - 4
Are protests pushing Iran's Islamic regime toward a tipping point? - 5
Vote in favor of Your Number one Smartwatch: Exactness and Style Matter
Vote In favor of Your Favored Sort Of Bevarage
Why some African countries are prone to military takeovers
4 astronauts are now on their path to the moon. Here’s what happens next
Lebanese Shi’a party Amal competing, coordinating with Hezbollah, experts tell ‘Post’
‘Aid for Ukraine’ pierogi fundraiser event
The Following Huge Thing: 5 Progressive Tech New businesses
Investigating Remarkable Espresso Flavors: Upgrade Your Day to day Blend
China Just Got A Lot Closer To Its First-Ever Manned Moon Landing
'Weezer: The Gathering' 2026 tour: How to get tickets, prices, dates and more












