When I was much younger, my mother would speak about “the dust from Africa” that made the sky hazy and I would dismiss it as yet another situation to blame on the so-called “Dark Continent,” but in the past few years I have found evidence that the complaint was based on science after all. Here are excerpts explaining how dust clouds from the African Sahara travels thousands of miles across the Atlantic Ocean in large quantities—and now, those particles have more than doubled.
In a recent study, Joseph Prospero, professor emeritus at the University of Miami Rosenstiel School of Marine and Atmospheric Science and collaborators at the University of Houston and Arizona State University found that the average air concentrations of inhalable particles more than doubled during a major Saharan dust intrusion in Houston, Texas. The researchers were able to distinguish between particles transported across the Atlantic and those from local sources in the Houston region. In this way they established the “fingerprint” of the African dust. To their knowledge, this is the first study that isolates, differentiates, and quantifies the air contaminants in the US during the incursion of African dust. There is a concern that the fine airborne dust particles could be a health problem for asthmatics and people with respiratory problems.
[. . .] The findings published in the journal of Environmental Science and Technology can also serve to address African dust intrusion in other affected regions of the world. For instance, the Caribbean Basin receives enormous quantities of African dust every year. In addition to its impact on air quality, an important factor for the Caribbean basin is the potential effect of Saharan air outbreaks on hurricane activity. “African dust storms are associated with hurricane season because the meteorological situations that are involved with generating tropical cyclones are also associated with the generation and transport of dust,” Prospero says. “The dust emerges from the coast of Africa in a hot, dry, elevated layer – the Saharan Air Layer (SAL) following behind Easterly Waves from which tropical cyclones sometimes develop,” he says. “The SAL interacts with the waves in complex way, so that the relationship is not entirely clear. It is the subject of much ongoing research.”
Also, the dust suspended in the wind absorbs and scatters solar radiation. Less sunlight reaches the ocean surface resulting in cooler temperatures in the tropical Atlantic Ocean, the main area where hurricanes develop. Cooler ocean temperatures mean less energy for hurricanes to form and strengthen. [. . .] “Dust activity has been very intense this year and sea surface temperatures are unusually low,” Prospero says. “These may have been contributing factors to the unusually weak hurricane season this year.”
Prospero and his collaborator from the University of Puerto Rico make practical recommendations for the creation of a cooperative project that include long-term measurements of African dust occurrences in the Caribbean Basin, in a recent study published in the journal of American Meteorological Society. The scientists hope this collaborative effort will lead to a better understanding of the range and complexity of Saharan dust storms and the impact of African dust on climate and human health.
For full article, see http://phys.org/news/2013-09-storms-africa-affect-caribbean-air.html