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Warmer ocean temperatures may decrease Saharan dust crossing the Atlantic

By Lara Streiff/ NASA’s Earth Science News Team

Every year, millions of tons of dust from the Sahara Desert are swirled up into the atmosphere by easterly trade winds and carried across the Atlantic. The plumes can make their way from the African continent as far as the Amazon rainforest, where they fertilize plant life. New research suggests that, as the climate changes and oceans continue to warm, dust transport will shrink to a 20,000-year minimum within the next century.

With projected global warming, NASA researchers’ data indicate at least a 30% reduction in Saharan dust activity from current levels over the next 20 to 50 years, and a continued decline beyond that. Dust plays a major role in the Earth system. A decrease of dust as the climate warms may have profound influences on a variety of phenomena, but these potential impacts may be good or bad, say the researchers.

Orbital view of Earth with wide tan streak reaching from Africa out across the cloud-spotted blue Atlantic ocean.

Satellite image of the July 2020 “Godzilla” dust plume. Image via NASA.

During 2020, global average surface temperatures were the hottest on record, tying with 2016 as the warmest recorded year. Last year was also the most active hurricane season on record, with many storms quickly intensifying. The warming climate influences all of our planet’s interacting temperature and weather systems, including the global transport of massive dust plumes from one continent to another.

In June 2020, a Godzilla dust plume traveled from the Sahara, the planet’s largest, hottest desert, across the Atlantic Ocean to North America. While this eye-catching plume made headlines, NASA scientists, using a combination of satellite data and computer models, predict that Africa’s annual dust plumes will actually shrink to a 20,000-year minimum over the next century as a result of climate change and ocean warming.

The Sahara Desert is 3,600,000 square miles (9,200,000 square km) of arid land stretched across the northern half of Africa, slightly smaller in size than the continental United States. Upwards of 60 million tons of its nutrient-laden mineral dust are lifted into the atmosphere each year, creating a massive layer of hot, dusty air that winds carry across the Atlantic to deliver those nutrients to the ocean and vegetation in South America and the Caribbean.

Recent NASA research outlines the domino-like connections between factors beyond the desert’s borders and the development of dust plumes. These start with temperature differences between the North and South Atlantic, which then impact the region’s consistent east to west winds as well as a tropical band of relatively high rainfall located near the equator, both of which impact the annual dust plumes. Supported by NASA’s Modeling, Analysis, and Prediction (MAP) Program and Radiation Sciences Program, the scientists used their new understanding of these relationships to forecast a more substantial reduction in dust activity than previous studies had predicted based on anticipated climate warming.

Recent dust estimates are derived from data collected by NASA satellite missions. Tianle Yuan is an atmospheric scientist at NASA’s Goddard Space Flight Center in Greenbelt, Maryland. He said:

From ground observations and satellite observations, we see African dust variability. In fact, it can change quite a bit, from month to month, day to day, year to year, even decade to decade.

The researchers were also interested in seeing if the relationship between global average temperature and Saharan dust activity occurred in the past. Geological records going back thousands of years help reveal past precipitation and nutrient levels as the Sahara went through dramatic environmental shifts.

The peak of Saharan dust transport to the eastern side of the Americas took place roughly between 12,000 to 17,000 years ago, at the end of the last Ice Age. Then began the African Humid Period, during which the vast expanse of desert was speckled with lakes, vegetation and human habitation. The increased moisture and plant life stabilized the ground and minimized dust plumes. North African sediment cores off the coast and pollen records show that there was more rainfall and vegetation present. Yuan said:

The Sahara Desert was relatively wet back then. Dust was much rarer.

Though dust transport has increased since then, the research team found that both natural processes and human activity are now likely driving Earth back toward a dust minimum as climate warms.

Sea surface temperatures directly impact wind speeds, so when the northern Atlantic warms relative to the South Atlantic, the trade winds that blow the dust from east to west become weaker. As a result, the slower winds pick up and transport less dust from the Sahara.

In addition to carrying less dust, the weakened winds also allow the band of steady rain that traverses the tropics to drift north over more of the desert, which dampens the dust and keeps it from getting swept away. Less dust in the air, which can reflect sunshine away from Earth’s surface like a sunshield, means more sunlight and heat reach the ocean, warming it further. All together this creates a feedback loop of warm sea surface temperatures leading to reduced dust, and reduced dust in turn contributing to additional warming, combining to impact climate, air quality, and storm and hurricane formation.

Hongbin Yu is an atmospheric researcher at NASA Goddard Space Flight Center. He said:

Dust plays a major role in the Earth system. A decrease of dust as the climate warms may have profound influences on a variety of phenomena, but these potential impacts may be good or bad.

On its journey across the Atlantic, Saharan dust sprinkles into the ocean, feeding the marine life, and similarly plant life once it makes landfall. Minerals like iron and phosphorus in the dust act as a fertilizer for the Amazon rainforest, Earth’s largest and most biodiverse tropical forest. Rains wash many of these valuable nutrients from the soil into the Amazon river basin, making the nutrient delivery from Africa important for maintaining healthy vegetation.

Though African dust transport plays an important role in the genesis of soils and sustaining vegetation, Yu says there are some negative effects because the increase in nutrients can lead to harmful algal blooms off the coast of Florida, and coral reef sicknesses and death linked to dust deposition.

Residents in the Caribbean could also see some benefits as less dust means better air quality. Breathing in dust is particularly hazardous for children, the elderly, and those with respiratory conditions such as asthma.

Yuan said:

The final piece of the story is looking to the future. We want to know what the Sahara dust will be, given the climate change picture we are painting. But directly predicting dust activity is really hard because it involves a lot of processes.

With projected global warming, the research team used model data from the Coupled Model Intercomparison Project 5 (CMIP5) that indicate at least a 30% reduction in Saharan dust activity from current levels over the next 20 to 50 years, and a continued decline beyond that. Yuan said:

The minimum humans experienced during the African Humid Period will likely be surpassed because of climate change. As the plumes of dust decline, so will their impacts on vegetation an ocean away.

Bottom line: Research by NASA scientists suggests that warmer ocean temperatures will decrease Saharan dust crossing the Atlantic.

Source: Anthropogenic Decline of African Dust: Insights From the Holocene Records and Beyond

Source: Understanding processes that control dust spatial distributions with global climate models and satellite observations

Via NASA

Eleanor Imster

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