Marine geologist prof dr Jan-Berend Stuut investigates desert dust’s role in the Earth’s climate. ‘We have placed a large series of measuring instruments in the Atlantic Ocean between Africa and the Caribbean, which all capture dust from the Sahara. When we first found sand grains of nearly half a millimetre in size in these traps, hardly anyone believed us because they seemed to be much too large. Now we have clearly shown that these large dust particles from the Sahara can be blown to the other side of the ocean. Satellite images beautifully reveal which dry riverbeds and dried-up lake floors this dust is emitted from. Furthermore, chemical analysis of the particles provides a sort of “fingerprint” as to where the dust comes from.’
‘This finding has consequences for both the atmosphere and the ocean. Dust scatters light and heat, influences the formation of raindrops and clouds, but also subdues the development of hurricanes. Furthermore, desert dust from the Sahara is full of nutrients as well as metals like iron. It therefore acts as a fertiliser that feeds the oceans. The growth of algae, for example, benefits from this fertiliser. This makes Sahara dust an important factor in the overall balance of algal growth in the oceans and therefore in global climate. Because when those algae die, they can take the carbon they have captured to the ocean floor, and that could somewhat counterbalance the emission of CO2 from fossil-fuel burning’
‘Besides being a fertiliser, which encourages the ocean’s uptake of carbon dioxide from the atmosphere, Sahara dust can also act as a reflector high in the atmosphere, keeping the sun’s heat away from the earth’s surface. Lower in the atmosphere, however, this same dust acts as a strongly insulating blanket, just like the greenhouse gas CO2, which retains heat. Amongst other things, our research provides meteorologists and other researchers with data about the quantity and quality of dust in the air. They can subsequently study the exact relationships between dust and temperature in the atmosphere.’
‘Besides investigating the various processes in which desert dust plays a role in the current climate, we are also trying to reconstruct the climate of the past using desert dust that can be found in depositions on the seafloor. The particle size of the dust tells us something about the strength of the ambient winds in the past and the amount of dust relative to river mud tells us something about the aridity in the source areas of these materials. In addition, by studying present-day relationships between wind and wind-blown sediments, we can try and infer quantitative wind-strength reconstructions from past dust deposits.’Read more +
I study two main aspects of desert dust:
1) the depositional aspect allows me to study dust dispersal in the geologic past. Just like rivers nearly always flow to the sea and deliver sediments, winds always blow off land masses and deposit dust in the ocean. Using such marine archives of sediment deposition, I try to reconstruct past environmental conditions in dust-source regions.
2) the marine-environmental effects that dust has are most likely enormous. Desert dust contains all kinds of nutrients and metals, from which marine life can profit. In a couple of projects I am trying to answer the question if dust can be used as an artifical fertiliser for the ocean. We think that this is happening in nature, and should this be the case, we could potentially apply it as a means to combat climate change.
Much more information on dust-related studies at NIOZ can be found at the institute's dustiest website at www.nioz.nl/dust .
In addition, we are regularly publishing dusty news in the NIOZ dust-blog
Alternatively, you can find more dusty info on my personal website at: www.stuut.tv