Global InformationSaharan dust information
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Saharan dust (also African dust, yellow dust, yellow sand, yellow wind or Sahara dust storms) is an aeolian mineral dust from the Sahara desert, the largest hot desert in the world. The desert spans just over 9 million square kilometers, from the Atlantic Ocean to the Red Sea, from the Mediterranean sea to the Niger River valley and the Sudan region in the south.[1]
The Sahara is the largest source of aeolian dust in the world, with annual production rates of about 400-700 x 106 tons/year, which is almost half of all aeolian desert inputs to the ocean.[2] Saharan dust is often produced by natural process such as wind storms and doesn't appear to be heavily impacted by human activities.[3]
In most cases marine bacteria and phytoplankton require small amounts of the micronutrient iron, which can be supplied by transport of Saharan dust. The dust delivered to the Atlantic Ocean and the Mediterranean Sea has a small percentage of dissolvable iron;[4] however, since so much iron is supplied to the regions, even with a low soluble percentage, Saharan dust is a large source of iron to these regions. Factors that contribute to dust solubility are particle size, the mineral composition of the dust, the temperature of the water, and its pH.[5][6] Organic molecules called ligands can also increase the solubility of iron and make it more accessible to organisms to use for primary production.[7]
Saharan dust has been found to travel to the Amazon basin, Scandinavia,[8] Japan,[9] and other regions. The dust supplied to the North Atlantic and the Mediterranean[10] brings nutrients that help to boost primary production. For the Amazon basin, which is limited in phosphorus in much of the soil in the basin, Saharan dust is a main source of phosphorus. This dust has also impacted ecosystems in the southeastern United States and the Caribbean by supplying limiting nutrients, and in some cases promoting soil development on land.[11] Saharan dust has even been found on glaciers and studied to examine atmospheric circulation.[11] Human impacts of Saharan dust can include respiratory difficulties[12][13] and other adverse health conditions during dust storms in the surrounding regions.[14]
- ^ Cook, Kerry H.; Vizy, Edward K. (2015). "Detection and Analysis of an Amplified Warming of the Sahara Desert". Journal of Climate. 28 (16): 6560. Bibcode:2015JCli...28.6560C. doi:10.1175/JCLI-D-14-00230.1.
- ^ Middleton, N. J.; Goudie, A. S. (2001). "Saharan dust: sources and trajectories". Transactions of the Institute of British Geographers. 26 (2): 165–181. doi:10.1111/1475-5661.00013. ISSN 0020-2754.
- ^ Kandler, Konrad; Benker, Nathalie; Bundke, Ulrich; Cuevas, Emilio; Ebert, Martin; Knippertz, Peter; Rodríguez, Sergio; Schütz, Lothar; Weinbruch, Stephan (2007). "Chemical composition and complex refractive index of Saharan Mineral Dust at Izaña, Tenerife (Spain) derived by electron microscopy". Atmospheric Environment. 41 (37): 8058–8074. Bibcode:2007AtmEn..41.8058K. doi:10.1016/j.atmosenv.2007.06.047.
- ^ Theodosi, C.; Markaki, Z.; Mihalopoulos, N. (2010). "Iron speciation, solubility and temporal variability in wet and dry deposition in the Eastern Mediterranean". Marine Chemistry. 120 (1–4): 100–107. Bibcode:2010MarCh.120..100T. doi:10.1016/j.marchem.2008.05.004.
- ^ Alshora, Doaa Hasan; Ibrahim, Mohamed Abbas; Alanazi, Fars Kaed (2016), "Nanotechnology from particle size reduction to enhancing aqueous solubility", Surface Chemistry of Nanobiomaterials, Elsevier, pp. 163–191, doi:10.1016/b978-0-323-42861-3.00006-6, ISBN 978-0-323-42861-3, retrieved 2020-11-07
- ^ Ravelo-Pérez, L.M.; Rodríguez, S.; Galindo, L.; García, M.I.; Alastuey, A.; López-Solano, J. (2016). "Soluble iron dust export in the high altitude Saharan Air Layer". Atmospheric Environment. 133: 49–59. Bibcode:2016AtmEn.133...49R. doi:10.1016/j.atmosenv.2016.03.030. hdl:20.500.11765/7502. ISSN 1352-2310.
- ^ Tagliabue, Alessandro; Williams, Richard G.; Rogan, Nicholas; Achterberg, Eric P.; Boyd, Philip W. (2014-10-28). "A ventilation-based framework to explain the regeneration-scavenging balance of iron in the ocean: Dissolved Iron Framework". Geophysical Research Letters. 41 (20): 7227–7236. doi:10.1002/2014GL061066.
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:25was invoked but never defined (see the help page). - ^ a b Aarons, S.M.; Aciego, S.M.; Gleason, J.D. (2013). "Variable HfSrNd radiogenic isotopic compositions in a Saharan dust storm over the Atlantic: Implications for dust flux to oceans, ice sheets and the terrestrial biosphere". Chemical Geology. 349–350: 18–26. Bibcode:2013ChGeo.349...18A. doi:10.1016/j.chemgeo.2013.04.010. hdl:2027.42/98095.
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