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ON MAY 26th 2008 Germany turned red. The winds of change, though, were meteorological, not political. Unusual weather brought iron-rich dust from Africa to Europe, not only altering the colour of roofs and cars on the continent but also, according to recent calculations by Max Bangert, a graduate student at the Karlsruhe Institute of Technology, making the place about a quarter of a degree colder for as long as the dust stayed in the air.
Unusual for Germany commonplace for the planet as a whole. The Sahara and other bone-dry places continually send dust up into the atmosphere, where it may travel thousands of kilometres and influence regional weather, the global climate and even the growth of forests halfway around the planet.
Earlier in 2008, for instance, Ilan Koren and his colleagues at the Weizmann Institute of Science, in Israel, detected a particularly voluminous burst of dust from the Bodélé Depression. This low-lying bed of silt in Chad, across which powerful jets of wind are wont to blow, constitutes less than 1% of the Sahara¡¯s area but is reckoned the world¡¯s dustiest place. It is thought to be responsible for a quarter or more of the Sahara¡¯s output of airborne dust.
Dr Koren observed the dust rise with a camera on a satellite called Aqua watched it obscure the sun using an automated photometer in Ilorin, Nigeria followed it across the Atlantic with another satellite, CALIPSO and finally saw a spike in levels of silicon, aluminium and iron as it landed on detectors in Manaus, Brazil. His results, presented at a meeting of the American Geophysical Union held in San Francisco in December, provide a remarkable account of the intercontinental transfer of dust.
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