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This dust-driven cooling, though, is patchy—and in some places it may not even be helpful. Dust that cools a desert can change local airflow patterns and lessen the amount of rain that falls in surrounding areas. This causes plants to die, and provides more opportunities for wildfires, increasing the atmospheric carbon-dioxide level.
To get a better sense of the net effects brought about by the ups and downs of dust, it would help to have a detailed historical record of the dustiness of the planet. And this is what Natalie Mahowald of Cornell University and 19 colleagues have achieved. They analysed cores from glaciers, lake bottoms and coral reefs and measured how the levels of some telltale chemicals changed with depth, and thus with time. They then used models of global wind circulation to deduce which dust sources have become stronger and which weaker. Their conclusion, published recently in Atmospheric Chemistry and Physics, is that in fits and starts over the past century the air became twice as dusty.
Part of the increase stems from human activities—directly, in the case of construction, or indirectly, when it results from clearing vegetation from marginal land in order to farm it. Another part of the explanation may be global warming itself, shifting the boundaries of deserts and intensifying dust production in some areas.
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