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Atmospheric Controls on North African Dust Emission Richard Washington Sebastian Engelstaedter Martin Todd, Gil Lizcano Fiona Mitchell Yoram Kaufman, Ilan Koren Oxford, UCL, GSFC NASA,
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JANFEBMARAPRMAYJUNJULAUGSEPOCTNOVDEC Annual dust cycle of TOMS AI (1980-92)
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Washington and Todd 2005 GRL Mean JFM Zonal Wind: latitude-height along 18 E
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Washington and Todd 2005 GRL Bodele daily dust Vs 1000 hPa geopotentials and 950 vector winds (JFM)
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Tibesti Ennedi Gap Flow Bodele LLJ Palaeo Lake
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Phase of TOMS AI 1980-1992
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Dust in Colour Rainfall black contours
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Annual Cycle of TOMS AI Vs Annual Cycle of ERA-40 Surface Wind
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Annual Cycle of TOMS AI Vs Annual Cycle of ERA-40 Surface Divergence
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Mean TOMS AI for main dust season May-Aug (1980-92) WA1 WA2 WA3 WA4 BOD EA
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WA1WA2WA3WA4BODEA Mean TOMS AI for dust season May-Aug (1980-92) Engelstaedter and Washington in prep
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Annual Cycle of TOMS AI Vs Annual Cycle of ERA-40 surface gustiness
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Eastern Sahara (Chad): Mean wind controls aerosol production Western Sahara (Mali/Mauri heat low): surface convergence and wind gustiness fits annual cycle better
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Parcel trajectory density climatology July (1979-98) Djouf region (17.5-22.5N, 2.5-7.5W) % trajectories remain over Sahara (> 15N < 30N) 69 33 6 % trajectories crossing the 15W meridian 33 66 83 After days 3 5 10
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