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Nocturnal low‐level jets (LLJs) are maxima in the wind profile, which often form above the stable nocturnal boundary layer. Over the Sahara, the world's largest source of mineral dust, this phenomenon is of particular importance to the emission and transport of desert aerosol. We present the first ever detailed large‐eddy simulations of dust‐generating LLJs. Using sensitivity studies with the UK Met...
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