Our results suggest that the amplifying feedback of dust on sea surface temperatures and regional climate may be significant and that accurate simulation of dust’s radiative effects is likely essential to improving model representations of past and future precipitation variations in North Africa. status released display-pdf yes is-olf no is-manuscript no is-preprint no is-journal-matter no is-scanned no is-retracted no Received 2016 Feb 29; Accepted 2016 Oct 20; Collection date 2016 Nov.
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Glacial to Holocene changes in trans-Atlantic Saharan dust transport and dust-climate feedbacks.
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