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Here we use climate model simulations to identify the Tortonian stage (~7–11 Myr ago) of the Late Miocene epoch as the pivotal period for triggering north African aridity and creating the Sahara desert.

Through a set of experiments with the Norwegian Earth System Model, we demonstrate that the African summer monsoon was drastically weakened by the Tethys Sea shrinkage during the Tortonian, allowing arid, desert conditions to expand across north Africa. linked the Saharan aridification to the emergence and evolution of early hominins.

CO;2&rft_id=info:pmid/&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.aulast=Lin&rft.aufirst=S.-J.&rft.jtitle=Mon. CO;2&id=pmid:&genre=article&aulast=Lin&aufirst=S.-J.&title=Mon. J.&title=Nature Geosci.&volume=4&spage=418&epage=420&date=2011&atitle=Convergent Cenozoic CO Z.

All authors contributed to discussion of the results and writing of the paper.

The atmospheric model is forced with observed SSTs from 1901-2002 and the resulting precipitation field is studied on multi-decadal timescales and compared to observations.

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If you are having problem viewing the Web Cam please refresh your screen by holding down CTL and F5 - this will update the webcam. visit to Tembe, so pretty much part of the furniture now.More detailed statistical techniques such as Maximum Covariance Analysis (MCA) are used to understand whether the key modes of variability between global SSTs and Sahel precipitation are similar in observations and the SST-driven model.It is found that on multi-decadal timescales, the ensemble-averaged precipitation maintains the overall characteristics in space and time of the 20th century observed precipitation fields.La masturbation en solo devant leur glace, elles adorent ça !Mate des videos x de filles noires sexy dans leur miroir qui ne se font pas une beauté mais du bien.CO;2&rft_id=info:pmid/&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.aulast=Chou&rft.aufirst=C.&rft.jtitle=J. Clim.&rft.volume=16&rft.spage=406&rft.epage=425& limiting the northward extent of the northern summer convection zones&rfr_id=info:sid/