The atmospheric conditions of hot and mild deserts to be geoengineered

dc.contributor.authorSevilmis, Ugur
dc.date.accessioned2024-03-20T08:26:07Z
dc.date.available2024-03-20T08:26:07Z
dc.date.issued2020-02-10
dc.descriptionSupplemental Materials: https://osf.io/u4b8r/
dc.description.abstractExcess evaporation due to hot, dry and sunny atmosphere with low precipitation and low water holding capacity in ground results with hot hyper arid zones in the world. Sahara, Australia and Arabian deserts are top three covering 9 billion, 2.7 billion and 2.3 billion ha respectively. This paper describes the current knowledge on general atmospheric circulations as a base to a theory to geoengineer the atmosphere to send the climate of Sahara back to 6.000 years ago where tropical grasslands were dominating.
dc.identifier.doihttps://doi.org/10.31730/osf.io/r8gxz
dc.identifier.urihttps://africarxiv.ubuntunet.net/handle/1/1082
dc.identifier.urihttps://doi.org/10.60763/africarxiv/1035
dc.identifier.urihttps://doi.org/10.60763/africarxiv/1035
dc.identifier.urihttps://doi.org/10.60763/africarxiv/1035
dc.subjectAfrican Humid Period
dc.subjectDesert
dc.subjectgeoengineering
dc.subjecthumidity
dc.subjecttemperature
dc.titleThe atmospheric conditions of hot and mild deserts to be geoengineered

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