Theoretical and experimental designs of the planetary boundary layer dynamics through a multifractal theory of motion

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SUMMARY

    Because of the effects of buoyancy, tropospheric temperature profiles limits the motion verticality of atmospheric entities, and therefore the PBL appears as a principal stable factor in atmospheric dynamics. The intent of this development is to continue the theoretical and practical advances into atmospheric physics using multifractality and to elaborate the basis of a multifractal theoretical model, which could be used to study the evolution of many types of parameters, most relevantly temperature. Starting with main theoretical aspects, the atmosphere is considered from a multifractal perspective, with all the mathematical consequences that this entails . . .

     

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