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- W969303127 abstract "In the present paper the AA. search an eventual phenomenonwith the universal diurnal variation, which may influence thenatural terrestrial phenomena. Considering that the first cause of thediurnal variations is the solar radiation arriving 011 the Earth, such a phenomenonmay be founded in the diurnal rotation of the Earth, therefore1 lie regions illuminated by the sun are different according to the universaltime. Since the regions of the Earth have different albedo, the solar radiationabsorbed by the entire Earth will have an universal diurnal variation.The A A. have calculated the apparent surface (with the sun as a pointof view) of the lands and of the seas at different hours (U.T.) and in thedifferent period of the year.In order of include in computation the absorption of the solar radiationby the atmosphere, the AA. have calculated these surfaces with acorrection due to this absorption. In these computations the eventualcloudiness not appears, because in this first approximation the cloudinessis supposed equal 011 the entire Earth. These surfaces with the correctionof the atmospheric absorption are proportional to the solar energy reallyabsorbed by the entire Earth.By the comparison of the universal diurnal variation of those surfaceswith that of a natural phenomenon (the atmospheric electric field), theAA. show that it is possible, with some reductions, to make these variationscoincide. These reductions are an advance of the maximum (4 hours) anda coefficient which reckons the albedo's difference.The AA. recognize that it is no possible with this preliminary studyto explain the influence of the solar energy absorbed by the entire Earth011 the atmospheric electric field; but according to the AA. this correlationwill take an important contribution also to the researches for the generalatmospheric circulation." @default.
- W969303127 created "2016-06-24" @default.
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- W969303127 date "2011-05-09" @default.
- W969303127 modified "2023-10-01" @default.
- W969303127 title "L'assorbimento della radiazione solare su scala planetaria" @default.
- W969303127 doi "https://doi.org/10.4401/ag-5062" @default.
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