Titlebook: Geophysik II / Geophysics II; Julius Bartels Book 1957 Springer-Verlag Berlin Heidelberg 1957 Wellen.atmosphere.density.diffraction.diffus

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書目名稱Geophysik II / Geophysics II影響因子(影響力)




書目名稱Geophysik II / Geophysics II影響因子(影響力)學(xué)科排名




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書目名稱Geophysik II / Geophysics II網(wǎng)絡(luò)公開度學(xué)科排名




書目名稱Geophysik II / Geophysics II被引頻次




書目名稱Geophysik II / Geophysics II被引頻次學(xué)科排名




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書目名稱Geophysik II / Geophysics II年度引用學(xué)科排名




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書目名稱Geophysik II / Geophysics II讀者反饋學(xué)科排名

Optimum

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PANG

Polarization of Skylight,he polarized component to be either perpendicular (positive polarization) or parallel (negative polarization) to the plane defined by the directions from the observer to sun and from the observer to point observed, and to reach its . at about 90° from the sun. In the sun vertical on the antisolar si

entail

,Ozon in der Erdatmosph?re,und sp?ter (1839, .) auch bei chemischen Prozessen, wie der langsamen Oxydation des Phosphors an der Luft, gefunden worden, ohne da? allerdings die chemische Natur dieses Gases schon bekannt gewesen war. Diese wurde erst 1864 durch . gekl?rt, der die richtige Formel O. aufstellte ..

otic-capsule

Geophysical Aspects of Meteors,ry great. The majority of these meteors are minute pieces of stone or iron moving in closed orbits in the solar system. Occasionally the earth encounters concentrated groups of meteors known as ., and these provide the most spectacular part of meteoric phenomena in which the visible hourly rate may

otic-capsule

The Physics of Clouds,rt of the science of meteorology. In the last fifteen years there has been a surge of activity in this science under the stimulus of development in civil and military aviation. The growth of cloud physics during this period has been fostered not only by this general invigoration, but also by recogni

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resistant

Oceanography,me, except that a brief treatment of internal waves is given here, because in the presence of internal waves caution has to be excercised when discussing other phenomena. The chemistry of the sea water is touched upon, because in some cases knowledge of the distribution of chemical constituents help

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