Titlebook: Compendium of Meteorology; H. R. Byers,H. E. Landsberg,H. G. Houghton,Thomas Book 1951 American Meteorological Society 1951 atmospheric s

Coronary-Artery

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隨意

https://doi.org/10.1007/978-3-030-26626-4al and trigonometrical considerations [61]; thus on a relative scale, the diurnal and seasonal variations of this solar irradiation above the atmosphere are known. On the average, variations similar to these occur also at the earth’s surface, and the associated diurnal and seasonal changes in atmospheric temperature are commonplace knowledge [52].

楓樹

Pamphlet

浮雕寶石

Solar Radiant Energy and its Modification by the Earth and its Atmosphereal and trigonometrical considerations [61]; thus on a relative scale, the diurnal and seasonal variations of this solar irradiation above the atmosphere are known. On the average, variations similar to these occur also at the earth’s surface, and the associated diurnal and seasonal changes in atmospheric temperature are commonplace knowledge [52].

FOIL

FOIL

Universal Aspects of Atmospheric Electricitypect of atmospheric electricity which is not universal. Lightning is seldom seen in the polar regions and even in temperate latitudes it is seen only a small fraction of the time. The study by Brooks [8] indicates that on one-fourth of the earth’s surface thunder may be heard on less than one day in a hundred.

圓柱

AGATE

Monotonous

https://doi.org/10.1007/978-981-97-4214-1charge production and transport processes in the atmosphere. One serious difficulty in the proper evaluation of precipitation electric phenomena is that the data thus far collected have been limited to a relatively few geographical regions and with few exceptions have covered only short periods of time. Many of the data are contradictory.