Titlebook: Meteorological Investigations of the Upper Atmosphere; R. S. Quiroz Book 1968 American Meteorological Society 1968 Mesosphere.Ionosphere.T

并排一起

書目名稱Meteorological Investigations of the Upper Atmosphere影響因子(影響力)




書目名稱Meteorological Investigations of the Upper Atmosphere影響因子(影響力)學(xué)科排名




書目名稱Meteorological Investigations of the Upper Atmosphere網(wǎng)絡(luò)公開度




書目名稱Meteorological Investigations of the Upper Atmosphere網(wǎng)絡(luò)公開度學(xué)科排名




書目名稱Meteorological Investigations of the Upper Atmosphere被引頻次




書目名稱Meteorological Investigations of the Upper Atmosphere被引頻次學(xué)科排名




書目名稱Meteorological Investigations of the Upper Atmosphere年度引用




書目名稱Meteorological Investigations of the Upper Atmosphere年度引用學(xué)科排名




書目名稱Meteorological Investigations of the Upper Atmosphere讀者反饋




書目名稱Meteorological Investigations of the Upper Atmosphere讀者反饋學(xué)科排名

profligate

Research on the Lower Fringe of Spaceeen the motions of the neutral atmosphere and the ionized portion; interactions, both by dynamic processes and by radiative transfer, between the upper and lower atmosphere; and refinement of indirect probing techniques which can be used to study this region from the ground or from satellites. Recen

LATER

Aerospace Systems Requirements for Environmental Data in the Altitude Range 60–200 Kmthe 60–200 km layer of the atmosphere. If history repeats itself, some urgently needed atmospheric data may not be recognized at the present stage of development of these vehicles any more than was the need for information on clear air turbulence data foreseen 10–15 years ago by designers and operat

ARCH

感染

聯(lián)想記憶

Lower Atmospheric Energy Sources for the Upper Atmosphere conversion. Brief attention is devoted to energy reaching the upper atmosphere by radiation and diffusion. Energy carried to the upper atmosphere by advection by the mean field and by vertically propagating waves is treated in greater detail. The explicit excitations of gravity waves, planetary wav

Crayon

Composition of the Mesosphere and Lower Thermosphere of the major constituents of the atmosphere. Above the turbopause, diffusive separation exists and the composition rapidly changes with increasing altitude. In the atmosphere the change probably does not occur sharply and the transition may be spread over an altitude range of as much as 30 km. For

oncologist

Temperature, Density and Pressure Variations in the Stratosphere and the Mesosphereriability of temperature, density and pressure in the stratosphere and mesosphere from 25 to 55 km. The results, which are in general agreement with those of previous investigations, show large changes with season at high latitudes, with the greatest variability in winter and spring. Standard deviat

同位素

無脊椎