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標(biāo)題: Titlebook: Meteorological Investigations of the Upper Atmosphere; R. S. Quiroz Book 1968 American Meteorological Society 1968 Mesosphere.Ionosphere.T [打印本頁]

作者: 并排一起    時(shí)間: 2025-3-21 18:12
書目名稱Meteorological Investigations of the Upper Atmosphere影響因子(影響力)




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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





作者: profligate    時(shí)間: 2025-3-21 20:31
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
作者: LATER    時(shí)間: 2025-3-22 04:05
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
作者: ARCH    時(shí)間: 2025-3-22 06:54

作者: 感染    時(shí)間: 2025-3-22 09:46

作者: 聯(lián)想記憶    時(shí)間: 2025-3-22 14:46
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
作者: Crayon    時(shí)間: 2025-3-22 17:33
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
作者: oncologist    時(shí)間: 2025-3-22 23:07
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
作者: 同位素    時(shí)間: 2025-3-23 03:30

作者: 無脊椎    時(shí)間: 2025-3-23 09:19

作者: 痛打    時(shí)間: 2025-3-23 12:02

作者: ANTH    時(shí)間: 2025-3-23 17:40
The General Circulation of the Atmosphere Above 60 Kmons are made for tests of the present theories. Energy, momentum and mass budgets are treated. Meridional cross sections of temperature are used as the basis for the discussion of the energy budget. Meteor trail winds are used as one item in the momentum budget. Atomic oxygen and ozone are treated a
作者: 使痛苦    時(shí)間: 2025-3-23 20:49
Tidal Oscillations, Shorter Period Gravity Waves and Shear Wavescal clarification of the excitation and distribution of diurnal tidal oscillations, 2) the introduction of sequential rocketborne measurements of tidal parameters to heights of 150 km, and 3) clarification of the roles played by thermal and wind gradients, and by dissipative processes, in the propag
作者: GORGE    時(shí)間: 2025-3-24 00:08
Some Observations of Turbulence in the 80 to 110 Km Region of the Upper Atmospherecity probability density, the structure function, eddy diffusivities, heating rate, and the altitude and seasonal variation of the energy balance parameters of the turbulence are discussed. Some aspects of the apparent disagreement between meteor trail and chemical release measurements are presented
作者: Synchronism    時(shí)間: 2025-3-24 03:25
D-Region Phenomena and Stratospheric-Mesospheric Couplingon and D-region phase heights, as well as from special events and anomalies in the wintertime behavior of the lower ionosphere. The paper presents examples of annual variations of ionospheric absorption and phase height at constant solar zenith angles, the results of investigations of sunrise phenom
作者: 符合你規(guī)定    時(shí)間: 2025-3-24 08:59

作者: AXIS    時(shí)間: 2025-3-24 11:44
Relative Motion of Ion and Neutral Clouds technique for evaporation and the process of ionization are described. By observing the drift motions of the ionized barium clouds, the electric fields have been determined in the upper atmosphere. Results are given in particular for measurements at mid-latitudes.
作者: 愛好    時(shí)間: 2025-3-24 15:32

作者: Diatribe    時(shí)間: 2025-3-24 19:06
Meteorological Rocket Measurements in the Mesospherethe relationship between synoptic data and special mesospheric data such as isolated soundings and indirect observations of various natural phenomena (e.g., noctilucent clouds, meteor trail drifts, air glow and ionospheric inhomogeneities). Progress in upward extension of current Global Meteorologic
作者: Amylase    時(shí)間: 2025-3-24 23:16
from the introductory chapter in Volume 1, the intensity of the fundamental with number . (. = 1,..., 3. ? 6 or i. ? 5, etc.), characterized by normal coordinate .., may be written after Introduction of Placzeck’s simplified polarizability theory as . The occurrence of . indicates dependence on the
作者: Aggrandize    時(shí)間: 2025-3-25 03:55
B. N. Charlesy, and species concentrations) for more than 5 decades. This technique is renowned for its ability to realize non-intrusive in-situ measurements in harsh environments with excellent spatial and temporal resolution and has become an important tool in multiple energy and combustion science application
作者: minimal    時(shí)間: 2025-3-25 10:57

作者: ABIDE    時(shí)間: 2025-3-25 12:22

作者: SEVER    時(shí)間: 2025-3-25 19:12
J. B. Gregoryopy has proven to be a powerful tool for the characterization of the structure of matter in the gaseous, liquid, and solid phases, one major difficulty in its application has been laser damage to the material under investigation, especially for biological samples. This book demonstrates how immersio
作者: Notify    時(shí)間: 2025-3-25 20:05

作者: 令人悲傷    時(shí)間: 2025-3-26 00:25

作者: 山崩    時(shí)間: 2025-3-26 06:38

作者: theta-waves    時(shí)間: 2025-3-26 09:42

作者: hedonic    時(shí)間: 2025-3-26 16:00

作者: 清楚    時(shí)間: 2025-3-26 19:27

作者: Perineum    時(shí)間: 2025-3-26 20:57

作者: 朦朧    時(shí)間: 2025-3-27 02:16

作者: Granular    時(shí)間: 2025-3-27 05:53

作者: Palate    時(shí)間: 2025-3-27 11:13
Purpose of the Symposiumand applications.” A wealth of scientific experience has proven that such exchanges inspire new findings, generate new concepts, and refresh and stimulate the seekers of new knowledge and those who apply such knowledge in the service of society.
作者: degradation    時(shí)間: 2025-3-27 16:33

作者: labile    時(shí)間: 2025-3-27 21:02
Book 1968tions, and the advancement of its professional ideals." The organization of the Society took place in affiliation with the American Association for the Advancement of Science at Saint Louis, Missouri, December 29, 1919, and its incorporation, at Washington, D. C., January 21, 1920. The work of the S
作者: 酷熱    時(shí)間: 2025-3-27 22:54
Lower Atmospheric Energy Sources for the Upper Atmospherees and thermal and gravitational tides, and the factors influencing their transmission to the upper atmosphere are discussed. In the case of tides a quantitative description of the magnitudes and energetics is presented. A simple model for evaluating the thermal effects of wave dissipation is also presented.
作者: fertilizer    時(shí)間: 2025-3-28 05:15

作者: HEDGE    時(shí)間: 2025-3-28 07:39

作者: Ferritin    時(shí)間: 2025-3-28 12:59
The Influence of the Neutral Wind Field on the Distribution of Ionization in the E-Region shown to be responsible for the production of two layers in a recent experiment. It is suggested that this neutral convergence mechanism may be responsible for the low-altitude layers whose occurrence cannot be predicted by the mechanisms depending solely on vertical shear of the horizontal neutral wind.
作者: 使更活躍    時(shí)間: 2025-3-28 16:36

作者: phytochemicals    時(shí)間: 2025-3-28 22:09
0065-9401 dissemination of knowledge of meteorology in all its phases and applications, and the advancement of its professional ideals." The organization of the Society took place in affiliation with the American Association for the Advancement of Science at Saint Louis, Missouri, December 29, 1919, and its i
作者: 防銹    時(shí)間: 2025-3-29 00:10
Ionospheric Winds and Associated Geomagnetic Variations winds over the dynamo region of the ionosphere, the weights being related to the conductivity distribution. However, given a theoretical wind model, . could provide a partial, if not complete, verification of the wind model in the dynamo region; a direct check by wind measurement with rockets, however, will require a prohibitive effort.
作者: 小說    時(shí)間: 2025-3-29 05:36

作者: 確認(rèn)    時(shí)間: 2025-3-29 09:30

作者: bleach    時(shí)間: 2025-3-29 11:39
Meteorological Rocket Measurements in the Mesosphere. It is concluded that synoptic exploration of the mesosphere is required before a comprehensive knowledge of the earth’s entire atmosphere can be obtained. The tools are available, and the time for mesospheric synoptic probing is now.
作者: 正面    時(shí)間: 2025-3-29 19:07

作者: 萬靈丹    時(shí)間: 2025-3-29 21:21

作者: 盡忠    時(shí)間: 2025-3-30 01:08

作者: modest    時(shí)間: 2025-3-30 06:33

作者: Accessible    時(shí)間: 2025-3-30 08:18

作者: 安定    時(shí)間: 2025-3-30 14:13
Density and Temperature Variations in the Intervening Layer (90–150 Km) km altitude. But even they must still be regarded as a theoretical compromise, linking, in essentially a schematic manner, a wealth of empirical data from altitudes below and above through an intervening layer whose physical processes we do not quantitatively understand. Comprehensive interdiscipli
作者: Lacunar-Stroke    時(shí)間: 2025-3-30 17:51

作者: 儲(chǔ)備    時(shí)間: 2025-3-30 23:33
Meteorological Investigations of the Upper Atmosphere
作者: 細(xì)節(jié)    時(shí)間: 2025-3-31 04:08

作者: Stable-Angina    時(shí)間: 2025-3-31 08:14

作者: 串通    時(shí)間: 2025-3-31 10:12

作者: HERTZ    時(shí)間: 2025-3-31 16:16

作者: 侵略    時(shí)間: 2025-3-31 19:37





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