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Titlebook: Noctilucent Clouds; Michael Gadsden,Wilfried Schr?der Book 1989 Springer-Verlag Berlin Heidelberg 1989 Absorption.Cloud.Variation.atmosphe

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書(shū)目名稱(chēng)Noctilucent Clouds
編輯Michael Gadsden,Wilfried Schr?der
視頻videohttp://file.papertrans.cn/667/666754/666754.mp4
叢書(shū)名稱(chēng)Physics and Chemistry in Space
圖書(shū)封面Titlebook: Noctilucent Clouds;  Michael Gadsden,Wilfried Schr?der Book 1989 Springer-Verlag Berlin Heidelberg 1989 Absorption.Cloud.Variation.atmosphe
描述An atmospheric phenomenon is considered as ‘explained‘ when we have succeeded in deducing it on the basis of accepted principles of physics. (H. Ertel, Methods and problems of dynamical meteorolo- gy,p. l) Until recently, noctilucent clouds were regarded merely as a curious atmos- pheric phenomenon, the occurrence of which aroused only limited scientific attention. However, in the last two decades the interest they have been given has markedly increased. The clouds, usually pale blue in colour, may be seen on a clear night at high latitudes. Typical examples are illustrated in the book. Clouds looking like these in daytime would be classified as cirrostratus. What sets noctilucent clouds apart is their occurrence in the middle of the night, their very obvious pale blue colour, and their disappearance into the dawn close to the onset of civil twilight when the Sun is 6° below the horizon. as being set apart from ordinary Noctilucent clouds were first recognized clouds in 1884/1885 and in a series of sightings that followed their return in the summer of 1885. That year marked the beginning of observations and the interpretation of twilight phenomena. The impetus came from the extraor
出版日期Book 1989
關(guān)鍵詞Absorption; Cloud; Variation; atmosphere; aurora; climatology; environment; modelling; photometry; planet; rad
版次1
doihttps://doi.org/10.1007/978-3-642-48626-5
isbn_softcover978-3-642-48628-9
isbn_ebook978-3-642-48626-5Series ISSN 0079-1938
issn_series 0079-1938
copyrightSpringer-Verlag Berlin Heidelberg 1989
The information of publication is updating

書(shū)目名稱(chēng)Noctilucent Clouds影響因子(影響力)




書(shū)目名稱(chēng)Noctilucent Clouds影響因子(影響力)學(xué)科排名




書(shū)目名稱(chēng)Noctilucent Clouds網(wǎng)絡(luò)公開(kāi)度




書(shū)目名稱(chēng)Noctilucent Clouds網(wǎng)絡(luò)公開(kāi)度學(xué)科排名




書(shū)目名稱(chēng)Noctilucent Clouds被引頻次




書(shū)目名稱(chēng)Noctilucent Clouds被引頻次學(xué)科排名




書(shū)目名稱(chēng)Noctilucent Clouds年度引用




書(shū)目名稱(chēng)Noctilucent Clouds年度引用學(xué)科排名




書(shū)目名稱(chēng)Noctilucent Clouds讀者反饋




書(shū)目名稱(chēng)Noctilucent Clouds讀者反饋學(xué)科排名




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Observations from Ground Level, what is involved in this scattering. It has become clear that noctilucent clouds are very thin and very sparse assemblies of scatterers. The cloud particles, whatever they may be, scatter light as individuals not as an assembly. Furthermore, there is a negligible amount of rescattering in the cloud
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Spectrophotometry, and there are no obvious emission lines. The relative spectral distribution in the scattered light differs from that of sunlight and, in principle, this difference can be measured and used to estimate the size of the scattering particles. In practice, this is neither easy to do nor exact in applica
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Other Observations,m outbreaks of solar activity. In determining the cause of noctilucent clouds, we can use both the regular emission of light (airglow) for diagnosis and the sporadic disturbances (aurorae) as tests of prognosis.
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Environment of Noctilucent Clouds,of clouds are formed. The physical processes of importance in discussing noctilucent clouds are correspondingly changed in importance. First, the mean free path in the region is much larger than the particle size in the cloud and the physical conditions are those of the Knudsen regime rather than th
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The Nature of Noctilucent Clouds, length. From the very start of the period, hypotheses have been formed and, to the extent practical, tested. Quite naturally, because noctilucent clouds came to notice with the increased awareness of twilight sky phenomena following the Krakatoa eruption, the earliest suggestions were that noctiluc
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on dioxide released during its use is an integral part of the carbon cycle. Increasing the share of biomass in the energy supply contributes to diminishing the environmental impact of CO. and to meeting the targets established in the Kyoto Protocol. The use of biomass waste material as a fuel, howev
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