The influence absorb stratification on absorptivity of atmosphere; Proceedings of SPIE; Vol. 9292 : Atmospheric and Ocean Optics: Atmospheric Physics

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Parent link:Proceedings of SPIE
Vol. 9292 : Atmospheric and Ocean Optics: Atmospheric Physics.— 2014.— [92920D, 4 р.]
Tác giả chính: Goryachev B. V. Boris Valentinovich
Tác giả của công ty: Национальный исследовательский Томский политехнический университет (ТПУ) Физико-технический институт (ФТИ) Кафедра общей физики (ОФ)
Tác giả khác: Mogilnitskiy S. B. Sergey Borisovich
Tóm tắt:Title screen
The authors have studied the radiation transfer in multilayer atmosphere. The analytical formulae for the calculation of the transmission coefficient, reflectance and absorption of dispersion media consisting of three plane layers were obtained. It was shown that absorption of dispersed media depends strongly on absorption layer’s position in dispersed media. The lowest value is marked when the layer takes place below of the media the light falls from above. Investigation of the radiation balance of the atmosphere is usually conducted on the basis of the theory of radiative transfer and numerical methods [1]. In conducting research using various models of the atmosphere [2-4]. Accuracy of the results depends on the accuracy of the approximation and taking into account all the effects that significantly affect the results, such as the effect of the spatial limitations of the dispersion medium [4-6].
Режим доступа: по договору с организацией-держателем ресурса
Ngôn ngữ:Tiếng Anh
Được phát hành: 2014
Những chủ đề:
Truy cập trực tuyến:http://dx.doi.org/10.1117/12.2075424
Định dạng: Điện tử Chương của sách
KOHA link:https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=641648

MARC

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330 |a The authors have studied the radiation transfer in multilayer atmosphere. The analytical formulae for the calculation of the transmission coefficient, reflectance and absorption of dispersion media consisting of three plane layers were obtained. It was shown that absorption of dispersed media depends strongly on absorption layer’s position in dispersed media. The lowest value is marked when the layer takes place below of the media the light falls from above. Investigation of the radiation balance of the atmosphere is usually conducted on the basis of the theory of radiative transfer and numerical methods [1]. In conducting research using various models of the atmosphere [2-4]. Accuracy of the results depends on the accuracy of the approximation and taking into account all the effects that significantly affect the results, such as the effect of the spatial limitations of the dispersion medium [4-6]. 
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461 |t Proceedings of SPIE 
463 |t Vol. 9292 : Atmospheric and Ocean Optics: Atmospheric Physics  |o proceedings 20th International Symposium, 23-27 June 2014, Novosibirsk  |v [92920D, 4 р.]  |d 2014 
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700 1 |a Goryachev  |b B. V.   |c physicist  |c associate Professor of Tomsk Polytechnic University, candidate of physical and mathematical Sciences  |f 1947-  |g Boris Valentinovich  |3 (RuTPU)RU\TPU\pers\34693  |9 18043 
701 1 |a Mogilnitskiy  |b S. B.  |c physicist  |c associate Professor of Tomsk Polytechnic University, candidate of physical and mathematical Sciences  |f 1951-  |g Sergey Borisovich  |3 (RuTPU)RU\TPU\pers\34694 
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