The distribution of temperature in an active region for a comet with known parameters of rotation and orbit

We calculated the temperature regime of an active region considered as a conical hole in dust layer. All the calculations are carried out for the case when the season effects are distinctly expressed. The temperature is defined from the geometrical parameters of the active region separately for ice...

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Veröffentlicht in:Кинематика и физика небесных тел
Datum:2005
Hauptverfasser: Ivanova, A.V., Shulman, L.M.
Format: Artikel
Sprache:English
Veröffentlicht: Головна астрономічна обсерваторія НАН України 2005
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Online Zugang:https://nasplib.isofts.kiev.ua/handle/123456789/79711
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Назва журналу:Digital Library of Periodicals of National Academy of Sciences of Ukraine
Zitieren:The distribution of temperature in an active region for a comet with known parameters of rotation and orbit / A.V. Ivanova, L.M. Shulman // Кинематика и физика небесных тел. — 2005. — Т. 21, № 5-додаток. — С. 509-512. — Бібліогр.: 6 назв. — англ.

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Digital Library of Periodicals of National Academy of Sciences of Ukraine
id nasplib_isofts_kiev_ua-123456789-79711
record_format dspace
spelling Ivanova, A.V.
Shulman, L.M.
2015-04-03T20:02:02Z
2015-04-03T20:02:02Z
2005
The distribution of temperature in an active region for a comet with known parameters of rotation and orbit / A.V. Ivanova, L.M. Shulman // Кинематика и физика небесных тел. — 2005. — Т. 21, № 5-додаток. — С. 509-512. — Бібліогр.: 6 назв. — англ.
0233-7665
https://nasplib.isofts.kiev.ua/handle/123456789/79711
We calculated the temperature regime of an active region considered as a conical hole in dust layer. All the calculations are carried out for the case when the season effects are distinctly expressed. The temperature is defined from the geometrical parameters of the active region separately for ice bottom and dust walls. It is shown that dust walls are cooled very slowly for the small vertex angles of the crater structure. The temperature of the ice bottom practically does not change over the whole period of rotation, because it is retained at an approximately constant level by concentration of reradiated energy from the dust walls heated by the Sun.
This work was supported by the Fundamental Research State Fund of the Ministry of Ukraine for Education and Science.
en
Головна астрономічна обсерваторія НАН України
Кинематика и физика небесных тел
MS5: Dynamics and Physics of Solar System Bodies
The distribution of temperature in an active region for a comet with known parameters of rotation and orbit
Article
published earlier
institution Digital Library of Periodicals of National Academy of Sciences of Ukraine
collection DSpace DC
title The distribution of temperature in an active region for a comet with known parameters of rotation and orbit
spellingShingle The distribution of temperature in an active region for a comet with known parameters of rotation and orbit
Ivanova, A.V.
Shulman, L.M.
MS5: Dynamics and Physics of Solar System Bodies
title_short The distribution of temperature in an active region for a comet with known parameters of rotation and orbit
title_full The distribution of temperature in an active region for a comet with known parameters of rotation and orbit
title_fullStr The distribution of temperature in an active region for a comet with known parameters of rotation and orbit
title_full_unstemmed The distribution of temperature in an active region for a comet with known parameters of rotation and orbit
title_sort distribution of temperature in an active region for a comet with known parameters of rotation and orbit
author Ivanova, A.V.
Shulman, L.M.
author_facet Ivanova, A.V.
Shulman, L.M.
topic MS5: Dynamics and Physics of Solar System Bodies
topic_facet MS5: Dynamics and Physics of Solar System Bodies
publishDate 2005
language English
container_title Кинематика и физика небесных тел
publisher Головна астрономічна обсерваторія НАН України
format Article
description We calculated the temperature regime of an active region considered as a conical hole in dust layer. All the calculations are carried out for the case when the season effects are distinctly expressed. The temperature is defined from the geometrical parameters of the active region separately for ice bottom and dust walls. It is shown that dust walls are cooled very slowly for the small vertex angles of the crater structure. The temperature of the ice bottom practically does not change over the whole period of rotation, because it is retained at an approximately constant level by concentration of reradiated energy from the dust walls heated by the Sun.
issn 0233-7665
url https://nasplib.isofts.kiev.ua/handle/123456789/79711
citation_txt The distribution of temperature in an active region for a comet with known parameters of rotation and orbit / A.V. Ivanova, L.M. Shulman // Кинематика и физика небесных тел. — 2005. — Т. 21, № 5-додаток. — С. 509-512. — Бібліогр.: 6 назв. — англ.
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