Balance of Transit Irradiation of Space Surrounding the Earth

Fedorov, V.M.; Kostin, A.A.; Frolov, D.M.

Авторы: Fedorov V.M., Kostin A.A., Frolov D.M.
Журнал: Cosmic Research (English translation of Kosimicheskie Issledovaniya)
Том: 60
Номер: 2
Год издания: 2022
Издательство: Pleiades Publishing, Inc.
Местоположение издательства: New York, USA
Первая страница: 89
Последняя страница: 97
Оригинальные версии: Баланс транзитного облучения окружающего Землю пространства
DOI: 10.1134/S0010952522020034
Аннотация: The irradiation of surfaces of high-altitude levels from the upper troposphere to the lower mesosphereis considered. Previously not performed calculations of the characteristics of transit irradiation of latitudinalzones of surfaces in tropical years and their parts from 3000 BCE to 2999 CE have been carried out. Energy characteristics(J) are calculated for all years and specific energy characteristics (J/m2) are calculated as average ofmany years and for individual years. For each pair (latitudinal zone and part of the tropical year), the specificentering (through this zone into a body bounded by the surface) transit energy, the specific outgoing (from abody bounded by the surface) transit energy and their difference (balance) are calculated. For the whole surface,the balance for any period of time is equal to zero (in the absence of the atmosphere); for the half-surface and5° latitude zone in the presence of transit irradiation, the balance is nonzero. On the surfaces of all altitude levels,the most significant spread between the balances for 5° zones is noted among the semiannual balances in thepolar regions. For 5° zones of each semisurface from the equator to the pole in the summer half of the year, thesemiannual balance to the 65th parallel is negative, then positive, and vice versa in the winter half of the year.The semiannual balance for the semisurface in the summer half of the year is positive and negative in the winterhalf of the year at all altitude levels. In the considered range of years, the modulus of the semiannual balance forthe semisurface decreases in both summer and winter halves of the year.
Добавил в систему: Федоров Валерий Михайлович

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