Национальный цифровой ресурс Руконт - межотраслевая электронная библиотека (ЭБС) на базе технологии Контекстум (всего произведений: 611400)
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Первый авторYakunin
Страниц6
ID453676
АннотацияA new method to evaluate the solar energy absorbed by the surface using remote sensing data and the method of basic spectra is presented. The proposed method allows one to calculate parameters of radiation transferring in the atmosphere without being related to specific satellite instruments or areas.
УДК528.8.04:528.88
Yakunin, MaximA. A Hybrid Method for Evaluating Absorbed Solar Energy at the Surface Level Using Remote Sensing Data / MaximA. Yakunin // Журнал Сибирского федерального университета. Математика и физика. Journal of Siberian Federal University, Mathematics & Physics .— 2015 .— №2 .— С. 102-107 .— URL: https://rucont.ru/efd/453676 (дата обращения: 13.05.2025)

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Mathematics & Physics 2015, 8(2), 224–229 УДК 528.8.04:528.88 A Hybrid Method for Evaluating Absorbed Solar Energy at the Surface Level Using Remote Sensing Data Maxim A.Yakunin∗ Altai state university, Krasnoarmeiskiy, 90, Barnaul, 695049 Russia Received 04.01.2015, received in revised form 13.02.2015, accepted 20.03.2015 A new method to evaluate the solar energy absorbed by the surface using remote sensing data and the method of basic spectra is presented. <...> The proposed method allows one to calculate parameters of radiation transferring in the atmosphere without being related to specific satellite instruments or areas. <...> Keywords: basic spectra method, remote sensing, transmittance, aerosol optical thickness, total precipitable water, absorbed solar energy. <...> Introduction The amount of solar energy absorbed by the "atmosphere–surface" system is a key parameter in the problem of global climate change. <...> The use of remote sensing satellite data is the most convenient way to establish monitoring of the radiation balance of the earth over vast areas. <...> The majority of current models for evaluating the solar energy absorbed by the surface using satellite data are based on statistical processing of data fromnumerical simulations of atmosphere radiation transfer. <...> It uses MODIS/Terra spectroradiometer data for the top of the atmosphere (TOA) radiances to calculate then amount of solar energy W (W/m2) absorbed at the surface level: W = (α′ −β′r)E0 cos θs/d2, (1) where r is the TOA broadband albedo, θs is the solar zenith angle, E0 is the TOA solar irradiance at one astronomical unit (1358 W/m2), d is the distance from Earth to the sun in astronomical units. <...> MODIS/Terra spectral radiances ρ are used to calculate TOA broadband albedo r: 7 r = b0 +  i=1 biρi. (2) The main drawback of this and other similar models [2, 3] is the need for solving systems of equations which are obtained by fitting a large number of numerical simulation data. <...> All rights reserved c – 224 – Maxim A.Yakunin A hybrid method for evaluating absorbed solar energy at the Surface Level . it is impossible to evaluate <...>