Daytime sky radiance as a source of information on surface albedo in IR spectral region. Part I
- Авторлар: Pavlov V.E.1, Orlov S.S.2, Pashnev V.V.2
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Мекемелер:
- Institute of Water and Ecological Problems
- Altai State University
- Шығарылым: Том 29, № 3 (2016)
- Беттер: 282-287
- Бөлім: Remote Sensing of Atmosphere, Hydrosphere, and Underlying Surface
- URL: https://journals.rcsi.science/1024-8560/article/view/187781
- DOI: https://doi.org/10.1134/S102485601603012X
- ID: 187781
Дәйексөз келтіру
Аннотация
We suggest a methodical justification of determining the surface albedo in the near-infrared (NIR) region using the observations of spectral atmospheric transparency and daytime clear-sky radiance in solar almucantar. The contribution of the component describing the reflection processes to radiance at different angular distances from the Sun is analyzed. The effect of aerosol absorption on radiance components used in albedo determination is estimated. The solar zenith angle and elongation of aerosol scattering phase function are found to affect the final result of albedo calculation.
Авторлар туралы
V. Pavlov
Institute of Water and Ecological Problems
Хат алмасуға жауапты Автор.
Email: pavlov@iwep.asu.ru
Ресей, ul. Molodezhnaya 1, Barnaul, 656038
S. Orlov
Altai State University
Email: pavlov@iwep.asu.ru
Ресей, pr. Lenina 61, Barnaul, 656015
V. Pashnev
Altai State University
Email: pavlov@iwep.asu.ru
Ресей, pr. Lenina 61, Barnaul, 656015
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