Evaluation of Long-Term Changes in Radiation, Cloudiness, and Surface Temperature on the Territory of the Former Soviet Union

G. M. Abakumova Meteorological Observatory, Department of Geography, Moscow State University, Vorobevy gory, Moscow, Russia

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E. M. Feigelson Institute of Atmospheric Physics, Russian Academy of Sciences, Pyzhevsky, Moscow, Russia

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V. Russak Institute of Astrophysics and Atmospheric Physics, Estonian Academy of Sciences, Tõravere, Estonia

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V. V. Stadnik Main Geophysical Observatory, Federal Russian Service of Meteorology and Monitoring of Environment, Karbysheva, St. Petersburg, Russia

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Abstract

Regular measurements of solar radiation carried out in the network of actinometric stations of the former Soviet Union (FSU) have shown a decreasing tendency in the time series of direct and global solar radiation during last decades. A statistically significant decrease has been found in 60% of the time series of global radiation annual totals obtained from 160 actinometric stations. Three large areas, where this decrease exceeded 2% per 10 years, were found (in the European part of the FSU, in West Siberia, and in the Far East). As the main reason for changes in solar radiation, increased cloudiness and atmospheric turbidity are considered. A more detailed analysis of long-term changes in radiation budget components obtained from two stations situated in rather different conditions (Moscow Meteorological Observatory in a large town and Tõravere Actinometric Station in a rural area) allows us to point out the influence of a large town as a source of air pollution on the radiation transfer in the atmosphere, as well as on cloudiness and air temperature.

Abstract

Regular measurements of solar radiation carried out in the network of actinometric stations of the former Soviet Union (FSU) have shown a decreasing tendency in the time series of direct and global solar radiation during last decades. A statistically significant decrease has been found in 60% of the time series of global radiation annual totals obtained from 160 actinometric stations. Three large areas, where this decrease exceeded 2% per 10 years, were found (in the European part of the FSU, in West Siberia, and in the Far East). As the main reason for changes in solar radiation, increased cloudiness and atmospheric turbidity are considered. A more detailed analysis of long-term changes in radiation budget components obtained from two stations situated in rather different conditions (Moscow Meteorological Observatory in a large town and Tõravere Actinometric Station in a rural area) allows us to point out the influence of a large town as a source of air pollution on the radiation transfer in the atmosphere, as well as on cloudiness and air temperature.

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