Seasonal, longitudinal, and latitudinal differences in the amount of precipitation in Russia during the years of maximum and minimum of solar actvity

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An analysis of a large array of observation data (over ~50–80 years) for 456 meteorological stations in Russia revealed a distinct difference in the monthly amount of precipitation (DP) during years of maximum and minimum solar activity depending on months and seasons of the year and on latitudes and longitudes. Particularly large DP values are observed in the latitude belt of U = 40–55° N in the longitude range D = 20–40° E in October, DP being 13.6±2.2 mm, as well as in the longitude range D = 110–130° E in June, DP being −8.5±1.0 mm. In the zone of maximum influence of solar activity on the amount of precipitation, a study was conducted on the presence of a correlation between Wolf numbers and the amount of precipitation. As a result, a strong increase in the correlation was discovered in the case of a backward shift in the Wolf numbers, which argued in favor of the influence of solar activity on weather. The author is convinced of the physical significance of the correlation, because it is obtained from data from several geographical points. It is concluded that solar and geomagnetic activity can govern the development of internal instabilities of the atmosphere and thereby influence climate.

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作者简介

V. Laptukhov

Pushkov Institute of Terrestrial Magnetism, Ionosphere, and Radio Wave Propagation

编辑信件的主要联系方式.
Email: laptuhov@mail.ru
俄罗斯联邦, Moscow, Troitsk

参考

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2. Fig. 1. Dependence of the parameter DP on the latitude U in the longitude range D = 20−50° E: (a) for November, December, January, February, March and April; (b) for May, June, July, August, September and October.

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3. Fig. 2. Dependence of the parameter DP on the longitude D in the latitude range U = 40−55° N: (a) for November, December, January, February, March and April; (b) for May, June, July, August, September and October.

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4. Fig. 3. Dependence of the average for November, December and January (a); February, March and April (b); May, June and July (c); August, September and October (d) of the parameter DP on the latitude U and longitude D for four latitude intervals in the range U = 40–80° N and eight longitude intervals in the range D = 20–180° E.

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5. Fig. 4. Dependence of the average value of DP and its error on the month number m for the entire range of latitudes and longitudes at 456 meteorological stations in Russia.

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6. Fig. 5. Correlation relationships between Wolf numbers and precipitation amounts for Krasnodar.

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7. Fig. 6. Correlation links between Wolf numbers and the amount of precipitation on Earth for Sochi.

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8. Fig. 7. Correlation links between Wolf numbers and the amount of precipitation on Earth for Blagoveshchensk.

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