Cite this article as:

Tsoi O. B., Kravchenko D. N. Allocation of a Half-Daily Period with the Maximal Contribution of a Day Thermal Convection in Summer Rain Genesis in the Volga-Region . Izvestiya of Saratov University. Earth Sciences, 2006, vol. 6, iss. 1, pp. 18-21. DOI: https://doi.org/10.18500/1819-7663-2006-6-1-18-21

This is an open access article distributed under the terms of Creative Commons Attribution 4.0 International License (CC-BY 4.0).
Heading: 
Geography
UDC: 
551.577.1
Language: 
Russian

Allocation of a Half-Daily Period with the Maximal Contribution of a Day Thermal Convection in Summer Rain Genesis in the Volga-Region

Authors: 
Tsoi Oleg Borisovich, Saratov State University, 83, Astrakhanskaya Str., Saratov, 410012, Russia, TsoyOB@list.ru
Kravchenko Denis N. , Saratov State University, 83, Astrakhanskaya Str., Saratov, 410012, Russia, TsoyOB@list.ru
Abstract

Results of definition of half-daily period with the maximal contribution of a day thermal convection in summer rain genesis are considered. This day period is determined for Penza and Saratov areas as 10–22 h. msk. The contribution of day thermal convection in strengthening of rain genesis of these regions is estimated. The diurnal heating of а underlying surface causes increase of the precipitations sum for not less than one third in average. 

Key words: 
Allocation of a Half-Daily Period with the Maximal Contribution of a Day Thermal Convection in Summer Rain Genesis in the Volga-Region
DOI: 
https://doi.org/10.18500/1819-7663-2006-6-1-18-21
References

1. Цой О.Б. Некоторые результаты исследования структуры летних осадков над Средним Поволжьем // Метеорология и гидрология. 1998. Вып.3. С 13–28. 

2. Волков С.А. Микроклиматы северной части Волгоградского водохранилища. Дис. … канд. геол. наук. Саратов, 1974. 148 с. 

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