Примеры использования Thunder-storms на Английском языке и их переводы на Русский язык
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Klossovsky,"Thunder-storms in Russia"(1884); article A.
Together with private cyclones also thunder-storms move.
Night thunder-storms are most frequent in the south of Russia and in the Western region.
Sometimes it happens that thunder-storms meet one another.
On it the thunder-storms which were in the southern Russia on June 5, 1886 are represented.
In a midland of Siberia, between 50 and 60,is to 15 thunder-storms a year.
In northern andCentral Russia thunder-storms most often in July, in the south- in June.
Behind polar circles they are extremely rare;often pass the whole years without thunder-storms.
In Russia the correct supervision over thunder-storms began on an initiative Imp.
Klossovsky("Thunder-storms in Russia", 1884), storm activity is distributed as follows.
Behind these exceptions in Russia summer thunder-storms resolutely prevail.
It is more for the thunder-storms moving from the West, and less for the thunder-storms going from the East.
Environmental impacts, such as strong wind and thunder-storms, can severely damage a tank system.
But sometimes thunder-storms move from an education place radially, in all directions; then izokhrona are close to circles of circles.
Through points with the simultaneous beginnings orthe simultaneous ends of thunder-storms lines- izobronta were drawn.
On the basis of supervision over thunder-storms of the end of XIX- the beginning of the XX century.
At coast of the Black Sea storm activity quickly falls;it is especially weak in the Crimea where in a year there are only about 6 thunder-storms.
Recently you heard on the TV how during strong thunder-storms lightning did accurately hit the tops of several city churches, but….
These thunder-storms are remarkable by the unusual force of electric discharges: lightnings sparkle continuously, the thunder rattles with a terrible force, fireballs(see the Fireball) in all directions plow the sky.
Supervision of storm networks led to many curious results in relation to thunder-storms of Europe from which we will specify the major.
The most northern thunder-storms were observed during especially hot summer in the Kara Sea and in the western part of Spitsbergen in latitude 78.
As the warm time of day is optimum for formation of the ascending air currents, thunder-storms in these times have to be most frequent.
Private cyclones, and together with them and thunder-storms, are most often formed in cyclones at their suburbs in a belt of 755 mm- 760 mm in southeast part them.
The same belongs, of course, and to Russia,apparently from the following table showing how often there are thunder-storms from the different countries of light as a percentage.
To the East and the Southeast from here their number remains almost invariable, to the South increases, and in the Southwest of Russia reaches a maximum;here in a year happens to 20 thunder-storms.
At that moment for which nacherchena of an isobar, thunder-storms were located on the line close to an axis of this minimum an izokhron of 9 hours.
It depends on distribution of temperature and amount of water vapor, on rainfall, and also local conditions,as it is clear as thunder-storms are a consequence of the ascending air movements.
In Europe most often thunder-storms move about the SKID, Z and SZ, as well as it was necessary to assume on the basis of their communication with cyclones; the thunder-storms going since Century are most rare.
Then where clear and dry weather, and in the spring in the summer dominates andin the fall more often there are rains, thunder-storms are also more often in these seasons and are rare in the summer.
So, thunder-storms, meeting on the way cold districts(the rivers, lakes and so forth), bend around them, or jump through them, or, at last, absolutely stop; opposite to that, districts marshy, rich with water vapor, and sometimes strongly heating up, as if attract thunder-storms and in general promote development of storm activity.