Приклади вживання Air masses Англійська мовою та їх переклад на Українською
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Air Masses and Fronts.
Front- the boundary between air masses.
The boundary between two air masses is called a frontal zone.
The jet forms a relatively sharp dividing line between the warm tropical andcold polar air masses.
The boundary between two air masses is called a frontal zone.
The plains in the east, by contrast,allow almost unhindered from the Atlantic to penetrate the warm and moist air masses deep into the mainland.
The zone between two different air masses is a frontal zone or front.
Sometimes, cold air masses from Russia can lower the temperature by many degrees, down to -20 °C(-4 °F), and sometimes even below.
Fronts are created when two air masses meet.
As the fronts between the air masses shift north and south across Alberta, the temperature can change rapidly.
The surface of separation between the two different air masses is called a frontal surface.
Thus, air masses, which are south-east trade winds from the Pacific Ocean, heated and saturated with moisture over warm Shidnoavstraliyskoyu Drift.
Stationary Front The border between cold and warm air masses that are not moving.
The country is exposed to both cold air masses from northern Europe or Russia, and warm air masses from the Mediterranean or North Africa.
Under normal dispersion conditions,hot pollutant gases rise as they come into contact with colder air masses with increasing altitude.
Transition from marine to continental, marine air masses is determined from the Atlantic Ocean and the Baltic Sea.
Climatic zones- a latitudinal bands, each with relatively homogeneous climate,as determined by the amount of solar radiation and prevailing air masses.
When a warm air mass goes up, cold air masses replacing it cause winds.
In the kitchen, clean the air masses are the main guarantee of a true hostess health, because more than half of the home time she spends within the kitchen.
The continental zone is slightly larger, because continental air masses flow easily into the unobstructed Danubian Plain.
Moist Maritime air masses from the North Atlantic and the Baltic sea often bring quite changeable weather with precipitation and winds, especially in the offseason.
In But the central and western parts of the continent, these air masses have already come dehydrated, there is a lack of moisture.
Arctic air masses in the winter produce extreme minimum temperatures varying from- 54 °C in northern Alberta to- 46 °C in southern Alberta.
Field of second main components,reflects influencing the more warm air masses, coming in the given area from the low latitudes.
Its mountains protect it from the winter Arctic air masses that hit Russia, while its Caspian Sea protects it from the summer hot dry air found in Central Asia.
Bulgarian mountains and valleys make natural barriers or channels for air masses, which creates sharp contrasts in weather over relatively short distances.
The prevailing hot and dry continental air masses with large temperature during the day leads to a rapid destruction of rocks and formation of stones and sand.
These corners do not produce for the kitchen in the air masses harmful substances, their material is resistant to the formation of mildew and rot.
On the other hand for the car having swirl air masses and formed a sparse space, which creates additional resistance to movement.
In Slovakia, separated by mountains from Western oceanic air masses, the climate is more continental than in the Czech provinces, located in the West of the country.