Примери коришћења Air masses на Енглеском и њихови преводи на Српски
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Fronts and air masses.
The climatic area of the Ibar valley is influenced by continental air masses.
Why are Colliding Air Masses Significant?
Hills and mountains can also block coastal air masses.
Above and around us, the air masses are always on the move;
The simplest classification is that involving air masses.
A front is the boundary between air masses of different temperature and humidity.
A front is a boundary line between 2 different air masses.
Fronts are boundaries between two air masses of different temperature and density.
These air masses enter the country in different ways thanks to its varied geography.
Depending on the territorial location, air masses can exert pressure in different ways.
Colder air masses are called polar or arctic, while warmer air masses are called tropical.
A weather front is the boundary zone between two distinct air masses with different features.
In atmospheric science, large air masses in the atmosphere often function as thermal reservoirs.
At the same time, the sea moderates the influence of hot and dry air masses coming from Central Asia.
Weather fronts separate air masses with different density(temperature and/or moisture) characteristics.
Cold air- A jet stream at high altitude brings cold,dry air masses from the West.
How those upper-level air masses translate into temperatures on the surface is a different story.
A similar air mass rising on the other side of the equator forces those rising air masses to move poleward.
Even during winter period,the Atlantic humid air masses bring rainy and snowy weather, rarely cold weather.
Air masses cover many hundreds or thousands of miles, and adapt to the characteristics of the surface below them.
The fan built into the unit will“drive” warm air masses around the perimeter, ensuring uniform heating of the room.
Different air masses that affect North America, as well as other continents, tend to be separated by frontal boundaries.
Bioclimatic and mechanical properties of the wind. Air masses and air fronts: Warm and cold air masses.
Subsiding, diverging, dry air masses associated with subtropical high pressure systems are extremely unfavorable for the development of convectional showers.
The city's climate is influenced both by dry(Central Asian/Siberian) air masses from the east and oceanic(Atlantic/Black Sea) air masses from the west.
Likewise, tropical hot air masses(subtropical anticyclone and southern cyclones), as well as Central Asian anticyclones and local weather conditions, have influence.
Unlike anywhere else, the unique combination of latitudinal position,distinctive topography, and varying air masses provides the United States, notably the Great Plains, with the world's ripest environment for tornadoes.
Continental and superior air masses are dry while maritime and monsoon air masses are moist.
Vojvodina possesses typical continental climate, with air masses from northern and western Europe which shape its climatic profile.