over a polar ocean region
A hot air mass that forms over land is called a continental air mass.
A continental tropical air mass typically brings dry and hot weather to the areas it moves over. This air mass originates over hot and arid regions, leading to high temperatures and low humidity.
No, hot air does not weigh more than cold air. In general, air at different temperatures still has the same mass per unit volume, or density. The weight of a given volume of air depends more on its mass and not on its temperature.
Continental Polar cP air mass is an air mass formed over land in a cold region with cold dry airMaritime tropical mT air mass is an air mass that forms over water in a warm region with warm wet air
Yes, the continental tropical air mass often forms over Mexico during the summer months, bringing dry and hot air to the southwestern United States. This air mass originates from the hot desert regions of northern Mexico and can lead to high temperatures and a lack of moisture in the affected areas.
This refers to a continental, tropical air mass. It is typically hot and dry.http://cimss.ssec.wisc.edu/wxwise/class/frntmass.html
A hot and dry air mass is typically associated with a continental tropical air mass. These air masses form over hot, arid regions and are characterized by high temperatures and low humidity levels.
A hot air mass that forms over land is called a continental air mass.
heat rises
a cold air mass colliding with a hot air mass
A continental tropical is a very hot and dry air mass produced over subtropical arid regions. A continental tropical air mass is found in the Southwest portion of the United States.
the hot and dry air mass are most likely to rise
Hot, dry and low pressure forms over hot deserts. Known as a tropical continental air mass.
Hot air has less mass which make it less dense, thus allowing it to rise over a cold air mass.
When air is heated, that volume of air expands (which is why hot air balloons go up). The hot air has changed in volume, but it is still the same mass.
The hot and dry air mass is most likely to move in the direction where lower pressure systems exist. This typically means that it will move towards areas with cooler temperatures or where moist air masses are located.
A hot air balloon behaves like an air mass in a high pressure area when it is descending. As the balloon descends, it enters a region of higher atmospheric pressure where the surrounding air is denser. This denser air can cause the hot air balloon to slow down and even sink if it cannot maintain its buoyancy.