thankfully we are seeing a break from the heat and humidity this week. The maritime tropical atmosphere mass that had us in its bobby pin stopping point week is being shoved bet on towards the south…for now. What is this vent mass and why does it get then hot and humid when it is around ? Read on for the explanation .
Characterizations of a Maritime Tropical Air Mass
| Temperature | Moisture |
| Warm | Moist |
The two words that best characterize this air mass are warm (80F-90F in the summer) (70F-80F in the winter) and damp (dew points greater than 50F year-round). equally far as constancy is concerned this vent mass is identical unstable and light. This leads to the development of changeable weather .
Development and Source of Air Mass
The maritime tropical atmosphere mass develops in warm ocean waters located in the tropics and subtropics. These types of air masses thrive in the South Atlantic, South Pacific, and indian Oceans. Most of our machine translation air out masses originate in the waters of the Gulf of Mexico and the Gulf Stream. The warm bodies of water warm the overlying air and constantly supply it with plenty of rich moisture .
Where Do Our Air Masses Originate?
All of the incoming solar radiation allows these waters to stay very warm throughout the year. During the winter months, the montana air travel aggregate is kept away from the continental United States. The reason is the about constant onslaught of cold air that we see push down from Canada.
What Type of Weather Can You Expect?
due to its very damp and precarious nature, this vent mass is responsible for most of the country ’ s thunderstorm activeness. Remember that a thunderstorm needs a warm and damp environment to form. The nautical tropical tune mass provides both of those conditions. In fact, most of the United States ’ rain comes from the presence of these publicize masses.
even without the thunderstorms imprint, this publicize mass is noticeable. You only need to step out the door to notice the very humid nature of the maritime tropical tune aggregate. This is the air mass responsible for the trio h ’ s presently plaguing the region. The trio h ’ mho are bleary, hot, and humid conditions.
View of the Grip of a Maritime Tropical Air Mass on the River Valley from our Mount Magazine Magtel Co. Cam.
Modification of the mT Air Mass
As the maritime tropical atmosphere mass moves inland it starts to change its characteristics. The biggest change is in the moisture message. The maritime tune mass starts to become drier the further and farther north it tracks. The atmosphere inland tends to be much drier due to several factors such as lower sunlight lean, less moisture available, and cool land. Often the meitnerium starts to take on more continental tropical ( connecticut ) publicize mass characteristics over fourth dimension. We will explore the connecticut air aggregate in a separate Weather 101 .
For early stimulate and interest digital weather contented, check out other Weather 101 and Weather Blog pieces .