cT= continental Tropical
cP=continental Polar
mT=maritime Tropical
there is also :
mP=maritime Polar
cA=continental Arctic
c(continental)=dry/not very humid
m(maritime)=wet/humid
T(Tropical=warm
P(Polar)=cold
A(Arctic)=very cold
these are all terms used during a weather topic
The five types of air masses that affect weather in the U.S. are Continental Polar (cP), Maritime Polar (mP), Continental Tropical (cT), Maritime Tropical (mT), and Continental Arctic (cA). cP air masses bring cool, dry conditions, while mP air masses are cool and moist. cT air masses are hot and dry, and mT air masses are warm and humid. cA air masses, which are less common, are extremely cold and dry, primarily influencing weather in the northern regions.
Cold polar (cp) air masses are characterized by lower temperatures and lower humidity, as they originate from cold regions. In contrast, maritime tropical (mt) air masses are warmer and more humid, having formed over warm ocean waters. This difference in temperature and humidity can significantly impact weather patterns, with cp air leading to cooler, drier conditions and mt air contributing to warmer, more humid weather.
The air masses that have the greatest influence on weather conditions in the Midwestern US are continental polar (cP) air masses in winter and maritime tropical (mT) air masses in summer. These air masses bring contrasting temperature and moisture conditions that can lead to significant weather events like thunderstorms, snowstorms, and severe weather.
cP (continental Polar) air masses are characterized by cold temperatures and low humidity, as they originate over land in polar regions. In contrast, mT (maritime Tropical) air masses are warm and humid, originating over warm ocean waters in tropical regions. The key difference lies in their temperature and moisture content, with cP being cold and dry, while mT is warm and moist. This distinction significantly impacts weather patterns when these air masses interact.
cP (continental polar) air masses bring cold and dry weather to much of the US during the winter, leading to low temperatures and clear skies. On the other hand, mT (maritime tropical) air masses bring warm and moist conditions during the summer, leading to higher temperatures and increased chances of thunderstorms and heavy rainfall.
The four letters used to describe air masses in weather maps are cP, cT, mP, and mT. "c" represents continental (dry) air, "m" represents maritime (moist) air, "P" represents polar air, and "T" represents tropical air.
California is primarily affected by four air masses: maritime tropical (mT), continental tropical (cT), maritime polar (mP), and continental polar (cP). The mT air mass, originating from the Pacific Ocean, brings warm, moist conditions and is responsible for much of the state's precipitation, especially in winter. The cT air mass from the desert Southwest contributes hot, dry weather, particularly in summer. Meanwhile, the mP and cP air masses can lead to cooler temperatures and increased cloud cover, especially during winter months in Northern California.
YES
Cold polar (cp) air masses are characterized by lower temperatures and lower humidity, as they originate from cold regions. In contrast, maritime tropical (mt) air masses are warmer and more humid, having formed over warm ocean waters. This difference in temperature and humidity can significantly impact weather patterns, with cp air leading to cooler, drier conditions and mt air contributing to warmer, more humid weather.
The primary air masses that influence the weather in North America are the continental polar (cP) air mass originating from Canada, bringing cold and dry conditions, and the maritime tropical (mT) air mass from the Gulf of Mexico, bringing warm and moist conditions. These air masses interact and can result in a variety of weather patterns across the continent.
The 4 major air masses are continental polar (cP), continental tropical (cT), marine polar (mP) and marine tropical (mT). Generally, continental air masses are drier than marine air masses, and polar air masses are cooler than tropical air masses. cT air masses are relatively limited in distribution existing in the south west North America and North Africa.
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The air masses that have the greatest influence on weather conditions in the Midwestern US are continental polar (cP) air masses in winter and maritime tropical (mT) air masses in summer. These air masses bring contrasting temperature and moisture conditions that can lead to significant weather events like thunderstorms, snowstorms, and severe weather.
Continental polar CP and Marine time Tropic MT
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There are five main types of air masses: continental polar (cP), continental tropical (cT), maritime polar (mP), maritime tropical (mT), and arctic. Each air mass has distinct characteristics based on its temperature and humidity, influencing weather patterns when they interact with each other.
A cP (continental polar) air mass is cold and dry, resulting in lower air temperature and humidity levels. On the other hand, an mT (maritime tropical) air mass is warm and moist, leading to higher air temperature and humidity levels. This contrast in characteristics can influence weather patterns when these air masses interact.