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
Wiki User
∙ 13y agoThose terms likely stand for cT (constant temperature), cP (constant pressure), mT (monotonic temperature), and mT (monotonic temperature). They describe specific thermodynamic processes or conditions, such as how temperature or pressure remains constant during a process, or how temperature changes in a monotonic manner.
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 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.
Energy W is the ability to do work, W = -vp + cP where v is motion (velocity/speed) and p=h/w= mv is momentum. Force is the first derivative of energy, Force F = XW =[d/dr, DEL] [-vh/w, cP] = [ vp/r -cDEL.P, cdP/dr -DEL vh/w + cDELxP] F = cp/r[v/c -cos(P), -1P + v/c 1R + sin(P) 1RxP] Force = cp/r = cp/ct = p/t = mv/t = ma Motion is the change in position per unit time and is related to Force and Energy.
The four main types of air masses that affect weather are continental polar (cP), maritime polar (mP), continental tropical (cT), and maritime tropical (mT). These air masses differ in temperature and moisture content based on their source region, and they play a significant role in shaping weather patterns when they interact.
Metric Tonnes=1016 kg One tonne is 1000kg, or 1 megagram. The prefix of a lowercase 'm' indicates milli- or one thousandth, so mt would be a millitonne. A thousandth of a tonne is a kilogram, as kilogram is the base unit of mass millitonnes would never be used, they would always be called kilograms.
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.
YES
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 main air masses that affect Ontario are the continental polar air mass from the north and the maritime air mass from the southeast. The continental polar air mass brings cold, dry air during the winter, while the maritime air mass brings warmer, more humid air during the summer. These air masses can lead to dynamic and sometimes unpredictable weather patterns in the region.
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.
A tornado forms when warm, moist air at the surface rises and meets cooler, dry air in the atmosphere, creating instability. As the warm air rises and cools, it can begin to rotate due to wind shear in the atmosphere. When this rotation becomes strong enough, it can develop into a tornado.
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.
Hartford, CT Honolulu, HI Helena, MT Harrisburg, PA
Continental polar CP and Marine time Tropic MT
A wet cold air mass would be called a maritime polar air mass. These air masses originate over bodies of water and bring cool, damp conditions when they move over land.
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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.