continental tropical
A high pressure system usually produces these conditions in winter. Continental polar (apex)
A warm and humid air mass, commonly known as a maritime tropical air mass, can bring thunderstorms to the US during summer. This type of air mass holds a lot of moisture, providing the necessary ingredients for thunderstorm development when it interacts with other weather systems.
in summer it can cover much of the US east of the Rockies. This air mass results from the warm waters of the Gulf of Mexico and Gulf Stream. The warm waters in this region evaporate an enormous volume of water. Cold water currents tend to stabilize the atmosphere and produce little evaporation while warm waters destabilize the atmosphere and add moisture. The warm waters warm the low levels of the atmosphere.
A steep slope with loose, unconsolidated material is more likely to produce mass movements due to the force of gravity. Higher precipitation levels and seismic activity can also increase the likelihood of mass movements on slopes.
air-mass weather
Continental Tropical
The maritime tropical (mT) air mass is responsible for producing warm, humid weather in summer. Originating over warm ocean waters, this air mass carries moisture and warmth, leading to higher temperatures and increased humidity levels when it moves inland. Regions affected by mT air masses often experience muggy conditions, which can contribute to thunderstorms and heavy rainfall during the summer months.
continental polar
A high pressure system usually produces these conditions in winter. Continental polar (apex)
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A warm and humid air mass, commonly known as a maritime tropical air mass, can bring thunderstorms to the US during summer. This type of air mass holds a lot of moisture, providing the necessary ingredients for thunderstorm development when it interacts with other weather systems.
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A continental tropical air mass originating from the desert regions of northern Mexico and the southwestern United States typically causes hot, clear, and dry summer weather in the U.S. This air mass brings high temperatures and low humidity, leading to the development of heatwaves and drought conditions.
A warm, dry air mass is typically associated with a continental tropical (cT) air mass, which originates over land in warm regions, such as deserts. This air mass is characterized by high temperatures and low humidity, leading to clear skies and little precipitation. Another contributor to warm, dry weather can be a continental polar (cP) air mass during certain conditions; however, it is not as warm as a cT air mass.
North Carolina's weather is most affected by two primary air masses: the maritime tropical (mT) air mass, which originates from the warm, moist waters of the Gulf of Mexico and the Atlantic Ocean, and the continental polar (cP) air mass, which comes from the cold, dry regions of Canada. The mT air mass typically brings warm, humid conditions and precipitation, especially in summer, while the cP air mass can lead to cooler, drier weather during the winter months. Additionally, the continental tropical (cT) air mass can influence summer weather with hot, dry conditions. These air masses interact to create the state's varied weather patterns.
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