This refers to a continental, tropical air mass. It is typically hot and dry.http://cimss.ssec.wisc.edu/wxwise/class/frntmass.html
An air mass that forms over the southwestern US is typically designated as "cT" (continental tropical). This air mass is characterized by its high temperatures and dry conditions.
An air mass classified as cT usually forms over hot and dry desert or semi-arid regions, such as in the southwestern United States or northern Mexico. It derives its characteristics from being a continental (c) air mass and originating from the tropics (T).
A continental tropical (cT) air mass is associated with low relative humidity and high air temperature. This air mass originates over hot, dry land areas and brings warm, dry conditions when it moves into a region.
The warm air mass that develops over land influencing weather in the US is the continental tropical air mass. It forms over warm, dry areas and brings hot and dry conditions to the region it affects.
A warm air mass that influences the weather in the US and develops over land is called a continental tropical (cT) air mass. This air mass originates over the southwestern United States and northern Mexico, bringing hot and dry conditions to the region it moves into.
A cT air mass refers to a type of air mass classification. The lowercase "c" stands for continental, or dry, while the uppercase "T" stands for tropical.
An air mass that forms over the southwestern US is typically designated as "cT" (continental tropical). This air mass is characterized by its high temperatures and dry conditions.
In weather terms, "cT" typically refers to a "continental tropical" air mass. This air mass originates from dry desert regions and is characterized by being hot and dry. When a cT air mass moves into an area, it can bring high temperatures and low humidity.
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cT represents a continental tropical air mass, which is warm and dry in nature. This air mass typically forms over desert regions and brings hot and dry conditions when it moves to other areas.
cT
it is the continental tropical (cT)
The air mass designated as "CT" refers to Continental Tropical air mass. It originates over warm, dry land areas, typically in the subtropics, and is characterized by high temperatures and low humidity. This type of air mass can bring hot and dry conditions to regions it affects, often leading to warm weather and clear skies.
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.
No, that would be continental tropical.
ct
The air mass associated with low relative humidity and high air temperature is typically classified as a continental tropical (cT) air mass. This type of air mass forms over warm, dry land regions, leading to high temperatures and low moisture content. cT air masses are common in areas such as deserts and can influence weather patterns, often resulting in hot and dry conditions.