they both are over colder land but maritime polar is over water in cold areas and continental polar is over land and in colder areas.
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.
The terminology here is a bit confused. In weather there are 4 basic types of large-scale air mass: Continental polar air masses come off the land in cold regions and are cool and dry. Maritime polar masses come off the ocean and are cool and somewhat moist. Continental tropical air masses come of the land from warm regions and are warm and dry. Finally maritime tropical masses come off of warm oceans and are warm and moist. When a continental polar air mass pushes into a maritime tropical air mass it forms a cold front. Since cold air is denser than warm air, the tropical air mass is forced upwards. This can trigger thunderstorms. Under the right conditions these storms can produce tornadoes.
The darker the shade of the surface texture, the lower the albedo percentage. Antarctica for instance has an albedo around 60% changing seasonally. Due to the light colour, the surface reflects at a higher rate then a tropical forest. Tropical Forests are hot and humid due to the lack of moisture in the air due to the low amount of reflectivity and the high amount of heat absorbed. Albedos are the key to climate and global warming. Therefore Tropical places have albedos of low percentage. Due to the dark colour of the forests and shadows the trees form. Therefore Polar Areas have high albedos due to the light shade of white which is perfect for reflecting heat. Fresh Snow has a reflect rate of 90%.
Both Earth and Mars have atmospheres composed primarily of carbon dioxide. They both experience weather patterns and have polar ice caps. However, Earth's atmosphere is significantly thicker and has more oxygen than Mars.
Hot dry air moves into the southwest in summer from the desert areas to the south and east, such as the Sonoran Desert and the Mojave Desert. This air mass brings high temperatures and low humidity to the region, contributing to the hot and arid conditions characteristic of the area during the summer months.
Four types of air masses that can affect the United States are continental polar (cP), maritime polar (mP), continental tropical (cT), and maritime tropical (mT). These air masses vary in temperature and moisture content, influencing the weather patterns when they move across the region.
maritime polar, maritime tropical, continental polar, and continental tropical
Maritime polar, maritime tropical, continental polar, & continental tropical
Maritime polar and tropical, continental polar and tropical.
continetal polar, maritime polar, continental tropical, and maritime tropical are the 4 air masses.
Maritime polar air masses bring cool and humid weather. These air masses originate over cold ocean waters and bring moisture with them, leading to cooler and more humid conditions as they move over land.
The six major air masses that influence weather in the United States are Continental Polar (cP), Continental Tropical (cT), Maritime Polar (mP), Maritime Tropical (mT), Arctic (A), and Equatorial (E). These air masses vary in temperature and moisture content, affecting weather patterns across the country.
they are both alike because they both are over water. they are different because the polar brings cold air and the tropical brings warm air.
Compared to a maritime tropical airmass, a maritime polar airmass has lower temperature and less water vapor.
The four are Maritime tropical, Continental tropical, maritime polar, and Continental polar
The four are Maritime tropical, Continental tropical, maritime polar, and Continental polar
Types of air masses that are characterized by their temperature and humidity characteristics. Continental polar and maritime polar air masses are cold and moist, while continental tropical and maritime tropical air masses are warm and humid. These air masses determine the weather conditions when they interact with each other.