first go get a science book and read it
Maritime tropical air masses affecting North America usually originate over the warm waters of the Gulf of Mexico and the Caribbean Sea. These air masses bring warm and moist air to regions along the Gulf Coast and eastern U.S., influencing weather patterns in those areas.
Uplift in the atmosphere can be caused by several factors, including convergence of air masses, orographic lifting as air is forced to rise over mountains, frontal boundaries where warm air rises over cold air, and convection due to heating of the Earth's surface. These processes lead to the formation of clouds and precipitation.
Maritime tropical and marine polar air masses are both maritime in nature, meaning they originate over bodies of water. They differ in temperature, with maritime tropical air masses being warm and humid, while marine polar air masses are cool and moist. Both air masses can influence weather patterns and bring changes in temperature and precipitation when they move over land.
Mountains are created in several ways. The most common way is when tectonic plates crash into one another. The major land masses of Earth move and crash into each other. Crash isn't the best word because it suggests something happening suddenly. This process takes millions of years. As one of the enormous land masses collides with another they do so with huge forces this cause one to slide under the other. This collision both lifts and pushes into the other. This pushing into the edge creates wrinkles. These wrinkles are the mountain ranges. The Andes, Alps, Appalachian and Himalayas and several others were formed this way
An arctic air mass is a mass of cold air that originates from the Arctic region and is characterized by very cold temperatures and high humidity. These air masses form over the polar regions which are characterized by snow and ice cover throughout the year and they can often spread southward to affect mid-latitude regions. Arctic air masses are usually very stable and move slowly meaning that they can last for long periods of time. They can also be quite dry and they often bring cold weather and snow to the regions they affect.Arctic air masses are typically classified according to their temperature and moisture content. The following are the three main types of arctic air masses: Polar Maritime (Pm): These air masses form over the Arctic Ocean and are usually moist with temperatures ranging from -5 to +5 degrees Celsius. Polar Continental (Pc): These air masses form over the continent of North America and are usually dry with temperatures ranging from -20 to -30 degrees Celsius. Polar High (Ph): These air masses form over the high Arctic and are usually dry with temperatures ranging from -30 to -50 degrees Celsius.Arctic air masses can cause a variety of weather phenomena including snowstorms blizzards and extreme cold waves. They can also cause a drop in temperatures in affected areas resulting in frost and even freezing temperatures. As such it is important to be aware of arctic air masses and their potential impacts on weather and climate.
Yes they impede the flow of the sir masses moving over them.
Air masses can affect the weather because different air masses differ in temperature, density, and moisture content.
becuse
The wind blows the clouds over a human who is blowing up themountain for granite and the clouds rain and the human stops. Wind doesn't really do much to mountains, it's possible it could start an avalanche.
The force that builds up mountains and land masses is called tectonic forces, specifically the movement of tectonic plates. When plates collide, they can push against each other, creating mountains through processes like folding and faulting. This gradual process of plate movement and collision over millions of years results in the formation of entire mountain ranges and land masses.
Maritime Masses form over water.
Continental Masses form over Land.
i think that because the climates change from the atmosphere ;* <3 .
Wind is blowing air up over the mountain. Going from about 1,000 feet at the base to 7,000 feet at the top, the temperature changes as the air goes over the mountain.
they are over land
they are over land
they are over land