Over Northern Canada , North Pacific Ocean , and North Atlantic Ocean.
What causes changes in the weather? The movement and interactions of air masses changes the weather.
The Arctic air masses that come from the Arctic region cause cold waves over the central and eastern United States. These air masses bring bitterly cold temperatures and can result in severe winter weather events such as snowstorms and blizzards.
Changes in weather patterns are often caused by the movement of air masses. These air masses can vary in temperature, humidity, and pressure, and when they collide or interact with each other, it can lead to changes in the weather, such as the formation of storms or changes in temperature.
When air masses with different temperatures and humidity levels meet, they can create weather fronts. These boundaries can lead to the formation of storms and changes in weather conditions as the air masses interact and mix.
The temperature and density of the air masses. the air masses moves when hot air and cold air gets together
the thing that causes it is that masses of air would stay and change the weather of that specific weather
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maritime tropical (M.T)
As the seasons change, they cause the weather to change also. For example, if the season is Winter then the weather will be colder because in Winter the Earth is facing further away from the Sun. But if it is Summer, then the weather will be warmer, because the Earth is closer to the Sun, making the atmosphere warmer.
All fronts involve the meeting of two air masses with different characteristics, leading to the formation of weather phenomena such as rain, thunderstorms, or snow. The type of weather associated with a front depends on the characteristics of the air masses involved, such as temperature, humidity, and air pressure.
The primary cause of most weather and climate is differences in temperature and air pressure. These differences drive the movement of air masses and the formation of weather systems such as storms, fronts, and winds. The uneven heating of Earth's surface by the sun is the main driver of these temperature and pressure variations.
Low latitudes, closer to the equator, tend to have warm air masses in summer due to more direct sunlight and high temperatures. High latitudes, closer to the poles, tend to have cold air masses in winter due to limited sunlight and low temperatures.