As the land surface heats up in summer, it generates a thermal low pressure. Air from the relatively high-pressure region over the ocean blows into this thermal low. This is called the <u>monsoon.</u>
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<h3><u>A Monsoon: What Is It?</u></h3>
A monsoon is a change in wind patterns that frequently results in either a very wet or a very dry season. Although monsoons are typically associated with sections of Asia, they can occur in many tropical and subtropical climates, including numerous locations in the United States.
<u>What triggers a monsoon?</u>
A seasonal change in the winds is what triggers a monsoon. The seasonal differences in land and water temperatures cause the winds to fluctuate. For instance, the ground warms up more quickly than bodies of water at the start of summer. The direction of the monsoon winds is always from chilly to warm. In the summer, conditions arise that cause the wind to blow in the opposite direction.
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If your result can be repeated.
The country in Europe that has marine west coast climate is Ireland
Explanation:
The marine west coast climate is one of the major climate types according to Koppen's climate classification. This climate type is mostly dictated by the sea. In Europe, the marine west coast climate can be found in a surprisingly high latitude, and the main reason for that are the warm ocean currents. The warm ocean currents of the Atlantic are running along the western coast of Europe, and they manage to have huge influence on the climate of the region.
- This climate type can be found at lower elevations and hills in Western Europe.
- The climate is warmer than it should be considering the latitude where this climate type is found in Europe.
- The summers are mild to warm, the springs and autumns mild to cold, while the winters are cold.
- The temperature extremes in both winter and summer are usually absent, and the climate is much more balanced.
- There is high amounts of precipitation throughout the whole year.
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