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There are many types of wind, such as:Tornado, typhoon, wind, monsoon, natural wind, light, soft wind, breeze, gale, strong wind, etc.
1. Tornado:
A tornado is a vortex: the air rotates rapidly around the axis of the tornado, attracted by the extreme decrease in the air pressure in the center of the tornado, and in a thin layer of air tens of meters thick near the ground, the air flow is drawn into the bottom of the vortex from all directions.
It then becomes an axial vortex, and the wind in the tornado is always cyclonic, and the pressure in its center can be lower than the pressure in the surroundings.
Ten percent. A tornado is a thunderstorm in the clouds.
products. Specifically, a tornado is a form in which a small portion of a thunderstorm's enormous energy is released in a concentrated area over a small area.
2. Typhoon: Typhoon is a tropical ocean that occurs in the Northwest Pacific Ocean and the South China Sea.
on the violent storm. You must have seen eddies in rivers from time to time, but in fact, typhoons are air vortices that rotate rapidly around their center in the atmosphere and move forward at the same time.
It is in the Northern Hemisphere.
Rotate in a counterclockwise direction and in a clockwise direction in the southern hemisphere. Meteorologists refer to atmospheric vortices as cyclones, and typhoons are called tropical cyclones because they occur in the tropical ocean.
3. Monsoon: Due to the different degrees of heating and cooling between the continent and the ocean, the monsoon is called the monsoon when the wind direction changes regularly with the seasons due to the different degrees of heating and cooling between the continent and the ocean.
The most fundamental reason for the formation of monsoons is due to the different properties of the earth's surface and the difference in thermal response. It is distributed by land and sea, and the atmospheric circulation.
Due to the large terrain and other factors, the phenomenon of opposite wind direction prevails in a wide range of winter and summer seasons with a cycle of one year.
The role of the wind:
1. Wind energy promotes the exchange of dry and cold and warm and humid air, wind is a natural energy source, people also use windmills to generate electricity, and sailboats are also driven by wind.
2. The wind does a lot of work in nature. Wind energy mixes and balances a wide range of heat and water vapor, and regulates the temperature and humidity of the air; It can send clouds and rain to distant places and circulate water on the earth.
It was done. 3. The soft breeze helps plants to disperse pollen, so that some cross-pollinated plants can get the necessary pollen, so that plants can "start a family", form seeds, bear fruits, and leave the next generation for plants. The wind can also blow the seeds of some plants to distant places, allowing them to grow and develop in their new environment and continue to thrive their "new family".
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Wind can be classified according to different classifications.
Depending on where it is generated, wind can be divided into land breeze, sea breeze, mountain breeze, and valley breeze.
Based on speed, winds can be classified as breezes, vicious winds, tornadoes, etc.
Depending on the direction, the wind can be classified into north, south, west, easterly, etc.
Depending on the season, winds can be classified into monsoons, gusts, etc.
According to the characteristics of the airflow, winds can be divided into cyclones, foehns, typhoons, monsoons, trade winds, etc.
In conclusion, the types of wind are very diverse.
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There are 6 types of wind, namely: gusts, cyclones, foehns, typhoons, monsoons, and trade winds.
1. Gusts of wind. Gust of wind refers to when the speed of air flow is large and small, the wind will become suddenly big and small, and there will be a gust of feeling on people's body, which is the gust of wind recognized in life.
2. Whirlwind. A cyclone is when the air carries dust and flies through the air to form a whirlpool.
3. Foehn. Foehn refers to a type of warm and dry wind that tends to occur on a leeward slope as the air sinks when the air crosses the ridge.
4. Typhoons. An atmospheric vortex occurs in a tropical ocean, so it is also called a tropical cyclone.
5. Monsoon. With the change of seasons, the prevailing winds change in a regular manner. In winter, air flows from high-pressure land to low-pressure sea, which is called the winter monsoon; In summer, the wind blows from the sea to the land, which is called the summer monsoon.
6. Trade winds. In the lower atmosphere, persistent winds blowing from the subtropical high over a wide area of the equatorial region. In the Northern Hemisphere, the trade winds prevail in the northeast; In the Southern Hemisphere, it is the Southeast.
Trade winds are characterized by being highly regular, blowing in one direction with almost constant force throughout the year.
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Sea and land winds, typhoons, foehn winds, prevailing winds, monsoons, valley winds.
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Whirlwind: When the air carries dust and flies in the air to form a whirlpool;
Foehn winds: When the air crosses a ridge, a warm and dry wind tends to occur on the leeward slope due to the sinking of the air;
Typhoon: An atmospheric vortex that occurs over a tropical ocean. When the maximum wind force in the center of the vortex reaches more than 8, it is called a typhoon;
Tornado: A small, destructive air vortex that extends from a cumulonimbus cloud to the ground. What happens on land is called a landspout, and what happens on the ocean is called a seaspout;
Valley wind: In the mountains, the wind blows up along the slopes and valleys during the day, and down the slopes and valleys at night. This kind of wind between the hillside and the valley, which changes the direction of the wind with the alternation of day and night, is called the valley wind;
Sea and land breeze: In the coastal area, the wind blows from the sea to the mainland during the day, and blows from the land to the sea at night.
Glacial winds: shallow winds that blow along the downslope of a glacier during the day and at night;
Monsoon: The wind that changes its direction regularly with the change of seasons;
Trade winds: persistent winds blowing from the subtropical high in the lower atmosphere over a wide area of the equatorial region;
Anti-trade winds: The hot air rising at the equator reaches the upper layers of the atmosphere and flows in two stages, which is called anti-trade winds.
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