The more weather terms the better, and the more detailed they are!

Wind is the horizontal flow of air. Expressed by wind direction and wind speed: wind direction is divided into sixteen directions; wind speed is expressed by wind level or meters/second, and is divided into average wind speed represented by the average situation of 2 minutes and instantaneous wind speed represented by the instantaneous situation. The intensity of the wind is expressed by wind speed, which is generally measured by wind level or meters per second. It is divided into thirteen levels: Quiet wind: Level 0 wind. Zephyr: Level 4 wind. The wind speed is between 5.5-7.9m/s. Breeze: Level 3 wind. Strong wind: that is, level 8 wind. The average wind speed is 17.2-20.7m/s. Strong wind: Level 10 wind. Storm: Level 11 wind. The wind speed is between 28.5-32.6m/s. Hurricane: that is, winds above level 12. (Tropical cyclones with maximum surface winds of level 12 or above near the center are called typhoons in the northwest Pacific). Gust: a phenomenon in which the wind speed suddenly increases and decreases in an instant, sometimes accompanied by changes in wind direction, and lasts for a very short period of time. Black wind: a kind of strong sandstorm weather with strong instantaneous wind speed and extremely low visibility. Hot and dry wind: Agricultural meteorological disaster weather with high temperature, low humidity and a certain amount of wind. Cold dew wind: The intrusion of cold air in autumn causes significant cooling and reduces rice yield. Monsoon: The seasonal almost reverse rotation of prevailing wind direction within a year. Trade winds: Trade winds are large-scale airflows in the lower atmosphere that blow from the south side of the subtropical high pressure to the low pressure area near the equator. Sea Breeze: In coastal areas, the wind blows from the sea to the land due to the heating of the continental surface during the day. Land wind: In coastal areas, surface wind blowing from land to sea due to nighttime radiation cooling of the continental surface. Downburst: A strong downdraft that generally causes divergent disastrous winds on or near the ground. Wind shear: The spatial variation of the wind vector in a specific direction. Mountain wind: In mountainous areas, the wind blows from the slopes to the valley at night caused by thermal factors. Valley breeze: In mountainous areas, the wind blows from the valley to the hillside during the day caused by thermal factors. Squall: A sudden onset of strong winds that lasts only a short time. Often accompanied by thunderstorms. In layman's terms, a front is the interface between warm and cold air masses. The front is the interface between two air masses with different physical properties such as temperature and humidity, or it is called the transition zone. The intersection between the front and the ground is called the front, also referred to as the front. The length of the front is roughly the same as the horizontal distance of the air mass, ranging from hundreds to thousands of kilometers. The width is much smaller than the air mass, only tens of kilometers, and the widest is only a few hundred kilometers. The vertical height is equivalent to the air mass, ranging from several kilometers to more than ten kilometers. Fronts can also be divided into warm and cold, moving, and stationary. Wind shear is a dynamic instability phenomenon associated with discontinuous wind speeds on both sides between adjacent air layers. When an airplane flies through such an area, turbulence will occur. The greater the wind shear, the more turbulent the airplane becomes. Confining front: When a warm air mass, a colder air mass, and an even colder air mass meet, they first form two fronts, and then one of the fronts catches up with the other front, forming a confining front. What is common in our country is the terrain restriction caused by the front being blocked by mountains; or the restriction caused by a cold front catching up with a warm front, or two cold fronts meeting head-on. They force the warm air in front of the cold front to lift off the ground and trap it high in the sky. We call the interface between the cold air mass behind the cold front and the cold air mass in front of the front the confining front. Strong convection is the abbreviation for forced convection. Fluid convective movement caused by uneven temperature of the fluid caused by external heating or lifting. The most forced convection in the atmosphere is thermal convection. However, when air flows over mountains, the lifting effect caused by the convergence of weather systems can often also cause dynamic forced convection.