What kinds of weather systems are there?

According to the spatial distribution of meteorological elements, the atmospheric motion system with typical characteristics (usually refers to the system composed of the spatial distribution of atmospheric pressure), such as high (gas) pressure, low (gas) pressure, high pressure ridge, low pressure trough, etc. Sometimes it refers to the wind distribution system, such as cyclone circulation, anticyclone circulation, shear line and so on. Sometimes it refers to the system of temperature distribution, such as high temperature zone, low temperature zone, front zone and so on. Sometimes it refers to. Such as thunderstorms and tropical clouds. This element system often has a certain configuration relationship with another element system. The relationship between pressure system and wind field is good: low pressure and cyclone circulation are configured, sometimes called low pressure and sometimes called cyclone; High pressure and anticyclone are juxtaposed, sometimes called high pressure and sometimes called anticyclone. Pressure system and temperature system are often used together. For example, the juxtaposition of low pressure area and low temperature area is called cold low pressure or cold vortex; The juxtaposition of low pressure area and high temperature area is called thermal low pressure. The atmospheric pressure system can also be matched with weather phenomena, such as thunderstorms and (small) high pressure, which is called thunderstorm high pressure. The weather system can be analyzed by various weather maps and satellite cloud images. \x0d Various weather systems have a certain spatial range. A certain process of birth, change and extinction. Different stages of the development of various weather systems have their corresponding weather phenomena distribution. In the weather forecast, we can roughly predict the future weather changes by forecasting various systems. The combination of many weather systems constitutes a large-scale weather situation and constitutes a hemispheric and even global atmospheric circulation.