What weather is generally controlled by the subtropics?

Regions controlled by subtropical highs are often sunny and hot. The eastern part of the subtropical high is an area of ​​strong subsidence. The downdraft is warmed due to adiabatic compression, and the control area will experience continuous sunny and hot weather. The reason is that the eastern part of the subtropical high pressure is an area of ​​strong subsidence movement. The downdraft is warmed due to adiabatic compression, and the control area will experience continuous sunny and hot weather. The western part of the subtropical high is a moving area where low-level warm and humid air converges and rises, and thunderstorms are prone to occur. As the seasons change, the intensity and location of the subtropical high pressure belt will change significantly. From January to July, the main body of the subtropical high moves northward and westward, and its intensity increases. From July to January, the main body of the subtropical high moves southward and eastward, and its intensity weakens. This seasonal change also has distinct stages of slow change and sudden change. Distribution pattern of subtropical high pressure area The subtropical high pressure area is the warm high pressure in the subtropical region. Located near 30 degrees north and south latitude. This high-pressure belt is the dividing line between the prevailing westerly belt and the easterly belt, and its high-latitude side is the westerly belt. Controlled by the subtropical high pressure, the weather is sunny, and there is a southwest airflow jump control area (Guanyu area) on its northwest side. The high pressure between the tropics and extratropics is called the subtropical high, and the high that controls the Pacific is often called the Pacific subtropical high.

It changes with the seasons, generally moving between 10° and 40 N