The reason why Cherrapunji became the rain pole is

The reason why Cherrapunji becomes the rain pole is that it is located on the windward slope of the Himalayas. The warm and moist airflow from the Indian Ocean meets the terrain and rises, forming abundant orographic rain. There are high mountain barriers on the east, west and north sides, especially the Himalayas in the north, which block the hot and humid airflow blown by the southwest monsoon from the ocean, forcing the airflow full of water vapor to rise, causing Cherrapunji to become the world's rain pole.

Introduction to Cherrapunji:

Cherrapunji is located on the southern slope of the Himalayas, about 1,150 meters above sea level. The topography here is special, it is a natural depression, like a funnel, allowing warm and moist airflow from the Indian Ocean to gather here. When the monsoon season comes, warm and humid air currents from the Indian Ocean are continuously transported here, forming a large amount of orographic rain.

The reason for the heavy rainfall in Cherrapunji:

The reason why Cherrapunji has such heavy rainfall is also related to its geographical location. It is located on the windward slope of the warm and humid air currents in the Indian Ocean. This special position allows the warm and humid air currents from the Indian Ocean to be lifted here. When the water vapor cools, it condenses into raindrops, forming a large amount of rainfall.

The topography of Cherrapunji also contributes to the formation of rainfall. There are many ridges and ravines here, and the terrain is rugged, which hinders the flow of warm and moist air here and is forced to rise, resulting in more rainfall.

Based on the above factors, Cherrapunji has become one of the regions with the richest rainfall in the world, with an average annual rainfall of 11,684 mm.

Characteristics of Yuji:

1. Huge rainfall:

The average annual rainfall in Yuji usually exceeds 2000 mm, and some even exceed 4000 mm. . This means that at the rain pole, a large amount of water vapor accumulates and forms rainfall every year.

2. High humidity:

Due to the huge amount of rainfall in the rain pole, the humidity in the air is often very high. This makes the weather in the rainy pole usually relatively muggy, and the high humidity also makes it easier for water vapor to condense in the air and form rainfall.

3. Rainy periods and dry periods are obvious:

The rainfall in the rainy pole is usually concentrated in specific seasons. For example, during the monsoon season, warm and humid air currents bring a large amount of water vapor from the ocean, forming Continuous rainfall. In other seasons, the rainy season may enter a dry period, with significantly less rainfall.

4. Influence of terrain and climate:

Rain poles are usually located in places with special terrain, such as the windward slopes of mountains or low-lying areas. These terrains block warm and moist airflow here and force it to rise, resulting in more rainfall. At the same time, climatic factors such as monsoons and ocean currents also have an important impact on the formation of rain poles and rainfall amounts.