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How do the wet and dry monsoons affect southeast Asia?

Wet Monsoon

- The wet monsoon brings very heavy rainfall (more than 250 mm per month) to Southeast Asia between May and September.

- This heavy rainfall is caused by the warm, moist air that rises from the Indian Ocean and flows over the region.

- This rainfall is essential for agriculture in the region, and it also supports a wide variety of plant and animal life.

- High temperatures

- Increased cloudiness

- Higher winds

Dry Monsoon

- The dry monsoon occurs between November and March.

- During the dry monsoon, Southeast Asia experiences very little rainfall, and the air is much cooler and drier.

- This is because the winds from the Indian Ocean are weaker during this time of year, and they do not carry as much moisture.

- Lower temperatures

- Decreased cloudiness

- Decreased winds

- Lack of rainfall can cause drought

The wet and dry monsoons have a significant impact on the climate and environment of Southeast Asia.

- The heavy rainfall during the wet monsoon can cause flooding and landslides.

- The lack of rainfall during the dry monsoon can cause droughts and wildfires.

The monsoons also play an important role in the region's economy and agriculture.

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