- 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.