What Is the Tropical Monsoon Climate?
Are you looking for an easy way to teach your child about weather and climate? We’ve put together a set of free materials that parents and teachers can use right away. In this lesson, your child will dive into the fascinating world of tropical monsoon climate.
We’ll explore the distinctive temperature and rainfall patterns of this hot climate. Explore science in a more engaging way with captivating 3D videos and interactive quizzes. Download our app to get started!
Table of Contents
What you will learn from this lesson
- he skin has threeTropical monsoon has a rainy summer and a dry winter.
- Seasonal wind shifts cause wet and dry seasons.
- This climate is excellent for farming and growing crops.
What Are the Features of Tropical Monsoon Climates?
The tropical monsoon climate is characterized by high temperatures throughout the entire year. This consistently hot weather occurs because most of the regions with this climate are located in low latitudes, generally within 30° of the Equator. The annual rainfall in areas with this climate is abundant overall.
The distinct pattern of the tropical monsoon climate is defined by its seasonal precipitation. It experiences a rainy summer and a dry winter. These seasonal changes in rainfall are primarily caused by the wind patterns that shift between the ocean and the land.
How Do Monsoons Cause Rain and Dryness?
The seasonal wind shift is what creates the distinct wet and dry seasons.
- Summer: During the summer, the land has low air pressure, while the nearby ocean has high air pressure. This causes the wind to blow from the high-pressure ocean towards the low-pressure land. These ocean winds bring a large amount of water vapor, which results in abundant rainfall in the summer.
- Winter: In contrast, winter brings the opposite situation: the land has high air pressure, and the ocean has low air pressure. The wind then blows from the high-pressure land towards the low-pressure ocean. Since winds coming from the land carry little water vapor, the winter season is dry and receives less rain.
How Does This Climate Affect Crops?
The combination of year-round high temperatures and generally plentiful rainfall makes the tropical monsoon climate an excellent location for farming. The conditions are so favorable for agriculture that certain crops in these regions can be harvested up to three times within a single year.
Fun Fact
- Tropical monsoon regions stay hot all year because they are close to the equator (within 30 degrees latitude).
- Wind flows from high air pressure to low air pressure, which is what causes the seasonal monsoons.
- Summer monsoon winds travel from the high-pressure ocean to the low-pressure land, carrying lots of water vapor.
- The dry winter is caused by winds blowing from the land toward the ocean, which brings very little moisture.
- Farms in the tropical monsoon climate can sometimes harvest crops three times a year due to the plentiful heat and rain.
Vocabulary
- Tropical monsoon climate: A type of climate characterized by consistently high temperatures year-round and distinct seasonal changes in precipitation. It features a rainy summer and a dry winter.
- Precipitation: The term for the rainfall in the tropical monsoon climate, which is abundant overall. The seasonal pattern is defined by a rainy summer and a dry winter.
- Water vapor: Large amounts of this moisture are carried by winds blowing from the ocean toward the land during the summer. This process is what causes the abundant rainfall in the rainy season.
- Low air pressure: During the summer, the land has this condition, which is what attracts the wind from the high air pressure over the nearby ocean. It is a key factor in causing the rainy season.
- High air pressure: During the summer, the ocean has this condition, which causes the wind to blow toward the low air pressure over the land. In the winter, the land has this condition, causing the wind to blow toward the low-pressure ocean.