Which of the following contributes to the wet monsoon during the summer in South Asia?

Which of the following contributes to the wet monsoon during the summer in South Asia?

The summer monsoon is known for its copious rains. As winter comes to a close, warm, moist air from the southwest Indian Ocean travels to South Asia, while the summer monsoon delivers humidity and copious rain. The summer monsoon affects most areas of India except for the dry desert regions of Rajasthan and parts of Gujarat.

The region receives more than 320 millimeters (12.9 inches) of precipitation during the summer months. This makes the summer monsoon one of the world's most important sources of water supply. It also causes major flooding problems since most of this rainfall occurs over a few days and accumulates in relatively small areas of land. When the rains stop, as they often do before dawn, these flooded areas are easily visible from space.

The location of the intertropical convergence zone, or ICZ, plays an important role in determining which part of the world will have a monsoon. The ICZ is the area of low pressure that develops between Africa and Asia each year as cold air from the Arctic flows south toward the equator. As it moves south, the temperature drops until it reaches 32 degrees Celsius (90 degrees Fahrenheit), at which point it becomes saturated with water vapor from the oceans and clouds around it. If this low-pressure system forms over hot ocean waters, it may cause heavy rains and strong winds across South Asia.

Why is the monsoon so crucial to life in South Asia?

Monsoons always blow from cold to warm locations. The South Asian monsoon season is critical to the region's crops and lives. Without these rains, there would be no food for the hundreds of millions of people who live here.

The monsoon affects everyone in South Asia, but it has special needs for farmers. A farmer must have good soil for successful planting. If it is too dry, the seeds will not grow. If it is too wet, the plants may drown. In between these two extremes is the right level of moisture. Too much water can cause the ground to become soggy and promote diseases such as rice sheath blight. Not enough water leads to drought, which can damage or destroy entire fields.

During the rainy season, rivers swell and overflow their banks. Flooding can cause severe damage to homes, businesses, and roads. It can also kill livestock and contaminate drinking water sources. Communities need safe places to go during a storm, so they can protect themselves from falling trees and other hazards. National governments often provide these services through the army or civil defense organizations. They help families find shelter, feed their animals, and move any valuable possessions to safety.

When storms sweep across South Asia, they usually bring some benefit.

What are the seasonal rains that occur in Southeast Asia called?

Monsoons always go from cold to warm areas. Most of India and Southeast Asia's climate is determined by the summer and winter monsoons. It generally occurs between the months of April and September. The rainy season in India is particularly severe, with an average of 60 inches (152 cm) of rainfall across the country.

The winter monsoon brings rain to most of India from October to March. The region receives more than 80 percent of its annual precipitation during this period.

In addition to these two monsoons, there is also a mid-summer monsoon that can cause problems for agricultural production if it fails to come along with the usual amounts of rain. When this happens, there will be no water available for growing crops. Mid-summer droughts are common in India because the country does not have a dry season. Any time of year can experience drought conditions, but they are more likely to happen during periods of high temperature and low humidity.

Mid-summer droughts usually begin around the middle of June and end around the middle of August. They are caused by the fact that the monsoon arrives late in Pakistan and northern India. When this happens, the region becomes vulnerable to drought because there isn't enough time for all the water to accumulate before it melts away in the hot weather.

About Article Author

Paul Goodman

Paul Goodman is a nature enthusiast and environmentalist. He has a degree in biology and is interested in the field of ecology. Paul loves reading about new discoveries in the field of biology, as well as learning about other environmental topics.


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