What is the main effect of vertical convection in the troposphere?
Answer and explanation
Correct answer: It helps vertical mixing of heat and moisture
Vertical convection occurs when warmer, less-dense air rises and cooler, denser air sinks. In the troposphere this circulation transports heat and moisture upward and downward, helping clouds, rainfall, and other weather processes develop. Option A is correct. Convection does not completely destroy ozone, densify the exosphere, or stop meteors.
Frequently asked questions
What is the correct answer to this question?
It helps vertical mixing of heat and moisture
Why is this the correct answer?
Vertical convection occurs when warmer, less-dense air rises and cooler, denser air sinks. In the troposphere this circulation transports heat and moisture upward and downward, helping clouds, rainfall, and other weather processes develop. Option A is correct. Convection does not completely destroy ozone, densify the exosphere, or stop meteors.
Which subject and chapter does this question cover?
This is a Class 11 Accountancy question. Chapter: Theory Base of Accounting. Topic: fundamental assumptions.
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