Knowee
Questions
Features
Study Tools

What will make air in the troposphere cooler?Group of answer choicessinkingwind from the equatorhigh pressurecoriolis effectrising

Question

What will make air in the troposphere cooler?Group of answer choicessinkingwind from the equatorhigh pressurecoriolis effectrising

🧐 Not the exact question you are looking for?Go ask a question

Solution

The cooling of air in the troposphere is primarily caused by rising air. As air rises, it expands due to lower pressure at higher altitudes. This expansion causes the air to cool. This is a fundamental principle of meteorology.

So, the correct answer is "rising".

The other options do not directly cause cooling of air in the troposphere.

  • Sinking air actually warms due to compression at lower altitudes.
  • Wind from the equator would be warm as the equator receives the most direct sunlight.
  • High pressure can lead to sinking air, which as mentioned, causes warming not cooling.
  • The Coriolis effect influences the direction of wind due to the Earth's rotation, but it does not directly affect temperature.

This problem has been solved

Similar Questions

When sea-ice forms what happens to the air above it?Group of answer choicesblows awayloses heatheats upnothinggets cooler

(Q002) The typical convection cell movement in the atmosphere means thatGroup of answer choicescool air close to the equator rises.rising air warms and compresses.cooled air spreads north and south, and its moisture condenses out in latitude zones between 20° and 30° N and S.cooled, sinking air absorbs moisture from the area below.

In Global Warming, the temperature of which part of the Atmosphere increases? a.Troposphere b.Mesosphere c.Stratosphere d.Ionosphere

What affects atmospheric pressure and why?

Convection moves air pollutants from higher altitudes to the ground.TrueFalse

1/3

Upgrade your grade with Knowee

Get personalized homework help. Review tough concepts in more detail, or go deeper into your topic by exploring other relevant questions.