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Assignment: Climate Education Modules

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Assignment: Climate Education Modules
1. Describe and give examples of the various ways that heat can be transported in the atmosphere.

Heat can be transported in the atmosphere by solar radiation. The earth then absorbs the solar radiation and then after that it will be change into heat, which will be suck back into the atmosphere. Conduction and turbulent eddies are other ways that heat raises back into the atmosphere. All heat being transported upward towards the atmosphere

2. What causes air pressure? Is there air pressure on the moon?

Barometric and air pressure is the weight of the air pushing down on the earth, the air below, and even the ocean. Atmospheric pressure is also known as air pressure. Also there is no air pressure on the moon do to not having low or no gravity.

3. What are the principal gaseous components of the earth's atmosphere? Where do scientists believe these gases came from?

The principal gaseous components of the earth’s atmosphere are nitrogen and oxygen with small amounts of carbon dioxide and water vapors. Scientists believe that these gases came from volcanic eruptions from the Earth dating back from the beginning of time to now.

4. Many people will blow on a bowl of hot soup to try to cool it. In your view, what are the two most important heat transport processes cooling the soup?

In my view the two most important heat transport processes are convection and conduction that are taking place when blowing into a hot bowl of soap.

5. Imagine that the temperatures of the sun were to change. Describe or discuss some of the effects that this might have on the earth's energy budget and the earth's climate. How might it affect the weather where you live?

It will affect infrastructure, agriculture, and even how we use or consume energy. Crops will lose some to maybe all the crops do to the temperature of the sun getter hotter or even colder causing change in food processing causing the earth’s energy to rise and my it more expensive in time.

Reference

Ahrens, Essentials of Meteorology – Chapters 1 & 2

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