1.) ________ feedback can lead to global warming or global cooling and is related to polar ice caps and glaciers.
2.) The reverse of the ice-albedo feedback is an increase in _______.
3.) _______ water increases the rate at which carbon dioxide can be dissolved inside the ocean.
4.) If a certain climate change process has ________ radiative forcing, one would expect that this would increase temperature.
5.) Blackbody radiation is one example of ________ feedback in Earth's climate.
Respond to the following based on your reading.
6.) Choose two feedback processes and describe how they're related to each other.
7.) Briefly explain how a Milankovitch cycle can start and end a prehistoric ice age.
Answers
Answer:
Explanation:
1.) Climate models feedback can lead to global warming or global cooling and is related to polar ice caps and glaciers.
2.) The reverse of the ice-albedo feedback is an increase in solar energy.
3.) Salt water increases the rate at which carbon dioxide can be dissolved inside the ocean.
4.) If a certain climate change process has potential radiative forcing, one would expect that this would increase temperature.
5.) Blackbody radiation is one example of negative climate feedback in Earth's climate.
6.) The Positive feedback that determines the amount of water vapor increases in the air and the Negative feedback of a climate shows the decrease if water vapor in the air.
7.) The system of the rotation of the earth around the sun is known as the Milankovitch cycle. The theory states that the summer characterizes the warm and ice terms at 65 degrees north. The climate archives coincide in the ice cores and marine sediments, believing this theory it is accurately accepted.
Answer:
1. ice-albedo
2. greenhouse gases
3. colder
4. positive
5. negative
Explanation:
6. ice-albedo feedback and greenhouse gas feedback are related to eachother. warming due to the ice-albedo feedback can place significant
amounts of carbon dioxide in the atmosphere, which can then affect the rate of emission of greenhouse gases.
7. during a milankovitch cycle, isolation on earth changes due to earths orbit. this can cause global cooling to begin if the isolation decreases during a milankovitch cycle, or it can cause global warming to begin if isolation increases during a milankovitch .
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