Respuesta :
Answer:
Explanation:
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 .
1. Ice-albedo
2. greenhouse gases
3. negative
4. ice-albedo feedback and greenhouse gas feedback are related to each other. Warming due to ice-albedo feedback can place significant amounts of carbon dioxide in the atmosphere, which can then affect the rate of emission of other greenhouse gases.
5. Increased insulation or decrease in albedo from greenhouse gases causes surface temperatures to increase. This will then cause polar ice caps and glaciers to melt, decreasing albedo. As polar ice caps and glaciers melt, they emit their trapped greenhouse gases back into the atmosphere. This causes Earth to trap more heat, leading to further increases in surface temperatures and melting