Fill in the blank. feedback can lead to global warming or global cooling and is related to polar ice caps and glaciers. the reverse of the ice-albedo feedback is an increase in water increases the rate at which carbon dioxide can be dissolved inside the ocean. if a certain climate change process has radiative forcing, one would expect that this would increase temperature. blackbody radiation is one example of feedback in earth's climate. respond to the following based on your reading. choose two feedback processes and describe how they're related to each other. briefly explain how a milankovitch cycle can start and end a prehistoric ice age.

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 .

> b takes place in the gas phase in an isothermal tubular reactor. the feed is one mole of a per one mole of c, an inert. the entering temperature and pressure are 427°c and 10 atm, respectively. the gas constant r = 0.08206 atm · l/mol · k.

the answer is 0.8m.

by: nicholas