ESS200A
Prof. Jin-Yi Yu
Three Possible Solutions
qSolution 1: Additional heat sources must have been presented
q      Unlikely: The geothermal heat from the early Earth is sometimes suggested one such additional heat source to warm Earth. However, the geothermal heat flux is not big enough to supply the required energy.
qSolution 2: The planetary albedo must have been lower in the past
q      Unlikely: It would require a zero albedo to keep the present-day surface temperature with the 30% weaker solar luminosity in the early Earth.
qSolution 3: Greenhouse effect must have been larger
q      Most Likely: The most likely solution to the faint young  Sun paradox is that Earth’s greenhouse effect was larger in the past.
q      But (1) why and (2) why that stronger greenhouse effect reduced to the present-day strength?