Or, you might consider the surface temperature of Venus to test your saturation hypothesis.
A simple grey-atmosphere model may be what you are looking for in the event you are serious. Here's a document (in MS Word format unfortunately) from an undergrad meteorology class that explains the basics. http://tinyurl.com/23ab9x mt --~--~---------~--~----~------------~-------~--~----~ You received this message because you are subscribed to the Google Groups Global Change ("globalchange") newsgroup. Global Change is a public, moderated venue for discussion of science, technology, economics and policy dimensions of global environmental change. Posts will be admitted to the list if and only if any moderator finds the submission to be constructive and/or interesting, on topic, and not gratuitously rude. To post to this group, send email to [email protected] To unsubscribe from this group, send email to [EMAIL PROTECTED] For more options, visit this group at http://groups.google.com/group/globalchange -~----------~----~----~----~------~----~------~--~---
