Climate Dynamics 11:670:461 Alan Robock

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FEEDBACK PARAMETERS Let T s = global mean surface air temperature R= net flux of heat into the climate system ΔR f = change in R due to some change in.

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Presentation transcript:

Climate Dynamics 11:670:461 Alan Robock robock@envsci.rutgers.edu Lecture 14, 10/24/13 Climate Dynamics 11:670:461 Alan Robock Department of Environmental Sciences Rutgers University, New Brunswick, New Jersey USA robock@envsci.rutgers.edu http://envsci.rutgers.edu/~robock

Temperature Feedbacks Start with temperature increase, e.g., from more CO2 – + + + – + – – – Robock, Alan, 1985: An updated climate feedback diagram. Bull. Amer. Met. Soc., 66, 786-787. External forcing

Poisson d’Avril = April Fool Of course! This is the best thing since sliced baguettes! http://www.realclimate.org/index.php/archives/2007/04/the-sheep-albedo-feedbacki/