Attribution of the present‐day total greenhouse effect
Gavin A. Schmidt,1 Reto A. Ruedy,1 Ron L. Miller,1 and Andy A. Lacis1
Received 30 March 2010; revised 27 July 2010; accepted 3 August 2010; published 16 October 2010.
[1] The relative contributions of atmospheric long‐wave absorbers to the present‐day
global greenhouse effect are among the most misquoted statistics in public discussions
of climate change. Much of the interest in these values is however due to an implicit
assumption that these contributions are directly relevant for the question of climate
sensitivity. Motivated by the need for a clear reference for this issue, we review the
existing literature and use the Goddard Institute for Space Studies ModelE radiation
module to provide an overview of the role of each absorber at the present‐day and under
doubled CO2. With a straightforward scheme for allocating overlaps, we find that water
vapor is the dominant contributor (∼50% of the effect), followed by clouds (∼25%)
and then CO2 with ∼20%. All other absorbers play only minor roles.
In a doubled CO2
scenario, this allocation is essentially unchanged, even though the magnitude of the total
greenhouse effect is significantly larger than the initial radiative forcing, underscoring
the importance of feedbacks from water vapor and clouds to climate sensitivity.