Comment on "Clouds and the Faint Young Sun Paradox" by Goldblatt and Zahnle (2011)

• Main Authors: R. Rondanelli, R. S. Lindzen
• Format: Article
• Language: English
• Published: Copernicus Publications 2012-03-01
• Series: Climate of the Past
• Online Access: http://www.clim-past.net/8/701/2012/cp-8-701-2012.pdf

Goldblatt and Zahnle (2011) raise a number of issues related to the possibility that cirrus clouds can provide a solution to the faint young sun paradox. Here, we argue that: (1) climates having a lower than present mean surface temperature cannot be discarded as solutions to the faint young sun paradox, (2) the detrainment from deep convective clouds in the tropics is a well-established physical mechanism for the formation of high clouds that have a positive radiative forcing (even if the possible role of these clouds as a negative climate feedback remains controversial) and (3) even if some cloud properties are not mutually consistent with observations in radiative transfer parameterizations, the most relevant consistency (for the purpose of hypothesis testing) is with observations of the cloud radiative forcing. Therefore, we maintain that cirrus clouds, as observed in the current climate and covering a large region of the tropics, can provide a solution to the faint young sun paradox, or at least ease the amount of CO<sub>2</sub> or other greenhouse substances needed to provide temperatures above freezing during the Archean.