Preprints
https://doi.org/10.5194/egusphere-2024-3829
https://doi.org/10.5194/egusphere-2024-3829
10 Dec 2024
 | 10 Dec 2024
Status: this preprint is open for discussion and under review for Atmospheric Chemistry and Physics (ACP).

Quantifying cloud masking in a single column

Lukas Kluft, Bjorn Stevens, Manfred Brath, and Stefan A. Buehler

Abstract. We add idealized clouds into a single column model and show that the cloud radiative effects as observed from satellites can be reproduced by a combination of high and either low or mid-level clouds. To quantify all-sky climate sensitivity we define a "fixed-cloud-albedo" null hypothesis, which assumes an understanding of how cloud temperatures change, but assumes no change in cloud albedo. This null-hypothesis depends on how clouds are vertically distributed along the temperature profile and how this changes as the surface warms. Drawing only distributions which match the cloud radiative effects of present day observations yields a mean fixed-albedo (also keeping surface albedo fixed) climate sensitivity of 2.2 K, slightly smaller than its clear-sky value. This small number arises from two compensating effects: the dominance of cloud masking of the radiative response, primarily by mid-level clouds which are assumed not to change with temperature, and a reduction of the radiative forcing due to masking effect by high clouds. Giving more prominence to low-level clouds, which are assumed to change their temperature with warming, reduces estimates of the fixed-albedo climate sensitivity to 2.0 K. This provides a baseline to which changes in surface albedo, and a believed reduction in cloud albedo, would add to.

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Lukas Kluft, Bjorn Stevens, Manfred Brath, and Stefan A. Buehler

Status: open (until 21 Jan 2025)

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Lukas Kluft, Bjorn Stevens, Manfred Brath, and Stefan A. Buehler
Lukas Kluft, Bjorn Stevens, Manfred Brath, and Stefan A. Buehler

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Short summary
Using a single column model, we investigate the effect of the vertical distribution of clouds on climate sensitivity. We show that, depending on their height, clouds can mask or unmask the radiative response of the clear-sky atmosphere. Our single column model yields an all-sky climate sensitivity of 2.2 K, slightly less than the clear-sky value. This value can be interpreted as a baseline to which changes in surface albedo and an assumed reduction in cloud albedo would add.