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Atmospheric Chemistry and Physics An interactive open-access journal of the European Geosciences Union
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Volume 8, issue 5
Atmos. Chem. Phys., 8, 1225–1230, 2008
https://doi.org/10.5194/acp-8-1225-2008
© Author(s) 2008. This work is distributed under
the Creative Commons Attribution 3.0 License.
Atmos. Chem. Phys., 8, 1225–1230, 2008
https://doi.org/10.5194/acp-8-1225-2008
© Author(s) 2008. This work is distributed under
the Creative Commons Attribution 3.0 License.

  04 Mar 2008

04 Mar 2008

Does the threshold representation associated with the autoconversion process matter?

H. Guo1, Y. Liu1, and J. E. Penner2 H. Guo et al.
  • 1Atmospheric Science Division, Brookhaven National Laboratory, Upton, NY, USA
  • 2Department of Atmospheric, Oceanic and Space Sciences, the University of Michigan, Ann Arbor, MI, USA

Abstract. Different ad hoc threshold functions associated with the autoconversion process have been arbitrarily used in atmospheric models. However, it is unclear how these ad hoc functions impact model results. Here systematic investigations of the sensitivities of climatically-important properties: CF (cloud fraction), LWP (liquid water path), and AIE (aerosol indirect effect) to threshold functions have been performed using a 3-D cloud-resolving model. It is found that the effect of threshold representations is larger on instantaneous values than on daily averages; and the effect depends on the percentage of clouds in their transitional stages of converting cloud water to rain water. For both the instantaneous values and daily averages, the sensitivity to the specification of critical radius is more significant than the sensitivity to the "smoothness" of the threshold representation (as embodied in the relative dispersion of droplet size distribution) for drizzling clouds. Moreover, the impact of threshold representations on the AIE is stronger than that on CF and LWP.

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