Anthropogenic Aerosol Indirect Effects in Cirrus Clouds

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  • Joyce E. Penner
    Department of Climate and Space Sciences and Engineering University of Michigan Ann Arbor MI USA
  • Cheng Zhou
    Department of Climate and Space Sciences and Engineering University of Michigan Ann Arbor MI USA
  • Anne Garnier
    Science Systems and Applications, Inc. Hampton VA USA
  • David L. Mitchell
    Desert Research Institute Reno NV USA

書誌事項

公開日
2018-10-27
権利情報
  • http://creativecommons.org/licenses/by-nc-nd/4.0/
  • http://creativecommons.org/licenses/by-nc-nd/4.0/
DOI
  • 10.1029/2018jd029204
公開者
American Geophysical Union (AGU)

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説明

<jats:title>Abstract</jats:title><jats:p>We have implemented a parameterization for forming ice in large‐scale cirrus clouds that accounts for the changes in updrafts associated with a spectrum of waves acting within each time step in the model. This allows us to account for the frequency of homogeneous and heterogeneous freezing events that occur within each time step of the model and helps to determine more realistic ice number concentrations as well as changes to ice number concentrations. The model is able to fit observations of ice number at the lowest temperatures in the tropical tropopause but is still somewhat high in tropical latitudes with temperatures between 195°K and 215°K. The climate forcings associated with different representations of heterogeneous ice nuclei (IN or INPs) are primarily negative unless large additions of IN are made, such as when we assumed that all aircraft soot acts as an IN. However, they can be close to zero if it is assumed that all background dust can act as an INP irrespective of how much sulfate is deposited on these particles. Our best estimate for the forcing of anthropogenic aircraft soot in this model is −0.2 ± 0.06 W/m<jats:sup>2</jats:sup>, while that from anthropogenic fossil/biofuel soot is −0.093 ± 0.033 W/m<jats:sup>2</jats:sup>. Natural and anthropogenic open biomass burning leads to a net forcing of −0.057 ± 0.05 W/m<jats:sup>2</jats:sup>.</jats:p>

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