Ice Crystal Complexity and Link to the Cirrus Cloud Radiative Effect
Geophysical monograph, pp. 47–85
Abstract
The aim of this chapter is to present emerging information on ice crystal morphology in the nano- and microscale from various sources, and explore its impact on ice crystal's single-scattering properties and ultimately on cirrus cloud radiative effect. Increasing amount of observations in the last decade have shown that cirrus ice crystals invariably contain some degree of facet roughness, hollowness, or other morphological complexities that make the crystal shape deviate from that of a pristine hexagonal shape. These morphological complexities are found to be present in a wide variety of environmental conditions. A set of physical and statistical complexity parameters is used to quantify ice crystal complexity depending on the application. Although laboratory studies have shown that complexity parameters tend to increase with increasing crystal growth rate, observations in natural cirrus indicate that complexity parameters only weakly vary at cirrus temperatures below 230 K. Morphological complexities affect the optical properties of ice crystals. Implementing the optical properties of complex ice crystals in climate models has shown that the radiative effect of crystal complexity is a cooling of 1–2 Wm −2 globally. Due to the prevalence of ice crystal morphological complexities and their influence on cirrus radiative properties, the radiative effect of crystal complexity should be taken into account in future climate models. However, work is still needed to transfer the increasing knowledge of the physical nature of ice crystal complexity into optical particle models and eventually into parameterizations used in models.
Authors 11
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Karlsruhe Institute of Technology
Affiliation as printed
Institute of Meteorology and Climate Research, Karlsruhe Institute of Technology, Karlsruhe, Germany
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Affiliation as printed
Center for Climate System Research, Columbia University, New York, NY, USA
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Affiliation as printed
Department of Physics, The College of New Jersey, Ewing, NJ, USA
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Affiliation as printed
Department of Chemistry, University of Puget Sound, Tacoma, WA, USA
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Karlsruhe Institute of Technology
Affiliation as printed
Institute of Meteorology and Climate Research, Karlsruhe Institute of Technology, Karlsruhe, Germany
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Karlsruhe Institute of Technology
Affiliation as printed
Institute of Meteorology and Climate Research, Karlsruhe Institute of Technology, Karlsruhe, Germany
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Centre National de la Recherche Scientifique · Université Clermont Auvergne · Observatoire de Physique du Globe de Clermont-Ferrand · Laboratoire de Météorologie Physique
Affiliation as printed
Laboratoire de Météorologie Physique, Université Clermont Auvergne/OPGC/CNRS, Clermont-Ferrand, France
Laboratoire de Météorologie Physique, Université Clermont Auvergne/OPGC/CNRS, Clermont-Ferrand, France
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Affiliation as printed
Department of Atmospheric Sciences, University of North Dakota, Grand Forks, ND, USA
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Karlsruhe Institute of Technology
Affiliation as printed
Institute of Meteorology and Climate Research, Karlsruhe Institute of Technology, Karlsruhe, Germany
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National Research Council - Institute of Methodologies for Environmental Analysis · National Research Council · Universitat Politècnica de Catalunya
Affiliation as printed
CommSensLab, Department of Signal Theory and Communications, Universitat Politècnica de Catalunya, Barcelona, Spain
Institute of Methodologies for Environmental Analysis, National Research Council of Italy, Tito, Italy
CommSensLab, Department of Signal Theory and Communications, Universitat Politècnica de Catalunya, Barcelona, Spain
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Langley Research Center · Space Research Organisation Netherlands
Affiliation as printed
NASA Langley Research Center, Hampton, VA, USA
now at SRON Netherlands Institute for Space Research, Leiden, Netherlands
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