Abstract

A single habit parameterization for the shortwave optical properties of cirrus is presented. The parameterization utilizes a hollow particle geometry, with stepped internal cavities as identified in laboratory and field studies. This particular habit was chosen as both experimental and theoretical results show that the particle exhibits lower asymmetry parameters when compared to solid crystals of the same aspect ratio. The aspect ratio of the particle was varied as a function of maximum dimension, D, in order to adhere to the same physical relationships assumed in the microphysical scheme in a configuration of the Met Office atmosphere-only global model, concerning particle mass, size and effective density. Single scattering properties were then computed using T-Matrix, Ray Tracing with Diffraction on Facets (RTDF) and Ray Tracing (RT) for small, medium, and large size parameters respectively. The scattering properties were integrated over 28 particle size distributions as used in the microphysical scheme. The fits were then parameterized as simple functions of Ice Water Content (IWC) for 6 shortwave bands. The parameterization was implemented into the GA6 configuration of the Met Office Unified Model along with the current operational long-wave parameterization. The GA6 configuration is used to simulate the annual twenty-year short-wave (SW) fluxes at top-of-atmosphere (TOA) and also the temperature and humidity structure of the atmosphere. The parameterization presented here is compared against the current operational model and a more recent habit mixture model.

Highlights

  • In 2013, the Intergovernmental Panel on Climate Change (IPCC) concluded that the coupling of clouds with the Earth's atmosphere is the largest uncertainty faced in predicting climate change today (Intergovernmental Panel on Climate Change, 2013)

  • In order to calculate the bulk scattering properties for each of these particle size distribution (PSD), firstly, the single scattering properties are interpolated onto size bins in each PSD, where the number of size bins in each PSD was 500 and these ranged in size between about 0.4 μm to 28,000 μm

  • The values of each of the bulk scattering properties are plotted as a function of wavelength for each of the 28 PSDs, these can be seen in Appendix D.1 and Appendix D.2 for parameterizations hex_cav1 and hex_cav2, respectively

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Summary

Introduction

In 2013, the Intergovernmental Panel on Climate Change (IPCC) concluded that the coupling of clouds with the Earth's atmosphere is the largest uncertainty faced in predicting climate change today (Intergovernmental Panel on Climate Change, 2013). One such cloud type that contributes to this uncertainty is cirrus due to their extensive global coverage of about 30%, with coverage reaching 60–80% in the tropics (Sassen et al, 2008). Cirrus has diverse microphysical properties, containing a multitude of particle habits which range in size over several orders of magnitude. This variety in size, shape and complexity poses many difficulties for the accurate representation of ice cloud in climate models. The diversity of particle shape presents many challenges, and it is well established that the particle habit significantly impacts upon the single scattering properties of ice crystals (Macke et al, 1998; Bacon and Swanson, 2000; Baran, 2012; Baum et al, 2014)

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