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rhoneyager authored Nov 9, 2016
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- Ids 0-10 are for the pristine snowflakes of Liu (2004) and Liu (2008). There are data for 233, 243, 253, 263 and 273 K. Numerous frequencies have been included (3, 5, 9, 10, 13.4, 15, 19, 24.1, 35.6, 50, 60, 70, 80, 85.5, 90, 94, 118, 150, 166, 183, 220 and 340 GHz).
- Ids 20-22 are for bullet rosette aggregates, described in Nowell, Liu and Honeyager (2013) and Honeyager, Liu and Nowell (2016). Over one thousand aggregates are included. We currently have results only for 263 K, but extrapolation is possible by examining the behavior of the Liu (2004,2008) particles over the appropriate ranges. Ten frequencies are currently available (10.65, 13.6, 18.7, 23.8, 35.6, 36.5, 89, 94, 165.5 and 183.31 GHz).

All calculationg were performed using [DDSCAT](http://www.ddscat.org/) versions 7.0-7.3. All dielectric indices are calculated using [Mätzler \(2006\)](http://www.atmos.washington.edu/ice_optical_constants/Matzler.pdf). Random particle orientations are presented in this database. This is achieved by averaging over thousands of possible orientations. The per-orientation and polarimetric data are retained for radar frequencies. This data may be obtained by contacting the authors directly.
All calculations were performed using [DDSCAT](http://www.ddscat.org/) versions 7.0-7.3. All dielectric indices are calculated using [Mätzler \(2006\)](http://www.atmos.washington.edu/ice_optical_constants/Matzler.pdf). Random particle orientations are presented in this database. This is achieved by averaging over thousands of possible orientations. The per-orientation and polarimetric data are retained for radar frequencies. This data may be obtained by contacting the authors directly.

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