TY - GEN
T1 - The radar simulator
T2 - Remote Sensing of Clouds and the Atmosphere XIV
AU - Kardas, Aleksandra E.
AU - McFarlane, Sally
AU - Morrison, Hugh
AU - Comstock, Jennifer
AU - Grabowski, Wojciech W.
AU - Malinowski, Szymon P.
PY - 2009
Y1 - 2009
N2 - We present an approach to simulate cloud radar signals on the basis of cloud model output, the radar simulator. The simulator is being developed to aid validation of the cloud model. The cloud model applies double-moment bulk warm-rain and ice schemes developed by Morrison and Grabowski.1, 2 As an input, the simulator uses profiles of the mixing ratios and number concentrations of cloud droplets, rain/drizzle drops, and ice crystals, as well as the air temperature. For the ice crystals, the rimed mass fraction predicted by the ice scheme is also used. The simulator applies precomputed look-up tables containing scattering properties of cloud and precipitation particles, such as reflectivities, extinction and absorption coefficients. For each grid point, the coefficients are integrated over particle size distributions and summed over hydrometeor types. Consistent with assumptions in the cloud model microphysical scheme, modified gamma size distributions are assumed for cloud droplets and ice crystals, whereas the exponential Marshall-Palmer size distribution is assumed for the rain/drizzle drops. Application of the radar simulator to a simulation of clouds observed during the TWP-ICE campaign over northern Australia is presented.
AB - We present an approach to simulate cloud radar signals on the basis of cloud model output, the radar simulator. The simulator is being developed to aid validation of the cloud model. The cloud model applies double-moment bulk warm-rain and ice schemes developed by Morrison and Grabowski.1, 2 As an input, the simulator uses profiles of the mixing ratios and number concentrations of cloud droplets, rain/drizzle drops, and ice crystals, as well as the air temperature. For the ice crystals, the rimed mass fraction predicted by the ice scheme is also used. The simulator applies precomputed look-up tables containing scattering properties of cloud and precipitation particles, such as reflectivities, extinction and absorption coefficients. For each grid point, the coefficients are integrated over particle size distributions and summed over hydrometeor types. Consistent with assumptions in the cloud model microphysical scheme, modified gamma size distributions are assumed for cloud droplets and ice crystals, whereas the exponential Marshall-Palmer size distribution is assumed for the rain/drizzle drops. Application of the radar simulator to a simulation of clouds observed during the TWP-ICE campaign over northern Australia is presented.
KW - Cloud
KW - Ice crystals
KW - Instrument simulator
KW - Model
KW - Radar
UR - https://www.scopus.com/pages/publications/70450200089
U2 - 10.1117/12.830100
DO - 10.1117/12.830100
M3 - Conference contribution
AN - SCOPUS:70450200089
SN - 9780819477804
T3 - Proceedings of SPIE - The International Society for Optical Engineering
BT - Remote Sensing of Clouds and the Atmosphere XIV
Y2 - 31 August 2009 through 1 September 2009
ER -