MODELING MELTING LAYER RADAR OBSERVATIONS AT GPM FREQUENCIES; COMPARISON TO MEASUREMENTS

被引:0
|
作者
von Lerber, A. [1 ]
Moisseev, D. [2 ]
Leinonen, J. [3 ]
Tyynela, J. [2 ]
Chandrasekar, V. [2 ,3 ,4 ]
Hallikainen, M. T.
机构
[1] Aalto Univ, POB 13000, FI-00076 Aalto, Finland
[2] Univ Helsinki, Helsinki, Finland
[3] Finnish Meteorol Inst, Helsinki, Finland
[4] Colorado State Univ, Ft Collins, CO 80523 USA
基金
芬兰科学院;
关键词
Melting layer; dual-frequency; melting hydrometeors; Wakasa Bay; GPM; WET SNOW; PART I; PRECIPITATION; ATTENUATION; SNOWFLAKES; LINKS;
D O I
10.1109/IGARSS.2011.6049721
中图分类号
TM [电工技术]; TN [电子技术、通信技术];
学科分类号
0808 ; 0809 ;
摘要
The melting layer attenuation is studied by fitting the modeled reflectivity factor and the reflectivity-weighted fall velocity to measured values at both Ku- and Ka-bands. In the fitting process the optimized snow density and velocity parameters are defined and the dependence of the modeled attenuation on these parameters is investigated. The study shows that for Ku-band the implemented model can describe the melting layer with sufficient accuracy, but for Ka-band there is discrepancy between the measured and modeled values despite the fitting process. At Ka-band the attenuation of water vapor and cloud water influence more than at Ku-band and this should be considered also in the model. The sensitivity study of the modeled attenuation shows that in the snow velocity power-law function V = alpha D-beta the changes in the factor alpha induces a significant deviation in the modeled attenuation. This is true for all of the tested effective permittivity models and at both frequency bands. The permittivity model of a coated sphere solution is out of the tested models the most susceptible on changes of snow related parameters.
引用
收藏
页码:2507 / 2510
页数:4
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