The Retrieval of Drop Size Distribution Parameters Using a Dual-Polarimetric Radar

被引:1
|
作者
Lee, GyuWon [1 ]
Bringi, Viswanathan [2 ]
Thurai, Merhala [2 ]
机构
[1] Kyungpook Natl Univ, Ctr Atmospher Remote Sensing CARE, Dept Atmospher Sci, Daegu 41566, South Korea
[2] Colorado State Univ, Dept Elect & Comp Engn, Ft Collins, CO 80523 USA
基金
美国国家科学基金会; 美国国家航空航天局; 新加坡国家研究基金会;
关键词
drop size distributions (DSDs); double-moment scaling normalization; dual-polarimetric radar; generalized gamma model; power law; S-shape; stability of normalized DSDs; 2-DIMENSIONAL VIDEO DISDROMETER; DIFFERENTIAL PHASE-SHIFT; AXIS RATIOS; MICROPHYSICAL INTERPRETATION; LABORATORY MEASUREMENTS; RAINFALL ESTIMATION; PART I; X-BAND; SHAPE; MODEL;
D O I
10.3390/rs15041063
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The raindrop size distribution (DSD) is vital for applications such as quantitative precipitation estimation, understanding microphysical processes, and validation/improvement of two-moment bulk microphysical schemes. We trace the history of the DSD representation and its linkage to polarimetric radar observables from functional forms (exponential, gamma, and generalized gamma models) and its normalization (un-normalized, single/double-moment scaling normalized). The four-parameter generalized gamma model is a good candidate for the optimal representation of the DSD variability. A radar-based disdrometer was found to describe the five archetypical shapes (from Montreal, Canada) consisting of drizzle, the larger precipitation drops and the 'S'-shaped curvature that occurs frequently in between the drizzle and the larger-sized precipitation. Similar 'S'-shaped DSDs were reproduced by combining the disdrometric measurements of small-sized drops from an optical array probe and large-sized drops from 2DVD. A unified theory based on the double-moment scaling normalization is described. The theory assumes the multiple power law among moments and DSDs are scaling normalized by the two characteristic parameters which are expressed as a combination of any two moments. The normalized DSDs are remarkably stable. Thus, the mean underlying shape is fitted to the generalized gamma model from which the 'optimized' two shape parameters are obtained. The other moments of the distribution are obtained as the product of power laws of the reference moments M-3 and M-6 along with the two shape parameters. These reference moments can be from dual-polarimetric measurements: M-6 from the attenuation-corrected reflectivity and M-3 from attenuation-corrected differential reflectivity and the specific differential propagation phase. Thus, all the moments of the distribution can be calculated, and the microphysical evolution of the DSD can be inferred. This is one of the major findings of this article.
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页数:26
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