The Retrieval of Drop Size Distribution Parameters Using a Dual-Polarimetric Radar
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Published:2023-02-15
Issue:4
Volume:15
Page:1063
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ISSN:2072-4292
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Container-title:Remote Sensing
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language:en
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Short-container-title:Remote Sensing
Author:
Lee GyuWon1, Bringi Viswanathan2, Thurai Merhala2ORCID
Affiliation:
1. Department of Atmospheric Sciences, Center for Atmospheric Remote Sensing (CARE), Kyungpook National University, Daegu 41566, Republic of Korea 2. Department of Electrical and Computer Engineering, Colorado State University, Fort Collins, CO 80523, USA
Abstract
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 M3 and M6 along with the two shape parameters. These reference moments can be from dual-polarimetric measurements: M6 from the attenuation-corrected reflectivity and M3 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.
Funder
Korea Meteorological Administration Research and Development Korea government National Science Foundation NASA’s Atmospheric Dynamics
Subject
General Earth and Planetary Sciences
Reference100 articles.
1. Ryzhkov, A., Zhang, P., Bukovčić, P., Zhang, J., and Cocks, S. (2022). Polarimetric Radar Quantitative Precipitation Estimation. Remote Sens., 14. 2. Germann, U., Boscacci, M., Clementi, L., Gabella, M., Hering, A., Sartori, M., Sideris, I.V., and Calpini, B. (2022). Weather Radar in Complex Orography. Remote Sens., 14. 3. Kumjian, M.R., Prat, O.P., Reimel, K.J., van Lier-Walqui, M., and Morrison, H.C. (2022). Dual-Polarization Radar Fingerprints of Precipitation Physics: A Review. Remote Sens., 14. 4. Confronting the Challenge of Modeling Cloud and Precipitation Microphysics;Morrison;J. Adv. Model. Earth Syst.,2020 5. A simple model of evaporatively driven downdraft: Application to microburst downdraft;Srivastava;J. Atmos. Sci.,1985
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