EventsThe 6th International Electronic Conference on Atmospheric Sciences
Published
This submission belongs to the session S5. Atmospheric Techniques, Instruments, and Modeling of the event The 6th International Electronic Conference on Atmospheric Sciences
Published date
31 Oct, 2023
Academic Editor
author-avatarAnthony Lupo
Citation
Merhala Thurai, Viswanathan Bringi, David Wolff, Charanjit Pabla, GyuWon Lee, Wonbae Bang, Aspects of Rain Drop Size Distribution Characteristics from Measurements in Two Mid-Latitude Coastal Locations, in Proceedings of The 6th International Electronic Conference on Atmospheric Sciences, 15 October–30 October 2023, MDPI: Basel, Switzerland, doi: 10.3390/ecas2023-15510
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Aspects of Rain Drop Size Distribution Characteristics from Measurements in Two Mid-Latitude Coastal Locations

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1. Department of Electrical and Computer Engineering, Colorado State University, Fort Collins, CO 80523, USA, USA
2. Department of Electrical and Computer Engineering, Colorado State University, Fort Collins, CO 80523, USA
3. NASA GSFC Wallops Flight Facility, Wallops Island, VA 23337, USA
4. Science Systems and Applications, Inc., Lanham, MD 20706, USA
5. Kyungpook National University (KNU) - Daegu Campus, 80 Daehak-ro, Buk-gu, Daegu, South Korea
Abstract

Numerous studies relating to the characterization of rain drop size distributions (DSD) have been conducted in the past several decades. Data include measurements from disdrometers as well as those retrieved from dual polarization and/or dual frequency weather radars. In this paper, we examine several different features of DSDs based on data and observations from two mid-latitude coastal locations: (a) Delmarva peninsula, USA, and (b) Incheon, ROK. In each case, the full DSD spectra were obtained from two collocated disdrometers, namely, Meteorological Particle Spectrometer (MPS) and 2D video disdrometer (2DVD). Two events from location (a) and one event from location (b) will be presented. For (a), observations and retrievals from NASA’s S-band polarimetric radar will also be included in the analyses as well as retrieved DSD parameters from the dual-wavelength precipitation radar onboard the Global Precipitation Measurement satellite. For (b), the MPS and 2DVD based DSD data will be compared with measurements from a collocated Precipitation Observation Sensor System (POSS). In all cases, emphasis will be on the underlying shape of the DSDs and its representation by the generalized gamma model, including for DSDs which correspond to light-rain.

Keywords
Rain drop size distribution
generalized gamma model
light rain
Manuscript
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