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Searching for Large Raindrops: A Global Summary of Two-Dimensional Video Disdrometer Observations.

Authors :
Gatlin, Patrick N.
Thurai, Merhala
Bringi, V. N.
Petersen, Walter
Wolff, David
Tokay, Ali
Carey, Lawrence
Wingo, Matthew
Source :
Journal of Applied Meteorology & Climatology; May2015, Vol. 54 Issue 5, p1069-1089, 21p, 1 Diagram, 2 Charts, 7 Graphs, 1 Map
Publication Year :
2015

Abstract

A dataset containing 9637 h of two-dimensional video disdrometer observations consisting of more than 240 million raindrops measured at diverse climatological locations was compiled to help characterize underlying drop size distribution (DSD) assumptions that are essential to make precise retrievals of rainfall using remote sensing platforms. This study concentrates on the tail of the DSD, which largely impacts rainfall retrieval algorithms that utilize radar reflectivity. The maximum raindrop diameter was a median factor of 1.8 larger than the mass-weighted mean diameter and increased with rainfall rate. Only 0.4% of the 1-min DSD spectra were found to contain large raindrops exceeding 5 mm in diameter. Large raindrops were most abundant at the tropical locations, especially in Puerto Rico, and were largely concentrated during the spring, especially at subtropical locations. Giant raindrops exceeding 8 mm in diameter occurred at tropical, subtropical, and high-latitude continental locations. The greatest numbers of giant raindrops were found in the subtropical locations, with the largest being a 9.7-mm raindrop that occurred in northern Oklahoma during the passage of a hail-producing thunderstorm. These results suggest large raindrops are more likely to fall from clouds that contain hail, especially those raindrops exceeding 8 mm in diameter. [ABSTRACT FROM AUTHOR]

Details

Language :
English
ISSN :
15588424
Volume :
54
Issue :
5
Database :
Complementary Index
Journal :
Journal of Applied Meteorology & Climatology
Publication Type :
Academic Journal
Accession number :
102703654
Full Text :
https://doi.org/10.1175/JAMC-D-14-0089.1