Characteristics of Raindrop Size Distribution in Typhoon Nida (2016) before and after Landfall in Southern China from 2D Video Disdrometer Data

<div>Observed track every 3 h from 14:00 BST July 30, 2016, to 05:00 BST August 3, 2016. The colored dots represent different grades of TC (a). Time evolutions of maximum wind speed (m s<sup>−1</sup>) and central pressure (hPa) of Typhoon Nida (b). Radar reflectivity <i>Z</i> (dBZ) observed from Guangzhou S-band polarimetric radar at 18:00 BST on August 1 (c) and at 06:00 BST on August 2, 2016 (d).</div>

Advances in Meteorology

fig1

Figure 1

Figure 1: Characteristics of Raindrop Size Distribution in Typhoon Nida (2016) before and after Landfall in Southern China from 2D Video Disdrometer Data 

Figure 1 | Characteristics of Raindrop Size Distribution in Typhoon Nida (2016) before and after Landfall in Southern China from 2D Video Disdrometer Data 