Microphysical features of typhoon and non-typhoon rainfall observed in Taiwan, an island in the northwestern Pacific

• Main Authors: J. Janapati, B. K. Seela, P.-L. Lin, M.-T. Lee, E. Joseph
• Format: Article
• Language: English
• Published: Copernicus Publications 2021-07-01
• Series: Hydrology and Earth System Sciences
• Online Access: https://hess.copernicus.org/articles/25/4025/2021/hess-25-4025-2021.pdf
• ISSN: 1027-5606; 1607-7938

<p>Information about the raindrop size distribution (RSD) is vital for comprehending the precipitation microphysics, improving the rainfall estimation algorithms, and appraising the rainfall erosivity. Previous research has revealed that the RSD exhibits diversity with geographical location and weather type, which leads to the assessment of the region and weather-specific RSDs. Based on long-term (2004 to 2016) disdrometer measurements in northern Taiwan, this study attempts to demonstrate the RSD aspects of summer seasons that were bifurcated into two weather conditions, namely typhoon (TY) and non-typhoon (NTY) rainfall. The results show a higher concentration of small drops and a lower concentration of large-sized drops in TY compared to NTY rainfall, and this behavior persisted even after characterizing the RSDs into different rainfall rate classes. RSDs expressed in gamma parameters show higher mass-weighted mean diameter (<span class="inline-formula"><i>D</i>_m</span>) and lower normalized intercept parameter (<span class="inline-formula"><i>N</i>_w</span>) values in NTY than TY rainfall. Moreover, sorting these two weather conditions (TY and NTY rainfall) into stratiform and convective regimes revealed a larger <span class="inline-formula"><i>D</i>_m</span> in NTY than in TY rainfall. The RSD empirical relations used in the valuation of rainfall rate (<span class="inline-formula"><i>Z</i></span>–<span class="inline-formula"><i>R</i></span>, <span class="inline-formula"><i>D</i>_m</span>–<span class="inline-formula"><i>R</i></span>, and <span class="inline-formula"><i>N</i>_w</span>–<span class="inline-formula"><i>R</i></span>) and rainfall kinetic energy (KE–<span class="inline-formula"><i>R</i></span> and KE–<span class="inline-formula"><i>D</i>_m</span>) were enumerated for TY and NTY rainfall, and they exhibited profound diversity between these two weather conditions. Attributions of RSD variability between the TY and NTY rainfall to the thermodynamical and microphysical processes are elucidated with the aid of reanalysis, remote sensing, and ground-based data sets.</p>