TY - JOUR
T1 - Raindrop size distribution characteristics of indian and pacific ocean tropical cyclones observed at India and Taiwan sites
AU - Janapati, Jayalakshmi
AU - Seela, Balaji Kumar
AU - Lin, Pay Liam
AU - Wang, Pao K.
AU - Tseng, Chie Huei
AU - Reddy, K. Krishna
AU - Hashiguchi, Hiroyuki
AU - Feng, Lei
AU - Das, Subrata Kumar
AU - Unnikrishnan, C. K.
N1 - Funding Information:
All authors thank IMD and JMA for providing TCs track information. This work is supported by the Ministry of Science and Technology (MOST), Taiwan, under grant numbers MOST 104-2923-M-008-003-MY5, MOST 106-2625-M-008-013, MOST 106-2811-M-008-084, MOST 107-2111-M-008-038, and MOST 108-2625-M-008-011, and partially by “Earthquake-Disaster & Risk Evaluation and Management Center, E-DREaM” from The Featured Areas Research Center Program within the framework of the Higher Education Sprout Project by the Ministry of Education (MOE), Taiwan. The first author, Jayalakshmi Janapati acknowledges MOST in carrying out this work under grant numbers MOST 104-2811-M-008-064, MOST 106-2811-M-008-084, MOST 107-2811-M-008-2551, and MOST 108-2811-M-008-558. The second author, Balaji Kumar Seela, acknowledges Academia Sinica, Taiwan, for providing the graduate fellowship under Taiwan international Graduate Program (TIGP) and MOST for providing the graduate fellowship under grant numbers MOST 106-2625-M-008-013 and MOST 107-2625-M-008-002. The second author also acknowledges MOST for providing the post-doctoral fellowship under grant numbers MOST 107-2111-M-008-038, MOST 108-2625-M-008-011 and MOST 108-2811-M-008-595, and the Central Weather Bureau (CWB), Taiwan under the grant number CWB 1072019C.
Publisher Copyright:
© The Author(s) 2020.
PY - 2020
Y1 - 2020
N2 - We made an effort to inspect the raindrop size distribution (RSD) characteristics of Indian Ocean and Pacific Ocean tropical cyclones (TCs) using ground-based disdrometer measurements from observational sites in India and Taiwan. Five TCs (2010 – 2013) from the Indian Ocean and six TCs (2014 – 2016) from the Pacific Ocean were measured using particle size and velocity disdrometers installed in south India and south Taiwan, respective-ly. Significant differences between the RSDs of Indian Ocean and Pacific Ocean TCs are noticed. For example, a higher number of small drops is observed in Indian Ocean TCs, whereas Pacific Ocean TCs have more mid-size and large drops. RSDs of Pacific Ocean TCs have higher mass-weighted mean diameter and lower normalized intercept parameter than Indian Ocean TCs. RSD values quantified based on rainfall rate and precipitation types also showed similar characteristics between Indian Ocean and Pacific Ocean TCs. The radar reflectivity and rainfall rate (Z-R) relations and shape and slope (μ-Λ) relations of both oceanic (Indian and Pacific) TCs are found to be distinctly different. Possible causes for the dissimilarities in RSD features between Indian Ocean and Pacific Ocean TCs are due to relative differences in water vapor availability and convective activity between TCs in these two oceanic basins.
AB - We made an effort to inspect the raindrop size distribution (RSD) characteristics of Indian Ocean and Pacific Ocean tropical cyclones (TCs) using ground-based disdrometer measurements from observational sites in India and Taiwan. Five TCs (2010 – 2013) from the Indian Ocean and six TCs (2014 – 2016) from the Pacific Ocean were measured using particle size and velocity disdrometers installed in south India and south Taiwan, respective-ly. Significant differences between the RSDs of Indian Ocean and Pacific Ocean TCs are noticed. For example, a higher number of small drops is observed in Indian Ocean TCs, whereas Pacific Ocean TCs have more mid-size and large drops. RSDs of Pacific Ocean TCs have higher mass-weighted mean diameter and lower normalized intercept parameter than Indian Ocean TCs. RSD values quantified based on rainfall rate and precipitation types also showed similar characteristics between Indian Ocean and Pacific Ocean TCs. The radar reflectivity and rainfall rate (Z-R) relations and shape and slope (μ-Λ) relations of both oceanic (Indian and Pacific) TCs are found to be distinctly different. Possible causes for the dissimilarities in RSD features between Indian Ocean and Pacific Ocean TCs are due to relative differences in water vapor availability and convective activity between TCs in these two oceanic basins.
UR - https://www.scopus.com/pages/publications/85084461803
UR - https://www.scopus.com/pages/publications/85084461803#tab=citedBy
U2 - 10.2151/jmsj.2020-015
DO - 10.2151/jmsj.2020-015
M3 - Article
AN - SCOPUS:85084461803
SN - 0026-1165
VL - 98
SP - 299
EP - 317
JO - Journal of the Meteorological Society of Japan
JF - Journal of the Meteorological Society of Japan
IS - 2
ER -