A numerical study of convection in rainbands of Typhoon Morakot (2009) with extreme rainfall: roles of pressure perturbations with low-level wind maxima
This paper investigates the formation and evolution of deep convection inside the east–west oriented rainbands associated with a low-level jet (LLJ) in Typhoon Morakot (2009). With the typhoon center to the northwest of Taiwan, the westerly LLJ occurred as a result from the interaction of typhoon ci...
Main Authors: | C.-C. Wang, H.-C. Kuo, R. H. Johnson, C.-Y. Lee, S.-Y. Huang, Y.-H. Chen |
---|---|
Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2015-10-01
|
Series: | Atmospheric Chemistry and Physics |
Online Access: | http://www.atmos-chem-phys.net/15/11097/2015/acp-15-11097-2015.pdf |
Similar Items
-
Convective Rainband Structure of Typhoon Morakot(2009)
by: CHUANG, YAO-CHUNG, et al.
Published: (2016) -
Perturbation Pressure in Cells of Rainbands Associated With Typhoon Morakot
by: Chun-Yen Lee, et al.
Published: (2013) -
The mesoscale characteristics of rainband from radar analyses: typhoon Morakot(2009).
by: Yu-shuang Tang, et al.
Published: (2010) -
Extreme Rainfall Mechanisms Exhibited by Typhoon Morakot (2009)
by: Ching-Yuang Huang, et al.
Published: (2011-01-01) -
Mesoscale processes for super heavy rainfall of Typhoon Morakot (2009) over Southern Taiwan
by: C.-Y. Lin, et al.
Published: (2011-01-01)