IMPACT OF AIR-SEA INTERACTION ON THE GENESIS OF TROPICAL INCIPIENT VORTEX OVER SOUTH CHINA SEA： A CASE STUDY

• Published in: Journal of Tropical Meteorology Vol. 22; no. 3; pp. 287 - 295
• Main Author: 郝赛 毛江玉 吴国雄
• Format: Journal Article
• Language: English
• Published: Guangzhou Guangzhou Institute of Tropical & Marine Meteorology 01.09.2016
• Subjects: Atmosphere; Cyclones; Heat; Marine; Vortices; Wind shear; ISEW, South China Sea; ISEW, Philippines, Luzon I; INW, Japan
• ISSN: 1006-8775
• DOI: 10.16555/j.1006-8775.2016.03.003

Based on 6-hourly sensible heat flux and latent heat flux from the NCEP Climate Forecast System Reanalysis （CFSR） and circulation data from the Japanese 25-year Reanalysis （JRA-25）, the initial developing process of tropical cyclone Mindulle （1005） in 2010 has been diagnosed to reveal the impact of air-sea interaction over the South China Sea （SCS） on the genesis of its incipient vortex. The results show that the incipient vortex first occurred east of the Luzon Island on 0000 UTC 20 August, suggesting that the topographic forcing of the Luzon Island for easterly winds over the western Pacific might be one of the factors responsible for the formation of the incipient vortex. During the formation stage of the incipient vortex, strong southeasterlies over the SCS caused warm water of the middle and eastem SCS to flow toward the Luzon Island due to Ekman transport resulting from wind stress, leading to an increase of the sea surface temperature and sensible heat flux into the atmosphere. Although the anomalous sensible heating favored surface pressure to reduce, it was not conducive to the increase of local vorticity associated with the vortex above the heating area because, according to the atmospheric thermal adaptation theory, the anticyclonic vorticity would be created in the lower troposphere due to the decreased vertical gradient of the sensible heating. However, the ascending motions occurred over the eastern area of the anomalous sensible heating due to the augmentation of the vorticity advection with increasing height, causing water vapor to condense in the middle and upper troposphere. In turn, cyclonic vorticity was generated in the lower troposphere due to the increased vertical gradient of the condensation latent heating, resulting in the formation and further growth of the incipient vortex. Therefore, the vorticity creation due to the condensation heating played a dominant role during the subsequent enhancing stage of the incipient vortex.