Tropical cyclone FANTALA's three turnbacks in the northeast of Madagascar Island.

Autor: Zhang L; School of Marine Technology and Geomatics, Jiangsu Ocean University, Lianyungang, Jiangsu province, China.; Lianyungang Meteorological Bureau, Lianyungang, Jiangsu province, China., Sun K; Nantong Marine Center of Ministry of Natural Resources, Nantong, Jiangsu province, China., Zhu Y; School of Marine Technology and Geomatics, Jiangsu Ocean University, Lianyungang, Jiangsu province, China., Cao Y; School of Marine Technology and Geomatics, Jiangsu Ocean University, Lianyungang, Jiangsu province, China., Feng Q; School of Marine Technology and Geomatics, Jiangsu Ocean University, Lianyungang, Jiangsu province, China., Zhou Y; School of Marine Technology and Geomatics, Jiangsu Ocean University, Lianyungang, Jiangsu province, China., Lü H; School of Marine Technology and Geomatics, Jiangsu Ocean University, Lianyungang, Jiangsu province, China.; Lianyungang Meteorological Bureau, Lianyungang, Jiangsu province, China.
Jazyk: angličtina
Zdroj: PloS one [PLoS One] 2024 Aug 30; Vol. 19 (8), pp. e0305873. Date of Electronic Publication: 2024 Aug 30 (Print Publication: 2024).
DOI: 10.1371/journal.pone.0305873
Abstrakt: The unique Tropical cyclone (TC) Fantala appeared in the central Indian Ocean (12.4°S, 73.5°E) at 00Z on April 11 in 2016 and moved northwestward along the northeast of Madagascar at 18 Z on April 15. Then, two incomprehensible turnbacks formed a unique TC track. The dynamic mechanisms of the three turnbacks were first studied based on remote sensing and multisource reanalysis data. The results reveal that the wind field with upper divergence and lower convergence promotes the development of Fantala. The anticyclone high pressure on the middle level atmosphere is an important factor for TC turnbacks. On 15 April, the TC made the first turnback to turn northwest due to the southward anticyclone weakened to moving northwest. On 18 April, the TC made the second turnback along the anticyclone edge due to the northern high-pressure and southern low-pressure trough. On 22 April, the TC made the third turnback because the anticyclonic high press center broke into two small independent anticyclonic centers in the southwest and northeast, which created a barrier band and pushed the northern TC to move to the northwest. Meanwhile, the vertical wind shear (VWS) also provides favorable conditions for TC turnbacks. On April 18, the middle atmosphere of the TC was affected by strong easterly shear and weak southerly shear, and the second turnback was completed. On April 22, the middle level environment was affected by strong westerly shear and weak north shear, and the third turnback was completed. Additionally, heat transport from the ocean to the atmosphere provides favorable conditions for TC development. On April 18, The maximum mean latent heat flux over northeastern Madagascar was 112.94 W/m2, Tropical Cyclone Heat Potential was 39.05 kJ/cm2, and the maximum wind speed at the center of the TC was 155 kts. On April 22, The heat transfer from the equator increased by 18.08 W/m2 compared with the latent heat on 21 April, the Tropical Cyclone Heat Potential was 33.30 kJ/cm2, the maximum wind speed in the TC center was 90 kts, the high PV centerspread down from 850 mb to 900 mb. This study deepens the understanding of track forecasting during the development of a TC.
Competing Interests: The authors have declared that no competing interests exist.
(Copyright: © 2024 Zhang et al. This is an open access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.)
Databáze: MEDLINE
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