4.4 Article

Sudden Track Changes of Tropical Cyclones in Monsoon Gyres: Full-Physics, Idealized Numerical Experiments

Journal

JOURNAL OF THE ATMOSPHERIC SCIENCES
Volume 72, Issue 4, Pages 1307-1322

Publisher

AMER METEOROLOGICAL SOC
DOI: 10.1175/JAS-D-13-0393.1

Keywords

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Funding

  1. National Basic Research Program of China [2013CB430103, 2015CB452803]
  2. National Natural Science Foundation of China [41275093]
  3. project of the specially appointed professorship of Jiangsu Province
  4. Natural Science Foundation for Higher Education Institutions in Jiangsu Province [14KJB170014]
  5. Nanjing University of Information Science and Technology [20133001]
  6. project of the startup foundation for scientific research of the Nanjing University of Information Science and Technology [20123037]
  7. open project of the State Key Laboratory of Severe Weather, Chinese Academy of Meteorological Sciences [2013LASW-A13]

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Tropical cyclones (TCs) in the eastern semicircle of large-scale monsoon gyres (MGs) were observed to take either a northward (sudden northward and northward without a sharp turn) or a westward TC turn, but only the northward turn was previously simulated in a barotropic model. To understand what controls TC track types in MGs, idealized numerical experiments are performed using the full-physics Weather Research and Forecasting (WRF) Model. These experiments indicate that TCs initially located in the eastern semicircle of MGs can generally take three types of tracks: a sudden northward track, a westward track, and a northward track without a sharp turn. The track types depend upon the TC movement relative to the MG center. In agreement with barotropic simulations, the WRF simulation confirms that approaching and being collocated with the MG center is crucial to the occurrence of sudden northward TC track changes and that sudden northward track changes can be generally accounted for by changes in the steering flow. TCs that take westward tracks and northward tracks without a sharp turn do not experience such a coalescence process. Westward TCs move faster than MGs and are then located to the west of the MG center, while TCs move more slowly than MGs and then take a northward track without a sharp turn. This study reveals that the specific TC track in the eastern semicircle of an MG is sensitive to the initial wind profiles of both MGs and TCs, suggesting that improvement in the observation of TC and MG structures is very important for predicting TC track types in MGs.

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