Articles | Volume 15, issue 1
https://doi.org/10.5194/cp-15-279-2019
https://doi.org/10.5194/cp-15-279-2019
Research article
 | 
13 Feb 2019
Research article |  | 13 Feb 2019

China's historical record when searching for tropical cyclones corresponding to Intertropical Convergence Zone (ITCZ) shifts over the past 2 kyr

Huei-Fen Chen, Yen-Chu Liu, Chih-Wen Chiang, Xingqi Liu, Yu-Min Chou, and Hui-Juan Pan

Related subject area

Subject: Climate Modelling | Archive: Historical Records | Timescale: Centennial-Decadal
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Cited articles

Baldini, L. M., Baldini, J. U. L., McElwaine, J. N., Frappier, A. B., Asmerom, Y., Liu, K. B., Prufer, K. M., Ridley, H. E., Polyak, V., Kennett, D. J., Macpherson, C. G., Aquino, V. V., Awe, J., and Breitenbach, S. F. M.: Persistent northward North Atlantic tropical cyclone track migration over the past five centuries, Sci. Rep.-UK, 6, 37522, https://doi.org/10.1038/srep37522, 2016. 
Bossak, B. H., Keihany, S. S., Welford, M. R., and Gibney, E. J.: Coastal Georgia is not immune: hurricane history, 1851–2012, Southeastern Geographer, 54, 323–333, https://doi.org/10.1353/sgo.2014.0027, 2014. 
Chan, J. C. L.: Tropical cyclone activity in the northwest Pacific in relation to the El Niño/Southern Oscillation phenomenon, Mon. Weather Rev., 113, 599–606, 1985. 
Chan, J. C. L. and Shi, J. E.: Frequency of typhoon landfall over Guangdong Province of China during the period 1470–1931, Int. J. Climatol., 20, 183–190, 2000. 
Chen, H. F., Wen, S. Y, Song, S. R., Yang, T. N., Lee, T. Q., Lin, S. F., Hsu, S. C., Wei, K. Y., Chang, P. Y., and Yu, P. S.: Strengthening of paleo-typhoon and autumn rainfall in Taiwan corresponding to the Southern Oscillation at Late Holocene, J. Quaternary Sci., 27, 964–972, 2012. 
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Short summary
China’s historical typhoon data show that (1) the tracks of typhoons correspond to the north–southward migration of the Intertropical Convergence Zone and phase of the North Atlantic Oscillation, which show a nearly 30-year and a 60-year cycle during the Little Ice Age (LIA) and (2) paleotyphoons made landfall in mainland China 1 month earlier during the Medieval Warm Period than during the LIA.