4.7 Article

The Impact of Tropical Cyclones on Extreme Precipitation over Coastal and Inland Areas of China and Its Association to ENSO

Journal

JOURNAL OF CLIMATE
Volume 31, Issue 5, Pages 1865-1880

Publisher

AMER METEOROLOGICAL SOC
DOI: 10.1175/JCLI-D-17-0474.1

Keywords

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Funding

  1. Fund for Creative Research Groups of the National Natural Science Foundation of China [41621061]
  2. National Science Foundation for Distinguished Young Scholars of China [51425903]
  3. Strategic Priority Research Program Grant of the Chinese Academy of Sciences [XDA19070402]
  4. Research Grants Council of the Hong Kong Special Administrative Region, China [HKBU22301916]
  5. Hong Kong Baptist University [FRG1/17-18/009]

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The coastal part of China and its surrounding regions are dominated by a highly dense population and highly developed economy. Extreme precipitation events (EPEs) cause a lot of damage and hence changes in these events and their causes have been drawing considerable attention. This study investigated EPEs resulting from western North Pacific (WNP) tropical cyclones (TCs) and their potential link to El Nino-Southern-Oscillation (ENSO), using TC track data, daily precipitation data from 2313 stations for 1951-2014, and the NCAR-NCEP reanalysis dataset. Two types of EPEs were considered: EPEs within 500 km from the TC center, and those caused by mesoscale and synoptic systems, referred to as predecessor rain events (PREs), beyond 1000 km from the TC center. Results indicated significant impacts of TCs on EPEs along the coastal areas, and discernable effects in inland areas of China. However, the effect of TCs on EPEs tended to be modulated by ENSO. During neutral years, inland areas of China are more affected by TC-induced extreme precipitation than during El Nino or La Nina years, with the highest density of TC tracks and larger-than average numbers of tropical storms, typhoons, and landfalling TCs. During the El Nino phase, the central and eastern equatorial Pacific was characterized by higher sea surface temperature (SST), greater low-level vorticity (1000 hPa) and upper-level divergence (250 hPa), and stronger prevailing westerlies, which combined to trigger the movement of mean genesis to the eastern and southeastern WNP, resulting in fewer TCs passing through the Chinese territory.

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