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Modulation of tropical cyclones in the southeastern part of western North Pacific by tropical Pacific decadal variability

  • Chao Liu
  • Wenjun ZhangEmail author
  • Xin Geng
  • Malte F. Stuecker
  • Fei-Fei Jin
Article

Abstract

The tropical cyclone (TC) genesis number in the western North Pacific (WNP) exhibits a pronounced decadal decrease around the mid-1990s, with prominent seasonal and spatial inhomogeneity. This decadal shift of TC activity is mostly confined to the southeastern part of the WNP and occurs mainly during the second half of the calendar year. Accordingly, westward and northeastward TC recurving movements strongly decreased in recent decades after 1995 compared with TC tracks in the earlier period (1979–1994). We find that this TC activity decadal change is associated with tropical Pacific decadal variability, which is measured here by a low-pass filtered Niño3.4 index. In contrast to the earlier period, the anomalous cold mean state in the tropical Pacific during recent decades favored the enhancement of zonal vertical wind shear (UVWS) and suppressed TC activity. This tropical Pacific mean state change is possibly related to decadal changes of El Niño–Southern Oscillation (ENSO) properties (i.e., more La Niña events occurred during recent decades). This relationship between tropical Pacific mean state change and the UVWS in the southeastern WNP on decadal timescales is further validated based on longer observations (1951–2017) and control simulations from the Coupled Model Intercomparison Project Phase 5 (CMIP5). The statistical relationships between TC activity and the Pacific Decadal Oscillation (PDO) or Atlantic Multidecadal Oscillation (AMO) are weaker and insignificant, both for the observations and for simulations. Our results imply that decadal variations of the tropical Pacific mean state should be taken into account when predicting WNP TC activities on decadal timescales.

Keywords

Tropical cyclone Decadal change Tropical Pacific decadal variability 

Notes

Acknowledgements

This work was supported by the National Key Research and Development Program on Monitoring, Early Warning and Prevention of Major Natural Disaster (2018YFC1506002), the National Nature Science Foundation of China (41675073), the SOA Program on Global Change and Air-Sea interactions (GASI-IPOVAI-03). M. F. Stuecker was supported by the Institute for Basic Science (Project Code IBS-R028-D1) and F.-F. Jin by the U.S. National Science Foundation Grant AGS-1406601 and the U.S. Department of Energy Grant DE-SC000511.

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Copyright information

© Springer-Verlag GmbH Germany, part of Springer Nature 2019

Authors and Affiliations

  • Chao Liu
    • 1
  • Wenjun Zhang
    • 1
    Email author
  • Xin Geng
    • 1
  • Malte F. Stuecker
    • 2
    • 3
  • Fei-Fei Jin
    • 4
  1. 1.CIC-FEMD/ILCEC, Key Laboratory of Meteorological Disaster of Ministry of Education, School of Atmospheric SciencesNanjing University of Information Science and TechnologyNanjingChina
  2. 2.Center for Climate Physics, Institute for Basic Science (IBS)BusanRepublic of Korea
  3. 3.Pusan National UniversityBusanRepublic of Korea
  4. 4.Department of Atmospheric SciencesSOEST, University of Hawai’i at ManoaHonoluluUSA

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