4.7 Article

Critical Role of Northern Off-Equatorial Sea Surface Temperature Forcing Associated with Central Pacific El Nino in More Frequent Tropical Cyclone Movements toward East Asia

Journal

JOURNAL OF CLIMATE
Volume 26, Issue 8, Pages 2534-2545

Publisher

AMER METEOROLOGICAL SOC
DOI: 10.1175/JCLI-D-12-00287.1

Keywords

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Funding

  1. National Research Foundation of Korea (NRF)
  2. South Korean government (MEST) [2012-0000850]
  3. Korea Meteorological Administration Research and Development Program [CATER 2012-3081]
  4. BK21 project of the South Korean government
  5. Korea Environmental Industry & Technology Institute (KEITI) [ARQ201303057001] Funding Source: Korea Institute of Science & Technology Information (KISTI), National Science & Technology Information Service (NTIS)
  6. Korea Meteorological Administration [CATER-2012-3081] Funding Source: Korea Institute of Science & Technology Information (KISTI), National Science & Technology Information Service (NTIS)
  7. Ministry of Education, Science & Technology (MoST), Republic of Korea [울산-001] Funding Source: Korea Institute of Science & Technology Information (KISTI), National Science & Technology Information Service (NTIS)
  8. National Research Foundation of Korea [2009-0083527] Funding Source: Korea Institute of Science & Technology Information (KISTI), National Science & Technology Information Service (NTIS)

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Observational records reveal that the number of tropical cyclones (TCs) approaching East Asia in July-October is positively correlated with sea surface temperatures (SSTs) in the equatorial and northern off-equatorial central Pacific (CP) oceans, indicating the significant impact of CP El Nino (CP-EN). Through experiments using a Weather Research and Forecast (WRF) model-based regional climate model, this study demonstrates that it is northern off-equatorial CP warming, rather than equatorial CP warming, that effectively induces local anomalous steering flows pertinent to the observed increase in TC activity over East Asia during CP-EN. Sensitivity experiments, in which the prescribed CP-EN-related SST anomaly is confined near the equator, do not capture the observed TC increase over East Asia, whereas those including the off-equatorial region successfully reproduce observed atmospheric and TC variabilities. The off-equatorial CP SST anomaly acts to expand the anomalous cyclonic response in the Philippine Sea farther northward. This produces a tunnel effect in the East China Sea, by which more TCs move to East Asian coastal regions (e.g., east China, Taiwan, Korea, and Japan).

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