Chile Niño/Niña — Australian Meteorological and Oceanographic Society

Chile Niño/Niña (#3)

Jiaqing Xue 1 , Jingjia Luo 1 , Chaoxia Yuan 1 2 , Toshio Yamagata 1 2
  1. Key Laboratory of Meteorological Disaster of Ministry of Education, Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters, Institute for Climate and Application Research (ICAR),Nanjing University of Information Science and Technology, Nanjing, China
  2. Application Laboratory, Japan Agency for Marine-Earth Science and Technology, Yokohama, Japan

A new ocean–atmosphere coupled mode is identified in the coastal region of the Southeast Pacific. This coastal mode displays remarkable interannual sea surface temperature (SST) variability off Chile, and we call this Chile Niño/Niña in analogy of equatorial warm/cold ENSO events. It shows a prominent seasonal phase locking nature with the largest variability in austral summer from January to March. The warm (cold) SST anomalies grow and decay with anomalous southward (northward) alongshore surface winds in association with the decreased (increased) cross-shore pressure gradient and coastal ocean downwelling (upwelling), suggesting the existence of the coastal Bjerknes feedback. During the developing phase of Chile Niño (Niña), the warm (cold) SST anomalies lead to increased (decreased) downward shortwave radiation through SST–low stratus cloud thermodynamic feedback. Meanwhile, the reduced (increased) surface wind speed off Chile shallows (deepens) the mixed-layer depth and varies the heat capacity of the surface mixed-layer. The combined effects of increased (decreased) shortwave radiation anomaly and thinner (thicker) mixed-layer depth also contribute to the development of Chile Niño (Niña). The present study reports the existence of an intrinsic coastal ocean–atmosphere coupled mode off Chile, adding a new member to the “coastal Niño/Niña” family.

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