State Key Laboratory of Earth System Numerical Modeling and Application, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China
College of Earth and Planetary Sciences, University of Chinese Academy of Sciences, Beijing 100049, China
Meteorological Institute, Center for Earth System Research and Sustainability, Department of Earth System Sciences, University of Hamburg, 20144 Hamburg, Germany
Meteorological Institute, Center for Earth System Research and Sustainability, Department of Earth System Sciences, University of Hamburg, 20144 Hamburg, Germany
Meteorological Institute, Center for Earth System Research and Sustainability, Department of Earth System Sciences, University of Hamburg, 20144 Hamburg, Germany
Meteorological Institute, Center for Earth System Research and Sustainability, Department of Earth System Sciences, University of Hamburg, 20144 Hamburg, Germany
Yuan-Bing Zhao
Meteorological Institute, Center for Earth System Research and Sustainability, Department of Earth System Sciences, University of Hamburg, 20144 Hamburg, Germany
Riyu Lu
State Key Laboratory of Earth System Numerical Modeling and Application, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China
College of Earth and Planetary Sciences, University of Chinese Academy of Sciences, Beijing 100049, China
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We analyze the equatorial wave circulation associated with the subtropical western North Pacific (SWNP) convection. Results show that Rossby and Kelvin waves resemble the Gill solution–enhance the equatorward side of the SWNP anticyclone/cyclone together, while mixed Rossby-gravity (MRG) and inertia-gravity (IG) waves dominate the cross-equatorial flow. Following peak convection, IG waves complement Rossby waves to link the SWNP convection and extratropical circulation during austral winter.
We analyze the equatorial wave circulation associated with the subtropical western North Pacific...