The eastward propagation processes of the Madden-Julian oscillation (MJO) was examined from a case study of the first MJO generated in late October during CINDY2011. The eastward propagation of the MJO was found to be synchronized with an extratropical cyclone in the Southern Hemisphere. The synchronized propagation of the MJO and the extratrpical cyclone was associated with the ridge and trough pair meridionally extending between 30 degrees S similar to 15 degrees N. The convection center of the MJO shifted eastward as a result of the westerly winds in the tropics, expanding eastward by the zonal pressure gradient force between the ridge and trough.
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Univ Tokyo, Dept Earth & Planetary Sci, Bunkyo Ku, Tokyo 1138654, Japan
Japan Agcy Marine Earth Sci & Technol, Yokohama, Kanagawa, JapanUniv Tokyo, Dept Earth & Planetary Sci, Bunkyo Ku, Tokyo 1138654, Japan
Miura, Hiroaki
Suematsu, Tamaki
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Univ Tokyo, Dept Earth & Planetary Sci, Bunkyo Ku, Tokyo 1138654, JapanUniv Tokyo, Dept Earth & Planetary Sci, Bunkyo Ku, Tokyo 1138654, Japan
Suematsu, Tamaki
Nasuno, Tomoe
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Japan Agcy Marine Earth Sci & Technol, Yokohama, Kanagawa, JapanUniv Tokyo, Dept Earth & Planetary Sci, Bunkyo Ku, Tokyo 1138654, Japan
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Univ Calif Los Angeles, Joint Inst Reg Earth Syst Sci & Engn, Los Angeles, CA 90095 USA
CALTECH, Jet Prop Lab, 4800 Oak Grove Dr, Pasadena, CA 91125 USAUniv Calif Los Angeles, Joint Inst Reg Earth Syst Sci & Engn, Los Angeles, CA 90095 USA