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- W2028296009 abstract "[1] Links are sought between Madden-Julian oscillation (MJO)-related variations in the troposphere and stratospheric circulation. Tropospheric variations of equatorial MJO-filtered 200 hPa zonal winds define indices of MJO activity for two equatorial regions in the Indian and western Pacific oceans. These indices are used to define composite means of MJO-filtered Extended Eliassen-Palm (E-P) fluxes for eight height levels from the upper troposphere well into the stratosphere. Evidence is presented for significant and coherent MJO departures throughout the lower stratosphere. Significant departures of the vertical component of E-P flux flow into the lower stratosphere both in the tropics and at higher latitudes, especially over Canada. These are accompanied by horizontal flux departures in the upper troposphere and lower stratosphere from the central tropical Pacific into northern Canada. In this region, there is a divergence of Extended E-P flux, piling up wave energy leading to the observed increased cyclonic motion. Evidence supports the hypothesis that these high-latitude circulation variations in the stratosphere are due to a combination of two quite distinct mechanisms. In the first, poleward propagation occurs in the upper troposphere with vertical propagation at higher latitudes. In the second, upward propagation occurs in low latitudes into the lower stratosphere. This is followed by poleward propagation into higher latitudes and then farther upward propagation." @default.
- W2028296009 created "2016-06-24" @default.
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- W2028296009 date "2010-12-18" @default.
- W2028296009 modified "2023-09-26" @default.
- W2028296009 title "Extended Eliassen-Palm fluxes associated with the Madden-Julian oscillation in the stratosphere" @default.
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- W2028296009 doi "https://doi.org/10.1029/2010jd014390" @default.
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