首页> 外文期刊>Geophysical Research Letters >Dynamical coupling of the stratosphere and mesosphere in the 2002 Southern Hemisphere major stratospheric sudden warming - art. no. L13804
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Dynamical coupling of the stratosphere and mesosphere in the 2002 Southern Hemisphere major stratospheric sudden warming - art. no. L13804

机译:2002年南半球主要平流层突然变暖中平流层与中层层的动力耦合-艺术。没有。 L13804

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摘要

NCEP data and a NCAR TIME-GCM simulation are used to explore the dynamical coupling of the stratosphere and mesosphere during the 2002 Southern Hemisphere major stratospheric sudden warming. The analyses suggest the possibility of feedback interactions between the planetary wave forcing and the mesospheric/stratospheric mean state changes. Multiple strong planetary waves before the warming penetrate into the mesosphere and weaken the polar jet. They alter the wave transmission condition in favor of more upward-poleward propagation of the wave energy at progressively lower altitudes. The jet reversal and the planetary wave surf zone also descend from the mesosphere down to the stratosphere, making wave breaking more likely at decreasing altitudes with each wave episode. These changes in the wave transmission and breaking conditions in the mesosphere and stratosphere may be critical for the extensive major stratospheric warming.
机译:NCEP数据和NCAR TIME-GCM模拟用于探索2002年南半球主要平流层突然变暖期间平流层和中层层的动力耦合。分析表明,行星波强迫与中层/平流层平均状态变化之间存在反馈相互作用的可能性。在变暖之前,多个强行星波会渗透到中层,并减弱极地射流。它们改变了波的传播条件,有利于在逐渐降低的海拔高度上波能的更多的向上极化传播。射流的逆转和行星波冲浪区也从中层下降到平流层,使得每次发生波浪时,在海拔降低的情况下发生波浪的可能性更大。平流层和中层的波传播和破坏条件的这些变化对于平流层大范围的暖化可能是至关重要的。

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