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INTERNAL GRAVITY WAVES ACTIVITY HOTSPOT AND IMPLICATIONS FOR THE MIDDLE ATMOSPHERIC DYNAMICS

机译:内部重力波动活跃度及其对中层大气动力学的启示

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Internal gravity waves are widely recognized torncontribute significantly to the energy and angularrnmomentum transport. They play a significant role inrnaffecting many of the middle atmospheric phenomenarn(like the QBO or Brewer-Dobson circulation). UsingrnGPS RO density profiles, we have discovered arnlocalized area of enhanced IGW activity and breaking inrnthe lower stratosphere of Eastern Asia/North-westernrnPacific region.rnWith a 3D primitive equation model of the middlernatmosphere we studied the effects of such a localizedrnbreaking region on large-scale dynamics and transport.rnPossible forcing and propagation directions of planetaryrnwaves caused by such a localized IGW forcing wererninvestigated and consequences for the polar vortexrnstability and stratosphere-troposphere exchange in therntropical region were discussed.rnFinally, applying 3D EP flux and 3D residualrncirculation diagnostics, we investigated the possible rolernof this area in the longitudinal variability of the Brewer-rnDobson circulation with a hypothesis of its enhancedrndownwelling branch in this region. In the proces, modelrnresults were compared with the ozone and tracerrndistribution data from GOME, GOMOS, MIPAS andrnSCIAMACHY further confirming the importance ofrnthe Eastern Asia/North-western Pacific region forrnmiddle atmospheric dynamics.
机译:人们广泛认识到内部重力波对能量和角动量传输起了重要作用。它们在影响许多中层大气现象(如QBO或Brewer-Dobson循环)中发挥着重要作用。利用rnGPS反渗透密度分布图,我们发现了增强的IGW活动并破坏了东亚/西北太平洋低平流层的局部区域。利用中层大气的3D基本方程模型,我们研究了这种局部破碎区域对大范围的影响研究了由这样的局部IGW强迫引起的行星波的可能强迫和传播方向,并讨论了在热带地区极涡旋稳定性和平流层-对流层交换的后果。最后,应用3D EP通量和3D残余环流诊断技术,我们研究了该区域可能在Brewer-Dobson环流的纵向变化中发挥作用,并假设其在该区域的下沉分支增强。在该过程中,将模型结果与来自GOME,GOMOS,MIPAS和SCIAMACHY的臭氧和微量元素分布数据进行了比较,进一步证实了东亚/西北太平洋地区对于大气动力学的重要性。

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  • 会议地点 Heraklion(GR)
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    Charles University in Prague, Faculty of Mathematics and Physics, Department of Atmospheric Physics, V Holešovičkách 2, Praha 8, 180 00, Czech Republic, Email: petr.sacha@mff.cuni.cz;

    Charles University in Prague, Faculty of Mathematics and Physics, Department of Atmospheric Physics, V Holešovičkách 2, Praha 8, 180 00, Czech Republic;

    Institute for Meteorology, University of Leipzig, Stephanstr. 3, D-04103 Leipzig, Germany;

    Institute for Meteorology, University of Leipzig, Stephanstr. 3, D-04103 Leipzig, Germany;

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