首页> 外文期刊>Izvestiya Atmospheric and Oceanic Physics >Dynamics of High-Altitude Jet Streams from Satellite Measurements and Their Relationship with Climatic Parameters and Large-Scale Atmospheric Phenomena
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Dynamics of High-Altitude Jet Streams from Satellite Measurements and Their Relationship with Climatic Parameters and Large-Scale Atmospheric Phenomena

机译:从卫星测量的高空喷射流动态及其与气候参数的关系和大规模大气现象

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This article presents the results of an investigation into the spatiotemporal variability of the main characteristics of jet streams (JSs) in the upper troposphere of the Northern and Southern hemispheres in the field of view of European geostationary meteorological satellites for the period of 2007-2017. Most attention is paid to their relationship with tropospheric temperature, the sea-ice area, and large-scale atmospheric phenomena. The general patterns and significant differences in the interannual variability of the main characteristics of JSs in the Northern and Southern hemispheres are established. Correlation and cross-wavelet analyses are used to show that the temperature of the upper troposphere (T) at 200-500 hPa and the JS area (S) in both hemispheres vary interannually in antiphase, while T and latitudes of its center (phi) vary interannually in phase. Annual variations in the sea-ice area (S-ice) and S occur in both hemispheres mostly in phase, while the variations in S-ice and phi in both hemispheres are close to antiphase. The feature of annual variations of the S-ice and S series in the Northern Hemisphere was found. Namely, S variations are 1.5-2.5 months ahead of S-ice variations. A complex, time-varying nature of the relationship between JS characteristics and the North Atlantic Oscillation (NAO) and the quasi-biennial oscillation (QBO) of the zonal averaged wind over the equator was revealed.
机译:本文介绍了2007 - 2017年欧洲地球静脉气象卫星北部和南部半球对流层上部对流层射流(JSS)的主要特征的调查结果。大多数人关注他们与对流层温度,海冰区和大型大气现象的关系。建立了北部和南部半球南半球主要特征持续变化的一般模式和显着差异。相关性和交叉小波分析用于表明,在200-500 HPA的上部对流层(T)的温度和JS区域在抗磷血中依然变化,而其中心(PHI)的T和纬度阶段依然变化。海冰区域(S-lec)和S的年变化主要发生在两个半球中,而两个半球中的S-冰和PHI的变化接近抗磷血。发现了北半球S-lece和S系列年变化的特征。即,S变化在S-冰变化之前是1.5-2.5个月。揭示了JS特征与北大西洋振荡(NaO)之间关系的复杂,时变性质,并在赤道上进行了区间平均风的Quasi-Biential振荡(QBO)。

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