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Atmospheric pressure variations at extratropical latitudes associated with Forbush decreases of galactic cosmic rays

机译:与Forbush相关的温带纬度的大气压变化使银河系宇宙射线减少

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Changes of troposphere pressure associated with short-time variations of galactic cosmic rays (GCRs) taking place in the Northern hemisphere's cold months (October-March) were analyzed for the period 1980-2006, NCEP/NCAR reanalysis data being used. Noticeable pressure variations during Forbush decreases of GCRs were revealed at extratropical latitudes of both hemispheres. The maxima of pressure increase were observed on the 3rd-4th days after the event onsets over Northern Europe and the European part of Russia in the Northern hemisphere, as well as on the 4th-5th days over the eastern part of the South Atlantic opposite Queen Maud Land and over the d'Urville Sea in the Southern Ocean. According to the weather chart analysis, the observed pressure growth, as a rule, results from the weakening of cyclones and intensification of anticyclone development in these areas. The presented results suggest that cosmic ray variations may influence the evolution of extratropical baric systems and play an important role in solar-terrestrial relationships.
机译:分析了1980-2006年期间北半球寒冷月份(10月至3月)发生的对流层压力变化与银河系宇宙射线(GCR)的短时变化,并使用了NCEP / NCAR再分析数据。在两个半球的温带纬度上,GCR的Forbush减小过程中压力变化明显。事件发生后第3至4天,在北半球的北欧和俄罗斯欧洲部分以及皇后对面的南大西洋东部,在第4至5天观察到了压力增加的最大值。莫德土地(Maud Land)和南大洋的d'Urville海。根据气象图分析,通常观察到的压力增长是由于这些地区气旋减弱和反气旋发展加剧所致。提出的结果表明,宇宙射线的变化可能会影响温带大气系统的演化,并在日地关系中发挥重要作用。

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