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Surface impacts of the Quasi Biennial Oscillation

机译:准双年生振荡的表面影响

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摘要

Teleconnections between the Quasi Biennial Oscillation (QBO) and the Northern Hemisphere zonally averaged zonal winds, mean sea level pressure (mslp) and tropical precipitation are explored. The standard approach that defines the QBO using the equatorial zonal winds at a single pressure level is compared with the empirical orthogonal function approach that characterizes the vertical profile of the equatorial winds. Results are interpreted in terms of three potential routes of influence, referred to as the tropical, subtropical and polar routes. A novel technique is introduced to separate responses via the polar route that are associated with the stratospheric polar vortex, from the other two routes. A previously reported mslp response in January, with a pattern that resembles the positive phase of the North Atlantic Oscillation under QBO westerly conditions, is confirmed and found to be primarily associated with a QBO modulation of the stratospheric polar vortex. This mid-winter response is relatively insensitive to the exact height of the maximum QBO westerlies and a maximum positive response occurs with westerlies over a relatively deep range between 10 and 70 hPa. Two additional mslp responses are reported, in early winter (December) and late winter (February/March). In contrast to the January response the early and late winter responses show maximum sensitivity to the QBO winds at similar to 20 and similar to 70 hPa respectively, but are relatively insensitive to the QBO winds in between (similar to 50 hPa). The late winter response is centred over the North Pacific and is associated with QBO influence from the lowermost stratosphere at tropical/subtropical latitudes in the Pacific sector. The early winter response con-sists of anomalies over both the North Pacific and Europe, but the mechanism for this response is unclear. Increased precipitation occurs over the tropical western Pacific under westerly QBO conditions, particularly during boreal summer, with maxi
机译:探讨了准双年生振荡(QBO)和北半球北半球北半球北半球平均的Zonal风的遥控,平均海平面压力(MSLP)和热带降水。将使用赤道Zonal风在单个压力水平下定义QBO的标准方法与赤道风的垂直轮廓的经验正交函数方法进行比较。结果以三种潜在的影响途径解释,称为热带,亚热带和极地路线。引入了一种新颖的技术,以通过与平坦层极性涡流相关的极性途径分离响应,来自其他两条路线。 1月份的先前报告的MSLP响应,具有类似于QBOWERERLY条件下的北大西洋振荡的正阶段的模式,得到了确认,发现主要与平流层极性涡旋的QBO调制相关。这种中冬响应对最大QBO Westerlies的确切高度相对不敏感,并且在10到70 HPA之间的相对深度范围内,Westerlies发生最大肯定响应。报告了两种额外的MSLP响应,在冬季(12月)和冬季(2月/ 3月)。与1月份的响应相比,早期和晚期冬季反应显示出与20类似于20的QBO风的最大敏感性,并且类似于70 HPA,但与QBO风相对不敏感(类似于50 HPA)。晚冬季反应以北太平洋为中心,与太平洋地区热带/亚热带纬度的最低层平流层的QBO影响有关。冬季冬季反应在北太平洋和欧洲的异常,但这种反应的机制尚不清楚。在西部的QBO条件下,热带西太平洋,特别是在北方夏天,较大的降水量增加,特别是在北方夏天

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  • 来源
    《Atmospheric chemistry and physics》 |2018年第1期|共21页
  • 作者单位

    Univ Oxford NCAS Dept Ocean Atmosphere &

    Planetary Phys Oxford OX1 3PU England;

    Univ Victoria Canadian Ctr Climate Modelling &

    Anal Environm &

    Climate Change Canada Victoria BC V8W 2Y2 Canada;

    Japan Agcy Marine Earth Sci &

    Technol Yokohama Kanagawa 2360001 Japan;

    British Antarctic Survey Cambridge CB3 0ET England;

    Univ Oxford NCAS Dept Ocean Atmosphere &

    Planetary Phys Oxford OX1 3PU England;

    Univ Oxford NCAS Dept Ocean Atmosphere &

    Planetary Phys Oxford OX1 3PU England;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 大气科学(气象学);
  • 关键词

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