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Comparison of large-scale dynamical variability in the extratropical stratosphere among the JRA-55 family data sets: impacts of assimilation of observational data in JRA-55 reanalysis data

机译:JRA-55族数据集间平流层大尺度动态变化的比较:JRA-55再分析数据中观测数据同化的影响

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摘要

This study compares large-scale dynamical variability inthe extratropical stratosphere, such as major stratospheric sudden warmings(MSSWs), among the Japanese 55-year Reanalysis (JRA-55) family data sets.The JRA-55 family consists of three products: a standard product (STDD) ofthe JRA-55 reanalysis data and two sub-products of JRA-55C (CONV) andJRA-55AMIP (AMIP). CONV assimilates only conventional surface and upper-airobservations without assimilation of satellite observations, whereasAMIP runs the same numerical weather prediction model without assimilationof observational data. A comparison of the occurrence of MSSWs in NorthernHemisphere (NH) winter shows that, compared to STDD, CONV delays several MSSWs by 1 to4 days and also misses a few MSSWs. CONV also misses the Southern Hemisphere(SH) MSSW in September 2002. AMIP shows significantly fewer MSSWs in Northern Hemisphere winter andespecially lacks MSSWs of the high aspect ratio of the polar vortex in which thevortex is highly stretched or split. A further examination of dailygeopotential height differences between STDD and CONV reveals occasionalpeaks in both hemispheres that are separated from MSSWs. The delayed andmissed MSSW cases have smaller height differences in magnitude than suchpeaks. The height differences for those MSSWs include large contributionsfrom the zonal component, which reflects underestimations in the weakening ofthe zonal mean polar night jet in CONV. We also explore strong planetarywave forcings and associated polar vortex weakenings for STDD and AMIP. Wefind a lower frequency of strong wave forcings and weaker vortex responsesto such wave forcings in AMIP, consistent with the lower MSSW frequency.
机译:本研究比较了日本55年再分析(JRA-55)系列数据集中温带平流层的大规模动态变化,例如主要的平流层突然变暖(JSR-55).JRA-55系列包括以下三种产品: JRA-55再分析数据的乘积(STDD)以及JRA-55C(CONV)和JRA-55AMIP(AMIP)的两个子产品。 CONV只吸收常规的地面和高空观测,而不会吸收卫星观测值,而AMIP运行相同的数值天气预报模型,而不会吸收观测数据。比较北半球冬季发生的MSSW,与STDD相比,CONV将多个MSSW延迟了1-4天,并且错过了几个MSSW。 CONV还错过了2002年9月的南半球MSSW.AMIP显示北半球冬季的MSSW显着减少,特别是缺少极高涡旋高度纵横比(其中涡旋高度伸展或分裂)的MSSW。进一步检查STDD和CONV之间的日地势高度差,发现在与MSSW分开的两个半球中偶尔有峰值。延迟的和遗漏的MSSW案例的幅度差异小于此类峰值。这些MSSW的高度差包括纬向成分的巨大贡献,这反映了CONV中纬向平均极地夜间急流减弱的低估。我们还探索了STDD和AMIP的强行星波强迫和相关的极涡减弱。我们在AMIP中找到了一个较低的强波浪强迫频率和较弱的涡旋响应,以与此类MSSW频率一致。

著录项

  • 作者

    Taguchi Masakazu;

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  • 年度 2017
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  • 原文格式 PDF
  • 正文语种 eng
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