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Synoptic energetics of planetary-scale collapses of available potential energy.

机译:可用势能的行星尺度崩溃的天气能量学。

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摘要

We identify physical processes and localized atmospheric structures that modulate the global-scale atmospheric available potential energy (APE). A 1979--95 time series of Northern Hemisphere APE is derived from the National Centers for Environmental Prediction (NCEP) reanalysis. We discern an average three-day cycle in the APE depletion rate dA/dt with a time series of intraseasonal (1.6--180-day) fluctuations. Synoptic-scale APE depletion events are falls and subsequent rises in dA/dt, and are classified as APE collapses when exceeding climatologically-derived thresholds of APE fall and dA/dt. Three associated regional baroclinic waves are observed. West Pacific warm surges (Type A) accompany cyclogenesis over Japan, anticyclogenesis over the west-central North Pacific, and shallow East Asian cold surges. Bering warm surges (Type B) comprise intense southerly flow across the Bering Strait, cyclogenesis near the Kamchatka Peninsula, and intense anticyclogenesis over Alaska. Atlantic Canada warm surges (Type C) include onshore warm flow and eastern North American storm tracks.; January/February 1989 brought the largest vacillation- and synoptic-scale APE collapses of the study period. A pronounced Madden-Julian Oscillation (MJO) modulated equatorial convection over the Indian Ocean during the APE build-up. The initial APE collapse coincided with Type A development and intensifying MJO convection shifting to the West Pacific warm pool, which was prominent because of the 1988--89 La Nina. Extensive large-scale ascent amplified the thermally direct Hadley cell circulation, with descent strong over East Asia. The second collapse was associated with Type B development characterized by a record-breaking Alaska anticyclone.; Factors explaining lacking precision in energy budget calculations include missing o values above 100 hPa, limited representation of subgrid processes, and limited temporal resolution of diurnal convection over tropical landmasses.; Correlation analysis shows baroclinic conversion (diabatic generation) accounting for 80% (20%) of vacillation-scale dA/dt fluctuations. Baroclinic conversion contributes considerably (69%) to the synoptic variability only during synoptic-scale APE collapses (23 January to 4 February), illustrating the prominence of resolvable baroclinic processes during these periods.
机译:我们确定物理过程和局部大气结构,这些结构和结构调节着全球范围内的大气可用势能(APE)。北半球APE的1979--95年时间序列来自国家环境预测中心(NCEP)重新分析。我们根据季节内(1.6--180天)波动的时间序列来识别APE损耗率dA / dt的平均三天周期。天气尺度上的APE消耗事件是dA / dt的下降和随后的上升,当超过气候派生的APE下降和dA / dt的阈值时,分类为APE崩溃。观察到三个相关的区域斜斜波。西太平洋的热浪(A型)伴随日本的气旋作用,北太平洋中西部的反气旋作用以及东亚的浅浪。白令暖潮(B型)包括穿过白令海峡的强烈南风,堪察加半岛附近的回旋作用和阿拉斯加的强烈回旋作用。加拿大大西洋的暖潮(C型)包括陆上暖流和北美东部风暴道。 1989年1月/ 2月带来了研究期间最大的动摇和天气尺度APE崩溃。在APE形成期间,印度洋上的Madden-Julian涛动(MJO)调节了赤道对流。最初的APE崩塌与A型发展和MJO对流向西太平洋暖池的迁移同时发生,这是由于1988--89 La Nina现象而突出的。大规模的大规模上升放大了热直接哈德利细胞的循环,并在东亚形成了强烈的下降。第二次崩溃与以创纪录的阿拉斯加反旋风为特征的B型发展有关。解释能源预算计算缺乏精确性的因素包括:缺少100 hPa以上的o值,次网格过程的表示有限以及热带陆地日对流的时间分辨率有限;相关分析表明,斜压转换(绝热生成)占波动规模dA / dt波动的80%(20%)。仅在天气尺度APE塌陷(1月23日至2月4日)期间,斜压转换才对天气变化做出了很大的贡献(69%),这说明在这些时期可分辨的斜压过程突出。

著录项

  • 作者

    Wintels, Werner.;

  • 作者单位

    McGill University (Canada).;

  • 授予单位 McGill University (Canada).;
  • 学科 Physics Atmospheric Science.
  • 学位 Ph.D.
  • 年度 2003
  • 页码 153 p.
  • 总页数 153
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 大气科学(气象学);
  • 关键词

  • 入库时间 2022-08-17 11:45:44

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