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The influence of African easterly waves on Atlantic tropical cyclone activity.

机译:非洲东风对大西洋热带气旋活动的影响。

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摘要

A high-resolution global atmospheric model is used to disentangle the relationship between African easterly waves (AEWs) and Atlantic tropical storms (TCs) from the large-scale environmental factors that may obscure their connection. Since the two most cited references on AEW interannual variability in relation to TC activity draw conflicting conclusions about the historical relationship, and the AEW counts in each study do not show agreement on historical variability, novel analysis procedures are developed to produce consistent AEW and TC count statistics for the historical record using reanalysis products. This reanalysis-derived historical record is used to legitimize the model for the study of AEWs, which is subsequently utilized to investigate the relationship between AEWs and TCs.;The internal variability of the relationship between AEW and TC count, including the sensitivity to ENSO phase and annual trends, and the interplay between environmental factors, AEW activity, and TC activity are probed using three sets of simulations: 1) climatological simulations, consisting of three ensemble members forced with historical seasonally and annually varying SST; 2) simulations with interannually invariant forcing, including a control simulation with climatological mean SST and a perpetual La Nina simulation with composite SST from strong La Nina years; 3) perturbed simulations, in which the large-scale environment is drastically altered through the manipulation of African albedo.;Since variability exists in AEW count that is unexplained by known indicators of large-scale environmental favorability, across all simulations and multiple timescales, it is unlikely that the ubiquitous covariance between AEW and TC count is simply a response to environmental factors. The statistically significant correlations between AEW and TC statistics suggest that AEW variability accounts for a portion of the observed variability in TC count not due to known environmental factors, since there is unexplained variance in AEW count, and both individual years and aggregated model runs with more (fewer) AEWs also tend to have more (fewer) TCs. It is argued that while half of the covariance between AEW and TC count interannually is mediated by the large-scale environment, the other half can be attributed to stochastic AEW variability.
机译:使用高分辨率的全球大气模型,将非洲东风(AEW)与大西洋热带风暴(TC)之间的关系与可能掩盖其联系的大规模环境因素区分开来。由于关于与TC活动有关的AEW年际变化的引用最多的两个参考文献就历史关系得出了相互矛盾的结论,并且每项研究中的AEW计数均未显示出历史变异性,因此开发了新颖的分析程序以产生一致的AEW和TC计数使用重新分析产品的历史记录的统计数据。这项重新分析的历史记录用于使AEW研究模型合法化,随后将其用于研究AEW与TC之间的关系。; AEW与TC数量之间关系的内部可变性,包括对ENSO相的敏感性利用三套模拟方法探讨了年趋势,环境因子,AEW活性和TC活性之间的相互影响:1)气候模拟,由三个受历史季节性和年度变化的SST强迫的合奏成员组成; 2)具有年际不变强迫的模拟,包括气候平均SST的控制模拟和强La Nina年复合SST的永久La Nina模拟; 3)扰动的模拟,其中通过操纵非洲反照率而大大改变了大型环境;由于AEW计数存在可变性,而在所有模拟和多个时间范围内,大型已知环境指标均无法解释AEW的可变性,因此AEW和TC计数之间普遍存在的协方差不太可能仅仅是对环境因素的响应。 AEW与TC统计数据之间的统计显着相关性表明,AEW变异性是观察到的TC计数变异性的一部分,而不是由于已知的环境因素造成的,因为AEW计数存在无法解释的差异,并且个别年份和汇总模型的运行都更多(更少)AEW也往往具有更多(更少)TC。有人认为,尽管AEW和TC计数之间的协方差的一半是由大规模环境介导的,但另一半可以归因于随机的AEW变异性。

著录项

  • 作者

    Staehling, Erica M.;

  • 作者单位

    Princeton University.;

  • 授予单位 Princeton University.;
  • 学科 Atmospheric Sciences.;Geophysics.;Climate Change.;Applied Mathematics.
  • 学位 Ph.D.
  • 年度 2015
  • 页码 204 p.
  • 总页数 204
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

  • 入库时间 2022-08-17 11:51:49

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