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Indexing, mode definition, and signal extraction in climate research: Analysis and applications involving the MJO, the AO, and ENSO .

机译:气候研究中的索引编制,模式定义和信号提取:涉及MJO,AO和ENSO的分析和应用。

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摘要

There are two objectives of the present study. The primary objective is to undertake following research projects involving the Arctic Oscillation (AO), the El Nino Southern Oscillation (ENSO), and the Madden Julian Oscillation (MJO): (1) an assessment of the utility of using Cyclo-stationary empirical orthogonal function (CSEOF) analysis to define the AO, (2) an empirical analysis of ENSO impacts based on varying indicator and impact regions, (3) detection and extraction of the MJO signal from QuikSCAT, and (4) the development of a general algorithm for determining optimal filter weights for time series endpoints. A secondary objective is to enumerate the statistical and analytical treatments of the AO, ENSO, and the MJO. This will include comparisons of how these three modes are defined (including their indices) and extracted from geophysical data sets.; The AO is defined using empirical orthogonal function (EOF) analysis of sea level pressure north of 20°N. The resulting spatial pattern and time series captures the regional influence of its precursor, the North Atlantic Oscillation (NAO), which is a measure of mid-latitude zonal winds over the North Atlantic. ENSO was originally defined as the pressure difference between Tahiti and Darwin, Australia: the Southern Oscillation Index. Scientists now primarily use sea surface temperature (SST) anomalies averaged over one of the Nino regions as ENSO indices. The MJO was originally observed using spectral analysis of zonal wind time series in the Indian Ocean and Western Pacific. Present day researchers use extensions of EOF analysis to construct MJO time series. For all three climate modes, the creation of high quality space-time data sets has allowed for more sophisticated indices, supplanting the simpler point-based metrics.; For the AO project, the cyclo-stationarity of Northern Hemisphere sea level pressure variability is considered. CSEOF analysis is an extension of EOF analysis that allows multiple spatial maps per mode. It accomplishes this by cyclically extending the covariance matrix based on a parameter called the nested period. (Abstract shortened by UMI.)
机译:本研究有两个目标。主要目标是进行以下涉及北极涛动(AO),厄尔尼诺南部涛动(ENSO)和马顿朱利安涛动(MJO)的研究项目:(1)对使用循环平稳经验正交的效用进行评估函数(CSEOF)分析来定义AO,(2)基于变化的指标和影响区域对ENSO影响进行经验分析,(3)从QuikSCAT中检测和提取MJO信号,以及(4)开发通用算法用于确定时间序列端点的最佳过滤器权重。第二个目标是枚举AO,ENSO和MJO的统计和分析处理。这将包括对这三种模式的定义(包括它们的索引)以及如何从地球物理数据集中提取的比较。 AO是使用经验正交函数(EOF)分析来定义的,该分析是对20°N以北的海平面压力进行的。由此产生的空间格局和时间序列捕获了其前兆北大西洋涛动(NAO)的区域影响,这是北大西洋上空的中纬度纬向风的量度。 ENSO最初定义为大溪地和澳大利亚达尔文之间的压力差:南方涛动指数。现在,科学家们主要将尼诺地区之一的平均海面温度(SST)异常作为ENSO指数。 MJO最初是使用印度洋和西太平洋纬向风时间序列的频谱分析来观测的。今天的研究人员使用EOF分析的扩展来构建MJO时间序列。对于所有三种气候模式,高质量时空数据集的创建都允许使用更复杂的指标,从而取代了基于点的简单指标。对于AO项目,考虑了北半球海平面压力变化的环平稳性。 CSEOF分析是EOF分析的扩展,允许每个模式使用多个空间图。它通过基于称为嵌套周期的参数循环扩展协方差矩阵来实现此目的。 (摘要由UMI缩短。)

著录项

  • 作者

    Arguez, Anthony.;

  • 作者单位

    The Florida State University.;

  • 授予单位 The Florida State University.;
  • 学科 Physical Oceanography.; Physics Atmospheric Science.
  • 学位 Ph.D.
  • 年度 2005
  • 页码 114 p.
  • 总页数 114
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 海洋物理学;大气科学(气象学);
  • 关键词

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