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Statistical analysis of a satellite imagery time series: Implications for the study of coastal and estuarine circulation.

机译:卫星图像时间序列的统计分析:对沿海和河口环流研究的意义。

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摘要

Empirical Orthogonal Functions analysis of a thirteen month AVHRR imagery time series was performed to assess the temporal and spatial variability of turbidity patterns in Delaware Bay and the coastal area to the south. The statistical results were interpreted in light of existing knowledge of the coastal and estuarine circulation in the study area, and compared to data sets of wind and river discharge for the concurrent period of time. Several analyses, including eigenvector rotation for the EOF modes and cluster analysis, were run on different subsets of the imagery data, normalized to tidal cycle or to wind strength as well as to location within and outside the estuary. The results produced spatial patterns of variability and plots of temporal modulation of such variability over subtidal time scales; tidal cycle normalization allowed a separate examination of the variability due to tidal forcing, the dominant circulation driving force, which was inadequately sampled in the original series.;The estuarine turbidity maximum variability was captured by the dominant EOF modes and corresponded to variability in the river discharge records. Analysis of the turbidity signal along the coastal zone to the south of Delaware Bay revealed a spatial pattern that is entirely consistent with the presence of a buoyant coastal current flowing out of the Delaware Estuary and hugging the coast in a southward flow, as reported recently by Garvine (1991) and Munchow (1992). Tidal variability analysis produced ambiguous results which suggest that further study is needed in this area. The main source of error was the occasional presence of localized clouds, but it did not affect the dominant first EOF mode, because of the random nature of such error.;The techniques developed for this study can be useful as a data reduction tool in the management of the large volumes of operational satellite-derived data, since the first few EOF modes summarize the variability of the data set.
机译:进行了13个月AVHRR图像时间序列的经验正交函数分析,以评估特拉华湾和南部沿海地区浊度模式的时空变化。根据研究区域沿海和河口环流的现有知识对统计结果进行解释,并与同期的风河流量数据进行比较。对图像数据的不同子集进行了一些分析,包括EOF模式的特征向量旋转和聚类分析,并根据潮汐周期或风强度以及河口内外的位置进行了归一化。结果产生了潮汐时间尺度上的变化的空间模式和这种变化的时间调制图;潮汐周期归一化允许对潮汐强迫引起的变异性(主要循环驱动力)进行单独检查,这在原始序列中未得到充分采样。;河道浊度最大变异性由优势EOF模式捕获,并对应于河流中的变异性放电记录。根据最近的报道,对特拉华湾以南沿海地区的浊度信号进行分析后发现,其空间格局完全与从特拉华河口流出并沿南向拥抱海岸的浮力沿海水流的存在一致。 Garvine(1991)和Munchow(1992)。潮汐变化分析得出的结果不明确,这表明需要对该领域进行进一步研究。错误的主要来源是偶尔出现局部云,但由于这种错误的随机性,它并未影响主要的第一个EOF模式。本研究开发的技术可用作数据还原工具。由于前几种EOF模式总结了数据集的可变性,因此可以管理大量可操作的卫星衍生数据。

著录项

  • 作者

    Matteoda, Anna Maria.;

  • 作者单位

    University of Delaware.;

  • 授予单位 University of Delaware.;
  • 学科 Physical oceanography.;Remote sensing.
  • 学位 Ph.D.
  • 年度 1992
  • 页码 213 p.
  • 总页数 213
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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