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Developing a satellite-based method of landscape drought assessment.

机译:开发基于卫星的景观干旱评估方法。

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摘要

This dissertation describes the major research components involved in the implementation, modification, and testing of a method for assessing surface moisture status with NOAA-AVHRR data, known as the Surface Moisture Index (SMI). Chapter two presents the initial landscape-scale development of the SMI model which is predicated on previous large-scale studies reviewed in chapter one. The initial landscape model relies on a moving neighborhood analysis that exploits the relationship between radiant surface temperature (T s) and a spectral vegetation index, namely the Normalized Difference Vegetation Index (NDVI), to elucidate surface moisture status.; Chapter three describes the Water Deficit Index (WDI), another large-scale technique, the logic of which was adapted and used to modify the original SMI model. The WDI logic dictates the incorporation of near surface air temperature (Ta) as an input for the model. Since Ta is a critical component, a method for estimating this variable was necessary. Chapter four discusses the implementation and testing of the Ta technique used in subsequent model development. Three methods of estimating Ta were tested. These methods differed only in the manner that earth-sun-sensor geometry was used to impose constraints in the model calculations. The most rigorous method, which had the most sophisticated geometry constraints, resulted in the fewest actual predictions, but also showed the best results (R = 0.742, MAE = 6.09°C).; The fifth chapter treats the final version of the SMI model. That model incorporates four significant revisions from the original model. Those are: (1) adaptation of the WDI logic for landscape-scale implementation, (2) inclusion of geometric constraints, (3) near-surface air temperature estimates, and (4) specification of a new landscape reporting unit. Validation exercises relied on a ten year comparison of SMI to the Palmer Z index, a popular index for tracking drought that relies on data from meteorological stations. The ability to predict Palmer Z from SMI values was assessed using the Autoregressive Integrated Moving Average (ARIMA) technique and resulted in excellent predictability with all coefficients being significant at the alpha = 0.05 level.
机译:本文描述了主要的研究组成部分,涉及利用NOAA-AVHRR数据评估表面水分状态的方法(称为表面水分指数(SMI))的实施,修改和测试。第二章介绍了SMI模型的初始景观尺度开发,该模型以第一章中回顾的先前的大规模研究为基础。初始景观模型依赖于移动邻域分析,该分析利用辐射表面温度(T s)与光谱植被指数(即归一化植被指数(NDVI))之间的关系来阐明表面湿度状态。第三章描述了缺水指数(WDI),这是另一种大规模技术,其逻辑已被修改并用于修改原始SMI模型。 WDI逻辑指示将近地表气温(Ta)合并为模型的输入。由于Ta是关键成分,因此需要一种估计该变量的方法。第四章讨论了用于后续模型开发的Ta技术的实现和测试。测试了三种估算Ta的方法。这些方法的不同之处仅在于使用地球太阳传感器的几何形状在模型计算中施加约束。 ;最严格的方法,具有最复杂的几何约束,产生的实际预测最少,但结果也最好(R = 0.742,MAE = 6.09°C)。第五章介绍了SMI模型的最终版本。该模型合并了原始模型的四个重要修订。它们是:(1)使WDI逻辑适用于景观尺度的实现;(2)包括几何约束;(3)近地表气温估算;以及(4)新景观报告单元的规范。验证工作依赖于SMI与Palmer Z指数的十年比较,Palmer Z指数是一种流行的用于跟踪干旱的指数,它依赖于气象站的数据。使用自回归综合移动平均(ARIMA)技术评估了从SMI值预测Palmer Z的能力,并得出了极好的可预测性,所有系数在alpha = 0.05时均很显着。

著录项

  • 作者

    Riddering, James Plummer.;

  • 作者单位

    University of Montana.;

  • 授予单位 University of Montana.;
  • 学科 Agriculture Forestry and Wildlife.; Physical Geography.; Remote Sensing.
  • 学位 Ph.D.
  • 年度 2004
  • 页码 161 p.
  • 总页数 161
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 森林生物学;自然地理学;遥感技术;
  • 关键词

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