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Modeling spatial surface energy fluxes of agricultural and riparian vegetation using remote sensing.

机译:利用遥感对农业和河岸植被的空间表面能通量进行建模。

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摘要

Modeling of surface energy fluxes and evapotranspiration (ET ) requires the understanding of the interaction between land and atmosphere as well as the appropriate representation of the associated spatial and temporal variability and heterogeneity. This dissertation provides new methodology showing how to rationally and properly incorporate surface features characteristics/properties, including the leaf area index, fraction of cover, vegetation height, and temperature, using different representations as well as identify the related effects on energy balance flux estimates including ET.;The main research objectives were addressed in Chapters 2 through 4 with each presented in a separate paper format with Chapter 1 presenting an introduction and Chapter 5 providing summary and recommendations. Chapter 2 discusses a new approach of incorporating temporal and spatial variability of surface features. We coupled a remote sensing-based energy balance model with a traditional water balance method to provide improved estimates of ET. This approach was tested over rainfed agricultural fields ∼ 10 km by 30 km in Ames, Iowa. Before coupling, we modified the water balance method by incorporating a remote sensing-based estimate for one of its parameters to ameliorate its performance on a spatial basis. Promising results were obtained with indications of improved estimates of ET and soil moisture in the root zone.;The effects of surface features heterogeneity on measurements of turbulence were investigated in Chapter 3. Scintillometer-based measurements/estimates of sensible heat flux (H) were obtained over the riparian zone of the Cibola National Wildlife Refuge (CNWR), California. Surface roughness including canopy height (hc), roughness length, and zero-plane displacement height were incorporated in different ways, to improve estimates of H. High resolution, 1-m maps of ground surface digital elevation model and canopy height, hc, were derived from airborne LiDAR sensor data to support the analysis.;The effects of using different pixel resolutions to account for surface feature variability on modeling energy fluxes, e.g., net radiation, soil, sensible, and latent heat, were studied in Chapter 4. Two different modeling approaches were applied to estimate energy fluxes and ET using high and low pixel resolution datasets obtained from airborne and Landsat sensors, respectively, provided over the riparian zone of the CNWR, California. Enhanced LiDAR-based hc maps were also used to support the modeling process. The related effects were described relative to leaf area index, fraction of cover, hc, soil moisture status at root zone, groundwater table level, and vegetation stress conditions.
机译:对表面能通量和蒸散(ET)进行建模需要了解土地与大气之间的相互作用,以及对相关的时空变化和异质性的适当表示。本文提供了新的方法论,展示了如何合理地并合理地结合表面特征的特性/特性,包括叶面积指数,覆盖率,植被高度和温度,使用不同的表示方法以及识别对能量平衡通量估计的相关影响,包括ET .;主要研究目标已在第2章至第4章中提出,每个目标均以单独的论文格式提出,第1章介绍,第5章概述和建议。第2章讨论了结合表面特征的时空变化的新方法。我们将基于遥感的能量平​​衡模型与传统的水平衡方法相结合,以提供对ET的改进估算。在爱荷华州的埃姆斯,在大约10公里乘30公里的雨养农田上对该方法进行了测试。在耦合之前,我们通过结合基于遥感的参数估计值之一来改进水平衡方法,以改善其在空间上的性能。获得了令人鼓舞的结果,表明对根区的ET和土壤水分的估计值有所改善。;在第3章中研究了表面特征异质性对湍流测量的影响。基于闪烁计的测量/显热通量(H)估计为在加利福尼亚的西博拉国家野生动物保护区(CNWR)的河岸带获得。以不同方式合并了包括冠层高度(hc),粗糙度长度和零平面位移高度在内的表面粗糙度,以改善H的估算。分别绘制了高分辨率的1-m地面数字高程模型图和冠层高度hc从机载LiDAR传感器数据中得出来支持分析。;在第4章中研究了使用不同的像素分辨率来说明表面特征的可变性对能量通量建模的影响,例如净辐射,土壤,显热和潜热。分别使用分别从机载和Landsat传感器获得的高像素分辨率数据集和低像素分辨率数据集,使用不同的建模方法来估算能量通量和ET,该数据集位于加利福尼亚州CNWR的河岸带。基于增强型LiDAR的hc图也用于支持建模过程。描述了与叶面积指数,覆盖率,hc,根区土壤水分状况,地下水位和植被胁迫条件有关的相关影响。

著录项

  • 作者

    Geli, Hatim Mohammed Eisa.;

  • 作者单位

    Utah State University.;

  • 授予单位 Utah State University.;
  • 学科 Hydrology.;Remote Sensing.
  • 学位 Ph.D.
  • 年度 2012
  • 页码 182 p.
  • 总页数 182
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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