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Summer land surface temperature: Small-local variation in intro-urban environment in El Paso, TX.

机译:夏季陆地表面温度:德克萨斯州埃尔帕索市内城市环境中的小局部变化。

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摘要

In recent decades, numerous approaches to study the variation of land surface temperature during daytime have emerged; however, little is known about the variation during nighttime. This study addressed the spatial variation of Summer Nighttime Land Surface Temperature (NLST) and their local determinants with comparison to Daytime Land Surface Temperature (DLST) in El Paso and its neighborhoods. Images from Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER), ASTER Global Digital Elevation Model V002 (GDEM), and Landsat 7 Enhanced Thematic Mapper Plus (ETM+) and Landsat 5 Thematic Mapper (TM 5) were used as main data sources for calculating and extracting variables, including; Land Surface Temperature (LST), Land Surface Albedo (LSA), Land Use Land Cover (LULC) classes, and Normalized Difference Vegetation Index (NDVI). Geographic Information Systems (GIS), ArcMap version 10.1, and Environment for Visualizing Images (ENVI) version 5.0 were utilized throughout this study to deal mainly with local determinants of the DLST and NLST during summer months locally. Application of Geographically Weighted Regression (GWR), a local spatial statistical technique version 4.0 employed to examine the spatially varying relationships between LST and explanatory variables including LSA, NDVI, elevation, and population density. This study also addressed the spatial distribution of social vulnerability to the LST during summer months between 1990 and 2010 using six social and biophysical indicators: total population, income, poverty, age over 65, LST, and NDVI.;The results suggested that there was a strong association between the NDVI and LST, especially during daytime. Also significant positive correlation was detected between LST, population density, LSA. The population density showed comparatively higher correlation during the night when compared to daytime, which further indicated the effect of UHI. The weaker relationships observed between the elevation and LST during day and nighttime at neighborhood levels compered to pixel units, which showed relatively significant negative correlation. The LST observed high variations based on the LULC types, which showed great increase over the urban area and further indicated the effect of urban heat islands especially during nighttime.;The results of GWR model indicate that four variables collectively were significant predictors of the variations of LST, which explained between 71% and 82% of the variance during daytime and totally explained ranged from 46% to 69% during nighttime. The analyses showed that vegetation played a dynamic part as a cooling factor in explaining the variation of LST during both day and nighttime, this effect tend to be stronger with the reduction of vegetation cover during daytime than nighttime. The population density was the second important variable influencing the LST during both day and nighttime which is acting as a warming factor. LSA and the elevation were the weaker explanatory variables during both day and nighttime.;Spatial vulnerability was found to increase over the urban area in the last 20 years. This distribution was also highly linked to the high LST distribution which indicated that the study area will be subjected to increase the vulnerability in the future since the high percentage of this vulnerable group tend to live in urban area.;In general, this dissertation casts light on an important issue in understanding the effect of built environment, biophysical and demographical factors on the local LST. Mixed methodology (correlation, descriptive, and GWR) was used in order to address this issue. The outcomes and methods used in this dissertation will be a beneficial reference for close investigation of local climate in the El Paso urban area in future work. (Abstract shortened by UMI.).
机译:近几十年来,出现了许多研究白天地表温度变化的方法。但是,对于夜间的变化知之甚少。这项研究与萨尔瓦多及其附近地区的白天夜间地面温度(DLST)相比,研究了夏季夜间地面温度(NLST)的空间变化及其局部决定因素。来自高级星载热发射和反射辐射计(ASTER),ASTER全球数字高程模型V002(GDEM)以及Landsat 7增强型专题测绘仪Plus(ETM +)和Landsat 5专题测绘仪(TM 5)的图像用作计算的主要数据源并提取变量,包括;土地表面温度(LST),土地表面反照率(LSA),土地利用土地覆盖(LULC)类和归一化植被指数(NDVI)。在整个研究过程中,都使用了地理信息系统(GIS),ArcMap版本10.1和可视化图像环境(ENVI)版本5.0,主要是在本地夏季处理DLST和NLST的本地决定因素。地理加权回归(GWR)的应用,一种本地空间统计技术版本4.0,用于检查LST与解释变量(包括LSA,NDVI,海拔和人口密度)之间的空间变化关系。这项研究还使用六个社会和生物物理指标(总人口,收入,贫困,65岁以上年龄,LST和NDVI)解决了1990年至2010年夏季LST社会脆弱性的空间分布。 NDVI和LST之间有很强的联系,尤其是在白天。在LST,人口密度,LSA之间也检测到显着正相关。与白天相比,夜间人口密度显示出相对较高的相关性,这进一步表明了UHI的影响。在白天和夜间,在邻居级别的海拔和LST之间观察到的较弱关系被归纳为像素单位,这表明相对显着的负相关。 LST观测到的基于LULC类型的高变化,显示出城市面积的极大增加,并进一步表明了城市热岛的影响,特别是在夜间。; GWR模型的结果表明,四个变量共同是变化的重要预测因子。 LST在白天解释了71%到82%的差异,而在夜间解释了从46%到69%的差异。分析表明,植被在解释白天和夜间LST的变化中起着凉爽作用,这是动态因素,而随着白天植被覆盖率的降低,这种效应往往比夜间更强。人口密度是日间和夜间影响LST的第二个重要变量,是变暖因素。 LSA和海拔高度是白天和晚上的较弱解释变量。在过去的20年中,发现城市地区的空间脆弱性在增加。这种分布也与高LST分布高度相关,这表明研究区域将来将受到更大的脆弱性的影响,因为该弱势群体的高比例往往生活在城市地区。关于了解建筑环境,生物物理和人口因素对当地LST的影响的重要问题。为了解决此问题,使用了混合方法(相关性,描述性和GWR)。本文的研究成果和方法将为今后深入研究埃尔帕索市区的局部气候提供有益的参考。 (摘要由UMI缩短。)。

著录项

  • 作者

    Mohamed, MacTar.;

  • 作者单位

    The University of Texas at El Paso.;

  • 授予单位 The University of Texas at El Paso.;
  • 学科 Geography.;Environmental Sciences.
  • 学位 Ph.D.
  • 年度 2013
  • 页码 145 p.
  • 总页数 145
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 语言学;
  • 关键词

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