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Aerosol characterization in the Southeastern U. S. using satellite data for applications to air quality and climate.

机译:使用卫星数据在美国东南部进行气溶胶表征,以应用于空气质量和气候。

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摘要

The goal of this thesis is to develop and implement methodologies for using satellite remotely sensed data in conjunction with ground based observations and modeling for characterization of regional aerosol variations with applications to air quality and climate studies in the Southeastern U. S. This region is of special interest because of distinct aerosol types, less warming climate trends compared to the rest of U.S., and growing population.;To support this primary goal, a technique is developed that exploits the statistical relationship between PM2.5 (particulate matter that has an aerodynamic radius of 2.5 µm or less) and satellite AOD (Aerosol Optical Depth) from MODIS (Moderate resolution Imaging Spectroradiometer) where a probabilistic approach is used for air quality assessments in the metropolitan Atlanta area.;Examination of the use of multiple satellite sensors to aid in investigating the impacts of biomass burning in the region is performed. The utility of data fusion is evaluated in understanding the effects of the large wildfire that burned in May 2007. This wildfire caused PM2.5 in the metropolitan Atlanta area to exceed healthy levels with some measurements surpassing 150 µg/m3 during the month. OMI (Ozone Monitoring Instrument) AI (Aerosol Index), which qualitatively measures absorbing aerosols, have high values of more than 1.5 during May 26 – 31, 2007. CALIPSO (Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observations) a space based lidar was used to determine the vertical structure of the atmosphere across the region during the active fire period. CALIPSO was able to identify wildfire aerosols both within the planetary boundary layer (likely affects local air quality) and aloft where aerosol transport occurs. This has important implications for climatic studies specifically aerosol radiative effects.;In-depth analysis of the satellite and ground based aerosol data records over the past decade (2000 – 2009) are performed from a climatic perspective. The long temporal scale allowed for better characterization of seasonality, interannual variability, and trends. Spatial analysis of ten years of AOD from both MODIS and MISR (Multi-angle Imaging Spectroradiometer) showed little variability of AOD during the winter with mean AOD below 0.1 for the entire region, while the summer had decidedly more variability with mean AOD around 0.33 for MODIS and 0.3 for MISR. Seasonal analysis of the PM2.5 revealed that summer means are twice as high as winter means for PM2.5 . All of the datasets show interannual variability that suggests with time AOD and PM2.5 are decreasing, but seasonal variability obscured the detection of any appreciable trends in AOD; however, once the seasonal influence was removed through the creation of monthly anomalies there were decreasing trends in AOD, but only MODIS had a trend of -0.00434 (per month) that statistically significant at the 95% confidence level.;Satellite and ground-based data are used to assess the radiative impacts of aerosols in the region. The regional TOA (Top Of the Atmosphere) direct radiative forcing is estimated by utilizing satellite AOD from MODIS and MISR both on Terra, along with satellite derived cloud fraction, surface albedo (both from MODIS), and single scattering albedo (SSA) from MISR data from 2000 – 2009. Estimated TOA forcing varied from between -6 to -3 W/m 2 during the winter, and during the warmer months there is more variation with ΔF varying between -28 to -12.6 W/m2 for MODIS and -26 to -11 W/m2 for MISR. The results suggest that when AOD, cloud fraction and surface albedo are all consider they add an additional 6 W/m2 of TOA forcing compared to TOA forcing due to aerosol effects only. Varying SSA can create changes in TOA forcing of about 5 W/m2. With removal of the seasonal variability timeseries anomaly trend analysis revealed that estimated TOA forcing is decreasing (becoming less negative) with MODIS based estimates statistically significant at the 95% confidence level. (Abstract shortened by UMI.).
机译:本文的目的是开发和实施将卫星遥感数据与地面观测结合使用并进行模型化以表征区域气溶胶变化特征的方法,并将其应用于美国东南部的空气质量和气候研究中。为了实现这一主要目标,开发了一种利用PM2.5(空气动力学半径为2.5的颗粒物)之间的统计关系的技术,以支持这一主要目标。 (μm或更小)和来自MODIS(中等分辨率成像光谱仪)的卫星AOD(气溶胶光学深度),其中概率方法用于亚特兰大市区的空气质量评估。;检查使用多个卫星传感器以协助调查进行了该地区生物质燃烧的影响。在了解2007年5月大火造成的后果后,评估了数据融合的效用。这种大火导致亚特兰大市区的PM2.5超过健康水平,其中某些测量值在一个月中超过了150 µg / m3。定性测量吸收气溶胶的OMI(臭氧监测仪器)AI(气溶胶指数)在2007年5月26日至31日期间的高值超过1.5。CALIPSO(云气激光雷达和红外探路者卫星观测)是一个基于太空的激光雷达用于确定活跃火灾期间整个区域大气的垂直结构。 CALIPSO能够识别行星边界层内的野火气溶胶(可能影响当地的空气质量)和发生气溶胶运输的高空。这对气候研究,尤其是气溶胶辐射效应具有重要意义。;从气候角度对过去十年(2000年至2009年)的卫星和地面气溶胶数据记录进行了深入分析。较长的时间尺度可以更好地表征季节性,年际变化和趋势。来自MODIS和MISR(多角度成像光谱仪)的十年AOD的空间分析显示,冬季AOD的变化很小,整个区域的平均AOD均低于0.1,而夏季则明显具有较大的变化,平均AOD约为0.33。 MODIS和MISR为0.3。对PM2.5的季节性分析显示,夏季的PM2.5平均值是冬季的两倍。所有数据集均显示年际变化,表明随着时间的变化,AOD和PM2.5均在降低,但季节性变化会掩盖AOD的任何明显趋势。但是,一旦通过创建月度异常消除了季节性影响,AOD的趋势便会下降,但只有MODIS的趋势为-0.00434(每月),在95%置信度水平上具有统计显着性。数据用于评估该地区气溶胶的辐射影响。通过利用Terra上来自MODIS和MISR的卫星AOD以及卫星衍生的云分数,地表反照率(均来自MODIS)和MISR的单散射反照率(SSA)来估算区域TOA(大气层顶部)的直接辐射强迫数据来自2000年至2009年。估计的TOA强迫在冬季介于-6至-3 W / m 2之间,而在温暖的月份,MODIS的ΔF在-28至-12.6 W / m2之间变化更大- MISR为26至-11 W / m2。结果表明,与仅由于浮质作用而产生的TOA强迫相比,当同时考虑AOD,云量和表面反照率时,它们会增加6 W / m2的TOA强迫。不同的SSA可能会导致TOA强制变化约5 W / m2。除去季节性变化的时间序列后,异常趋势分析显示,基于MODIS的估计值的TOA强迫估计值正在下降(负值逐渐减小),在95%的置信水平下具有统计学意义。 (摘要由UMI缩短。)。

著录项

  • 作者

    Alston, Erica J.;

  • 作者单位

    Georgia Institute of Technology.;

  • 授予单位 Georgia Institute of Technology.;
  • 学科 Atmospheric Sciences.;Remote Sensing.
  • 学位 Ph.D.
  • 年度 2012
  • 页码 200 p.
  • 总页数 200
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

  • 入库时间 2022-08-17 11:43:40

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