Landsat7 ETM+ SLC-OFF数据的修复及其在武汉东湖水质反演中的应用

自从2003年5月31日,从陆地卫星 7发回的ETM+图像数据就存在缺陷。这是由于增强专题制图仪的扫描线校正器发生故障引起的。这些称为SLC OF数据的图像有一些黑色的不存在任何数据的扫描行。丢失的数据约占全景数据的25％,使它们难以正常使用。但是,数据本身仍然保留了良好的辐射和几何性质,如加以妥善修复,仍可以在一些特殊领域中使用。首先介绍了如何使用自适应局部回归算法(ALR)恢复这些图像,然后使用修复后的图像反演武汉东湖的水质参数。结果表明：ALR算法可以对SLC OF图像进行较好的修复,而且利用修复后的图像和东湖的地面水质监测数据,通过多元逐步回归分析,可以建立很好的叶绿素a、透明度、总磷以及总氮等水质参数的经验遥感反演模型,模型的相关系数R²分别为0.86、0.75、0.73和0.71。反演得到的水质参数分布与实际情况符合。这些数据有许多优点,如空间分辨率高、存档数据非常丰富、可以从NASA的服务器免费下载等。在其他遥感数据不足或无法获得的情况下,这些数据经过适当的修复,可以作为补充或替代数据使用。〖     

The use of Landsat multispectral scanner data for the analysis and management of flooding on the river Severn,England

Remote sensing has emerged as one of the major techniques for the analysis and delineation of large floods. This analysis can provide data invaluable for the hydrological management of large river systems. A need for information on the extent of floodplain inundation for the lower reaches of the largest river in the UK was met by a search through Landsat images of floods and the analysis of the best example recorded. Automated classification of the Landsat imagery of this flood on the river Severn in 1977 was used to provide estimates of the extent and spatial distribution of inundation. Flood images were generated using the Plessey IDP 3000 image processor, and the maps derived accorded well with aerial photography and qualitative flood information. Three distinct floodplain environments were delineated and flood images produced by different spectral bands compared. Specific questions prompted by flood hazard management and concerning the processes and extent of flooding were answered by the Landsat data analysis. Management of the flood risk of large rivers is expensive and remote sensing data is a relatively cheap and effective way of monitoring control works and providing data for the prediction of the effects of future hydrological works. Remote sensing is a practical way in which spatial information concerning the behavior of large dynamic systems can be obtained both quickly and relatively cheaply.     

Land-cover change in upper Barataria Basin estuary,Louisiana, 1972-1992: increases in Wetland area

The Barataria Basin, Louisiana, USA, is an extensive wetland and coastal estuary system of great economic and intrinsic value. Although high rates of wetland loss along the coastal margin of the Barataria Basin have been well documented, little information exists on whether freshwater wetlands in the upper basin have changed. Our objectives were to quantify land-cover change in the upper basin over 20 years from 1972–1992 and to determine land-cover transition rates among land-cover types. Using 80-m resolution Landsat MSS data from the North American Landscape Characterization (NALC) data archive, we classified images from three time steps (1972, 1985, 1992) into six land-cover types: agriculture, urban, bottomland hardwood forest, swamp forest, freshwater marsh, and open water. Significant changes in land cover occurred within the upper Barataria Basin over the study period. Urban land increased from 8% to 17% of the total upper basin area, primarily due to conversions from agricultural land, and to a lesser degree, bottomland forest. Swamp forest increased from 30% to 41%, associated with conversions from bottomland hardwood forest and freshwater marsh. Overall, bottomland forest decreased 38% and total wetland area increased 21%. Within the upper Barataria, increases in total wetland area may be due to land subsidence. Based on our results, if present trends in the reduction of bottomland forest land cover were to continue, the upper Barataria Basin may have no bottomland hardwood forests left by the year 2025, as it is subjected to multiple stressors both in the higher elevations (from urbanization) and lower elevations (most likely from land subsidence). These results suggest that changes in the upper freshwater portions of coastal estuaries can be large and quite different from patterns observed in the more saline coastal margins.     

Mapping Disturbances in a Mangrove Forest Using Multi-Date Landsat TM Imagery

To evaluate the accounts of local fishermen, Landsat TM images (1986, 1993, 1999) were examined to assess potential losses in the mangrove forests of the Teacapán–Agua Brava lagoon system, Mexico. A binary change mask derived from image differencing of a band 4/3 ratio was employed to calculate any changes within this forested wetland. The results indicate that by 1986 approximately 18% (or 86 km²) of the mangrove area under study was either dead or in poor condition. The majority of this damage had occurred in the eastern section of the Agua Brava basin, which coincides, with the reports of the elderly fishermen. Examination of aerial photographs from 1970 revealed no adverse impacts in this area and would suggest, as postulated by the fishermen and other scientists, that modifications in environmental conditions following the opening of a canal, Cuautlá canal, in 1972 may have initiated the large-scale mortality. Although these areas of impact are still developing, the results from the satellite data indicate that the majority of the more recent changes are occurring elsewhere in the system. Obvious in the 1999 satellite data, but not so in the 1993, are large areas of mangrove degradation in the northern section of the Teacapán region. In the Agua Brava basin, the more recent transformations are appearing on the western side of the basin. Since long-term records of environmental conditions are absent, it is difficult to determine why these latest changes are occurring or even if the earlier losses were the result of the canal. Potential agents of change that have recently been observed include a hurricane, a second canal, and the uncontrolled expansion of the Cuautlá canal since 1994.     

LANDSAT MID-INFRARED DATA AND GIS IN REGIONAL SURFACE SOIL-MOISTURE ASSESSMENT1

ABSTRACT: Landsat satellite Thematic Mapper (TM) data were used to assess regional soil moisture conditions. The mid-infrared (MIR) data of TM band 7 were overlain onto four principal land-use categories (Agricultural/Irrigated, Urban/Clearings, Forest/ Wetlands, Water) using a geographic information system (GIS). M data were used to assess four qualitative surface soil-moisture conditions (water/very wet, wet, moist, and dry) within each land-use category of a 208,354 ha southwestern Florida study area. The MIR response was inversely related to the qualitative surface soil-moisture content. Integration of Landsat TM MIR data with land use through GIS appears to be a useful technique for high-resolution regional soil moisture assessment, and further research to reline this technique is recommended.     

基于面向对象的海岸带土地利用信息提取研究

针对海岸带复杂多样的土地利用信息,选取山东省乳山市海岸带为研究区域,运用 Landsat TM遥感影像数据,基于面向对象分类方法,利用不同地物的光谱、形状、纹理和空间关系等特征,通过多尺度分割、隶属度函数法和标准最邻近分类法提取研究区土地利用信息,并对分类结果进行精度评估。结果表明：①隶属度函数法和标准最邻近分类法结合,提取出乳山市海岸带12 种土地利用类型信息,很好地区分了盐田和养殖水面、林地和园地,可提取出主要的道路和河流等细长线状地物;②将提取结果与最大似然法对比,面向对象分类方法提取精度达到82.50%,Kappa系数为0.809 1,分别比最大似然法提高了11.44%和0.105 5,很好地避免“同物异谱”和“异物同谱”对分类精度造成的影响,有效地避免了“椒盐”现象。面向对象分类方法提取中分辨率遥感影像精度较高,为海岸带土地利用信息的快速、准确提取提供了有效的技术手段。     

城市公园的冷岛效应研究——以常州市为例

在长江三角洲地区快速城市化的常州市内研究公园组成与冷岛效应的量化关系.基于Landsat 8TIRS和天地图高分辨率遥感影像提取公园指标以及冷岛效应指标.使用辐射传输方程法反演研究区的地表温度,使用ArcGIS的缓冲区分析和分段回归的方法研究每个公园的地表温度、降温范围和降温幅度作为冷岛效应指标;提取公园的周长、面积,并计算融合指数作为公园组成指标,在天地图高清遥感影像中提取公园的绿地覆盖率、水体覆盖率、不透水面覆盖率以及乔木覆盖率作为公园地表覆盖指标.通过相关性分析和回归模型研究,发现公园的面积为26hm²、周长阈值为3600m,公园的面积和周长在阈值范围内能够发挥较强的降温效率,超过阈值则降温效率下降.公园的融合指数与冷岛效应呈线性相关关系,融合指数较小的公园能获得较大的降温幅度.公园的乔木覆盖率、水体覆盖率与公园内部的地表温度呈显著相关关系,不透水面覆盖率、绿地覆盖率与公园内部的地表温度相关性不显著.公园规划设计需要结合公园的面积、周长阈值,融合指数的数值以及乔木、水体的覆盖率,充分发挥公园的冷岛效应.     

基于Landsat TM遥感数据的沈阳市生态环境监测与评价

以近年Landsat TM 遥感图像为基础数据源,利用遥感与GIS技术对沈阳市生态环境状况进行了监测.结果表明,2009年间沈阳市生态环境质量处于一般水平,与2008年相比,生态环境质量指数上升,生态环境状况呈现变好的趋势.     

塔里木河下游区域植被时空变化

为了对比生态输水工程实施前后塔里木河下游植被变化,分析植被对生态输水的时空响应,基于1986-2017年研究区上方无云的22期Landsat NDVI数据,辅以波动分析、趋势分析,探索研究区植被的时空变化特征,并对其驱动因素进行分析。结果表明：（1）空间上,植被的分布与水资源的分布密切相关,主要沿河道和积水区域分布。（2）1986-2000年,NDVI呈现缓慢下降趋势,2000-2017年NDVI总体呈现波动增加趋势;植被对生态输水有一定的滞后性,且与输水量密切相关。（3）研究区NDVI时间序列的方差介于0.0077~0.1957间,存在明显的空间差异,其波动的大小与植被种类密切相关。（4）1986-2000年,植被的NDVI空间趋势以减小为主,并主要发生在英苏和老英苏附近;2000-2017年,植被的NDVI空间趋势以增加为主,且主要发生在沿河道区域和喀尔达依东侧。     

基于GEE的1998～2018年京津冀土地利用变化对生态系统服务价值的影响

在京津冀地区可持续发展评估研究中,对生态系统服务价值进行动态估算具有重要意义.本文以京津冀地区为研究区,基于谷歌地球引擎(GEE)云平台采用分类决策树(CART)分类算法对研究区内1998、2003、2008、2013及2018年的Landsat TM/OLI影像进行监督分类得到5个时期土地利用数据并定量分析1998～2018年京津冀地区土地利用动态变化规律,再利用生态服务价值(ESV)当量估算方法定量估算京津冀地区的ESV并结合15 km×15 km尺度格网探明其时空动态变化.结果表明:①1998～2018年间,京津冀地区6种土地利用类型中建设用地(增加16. 67%)及草地(减少13. 73%)面积占比变化幅度最大,水体(减少0. 2%)面积占比变化幅度最小.②京津冀地区ESV总价值在1998～2003年间出现短暂增长(增加91. 97亿元),2003～2018年间持续降低(减少239. 07亿元),主要与建设用地面积在除1998～2003年的其余3个时间段扩张较快有关,6种土地利用类型中林地提供的ESV最高,建设用地及未利用土地提供的ESV最低.③基于15 km×15 km尺度格网的ESV时空分析表明,1998～2018年间京津冀地区ESV中等区逐渐较少,ESV较低区及较高区逐渐增加,且ESV较低区增速高于较高区.④1998～2018年间,京津冀地区6种土地利用类型对价值系数的敏感性系数(SI)范围为0～0. 40,且均低于1,表明本文ESV对修订后的生态系统服务价值系数缺乏弹性,证明本文定量估算ESV的结果是可靠的.在未来经济发展中,京津冀地区应合理优化土地利用格局,加强对林地、草地、水体及耕地的保护.研究可为制定可持续发展战略,建设生态友好型社会提供参考.