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在人力和地质不断变化的背景下,必须及时进行土地利用变化测绘来保证土地资源的可持续发展,常规的土地利用变化测绘方法测绘精度低,无法满足快速变化的土地测绘需求。因此,基于中国北斗卫星导航系统（BDS）与全球定位系统（GPS）设计了新的土地利用变换测绘方法。首先,处理了土地利用变化测绘数据,基于BDS与GPS处理了土地变化测绘遥感影像;其次,检测了土地利用变化测绘遥感影像变化特征;最后选择了土地利用变化指数,实现了土地利用变化测绘。实验结果表明,设计的土地利用变化测绘方法的测绘精度高,符合现有的土地利用变化需求,有一定的应用价值。 相似文献
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基于DEM的广东省山区土地利用变化分析 总被引：2，自引：0，他引：2
土地利用/覆盖变化研究是全球环境变化与可持续发展研究的热点和前沿领域。近年来,随着广东省经济发展迅速,土地利用在受珠江三角洲地区辐射影响的广东山区也发生了较大的变化。在DEM的基础上,分析1993~2003年来广东省山区韶关市的土地利用变化与高程、坡度和坡向的关系。研究结果表明,1993~2003年来广东省山区韶关市的土地利用变化在高程、坡度和坡向有很大差异,这些因素对该地区的土地利用有着重要的影响。为促进该地区的土地可持续利用,需进一步因地制宜,结合高程、坡度和坡向等影响因素优化土地利用类型和改善地表覆盖。 相似文献
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土地利用监测,是根据实时更新的土地利用信息,全面地检测全市内的土地利用状况,便于人们更快的了解信息;土地利用预测,是根据近十年来的土地利用数据,使用科学的方法,预测土地行业的发展趋势,帮助政府及个人决策。本文利用ArcIMS技术构建了一套土地市场监测的WebGIS系统。从工程人员在服务器端的具体实施方法和客户端的最终成果两方面着重介绍了WebGIS在北京市国土资源局土地市场监测预测中的应用。本系统具有操作简单快捷、可视化、多时态、多模式显示、多用户同时使用等特点,较好的解决了用户在土地监测中出现的问题。 相似文献
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武夷山市土地利用变化遥感监测分析 总被引：1，自引：0，他引：1
针对近20年来武夷山市土地利用变化信息相对不足的问题,提出运用现代遥感与GIS技术进行武夷山市土地利用变化动态监测的方法。在分析1996年、2005年和2014年3期Landsat影像的基础上,采用监督分类方法提取土地利用信息,然后采用土地利用转移矩阵分析法和动态度分析法,分析了土地利用类型的时空变化情况及发展趋势。结果表明:1996年以来,武夷山市土地利用变化的特点表现为耕地显著增加,而林地明显减少;20年间其他未利用地和城镇的空间变化幅度很大;经济快速发展,旅游业大力发展等是武夷山市土地利用变化的驱动因素。研究结果对武夷山市的生态环境保护以及探究旅游业对土地利用变化的影响有参考价值。 相似文献
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三峡库区近30年土地利用时空变化特征分析 总被引：6，自引：0，他引：6
利用三峡库区1975年、1987年、1995年、2000年和2005年的遥感影像数据,提取各期土地利用图。以各期土地利用图为基础图件,利用G IS技术,分析了三峡库区各期土地利用类型的数量、空间分布及变化趋势,分析表明库区的耕地、林地和草地都在减少,库区近30年建设用地和河流水面的增加最为明显。同时引入土地利用变化的景观特征指数、土地利用变化速度、土地利用程度指数来总结三峡库区近30年来土地利用变化的主要时空变化特征。采用多种特征指数相结合的研究方法,有利于了解三峡库区土地利用变化的特征,可以进一步指导库区的土地利用规划,为库区的生态环境保护提供参考。 相似文献
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土地利用的时空变化可以直观地表达人类活动与自然环境的相互作用关系。以巢湖流域为例,利用多种指标,对巢湖流域1985年、2000年、2016年的数据进行分析,主要从土地利用变化动态度、土地利用状况转移矩阵、土地利用程度、土地利用重心变化4个方面进行研究。结果表明,1985―2000年、2000―2016年、1985―2016年3个时间段巢湖流域土地利用综合动态度分别为0.08%、0.12%、0.1%,表明30年来巢湖流域人类活动对土地利用的影响越来越大;1985年以来,巢湖流域土地利用类型之间的转换主要体现在耕地对建设用地的转换和水域、草地对耕地的转换,其中耕地转化为建设用地的比例最大,表明社会经济因素是土地利用变化的主要驱动因素;巢湖流域的土地利用程度较高,各县市30年来的土地利用程度各有增减;除林地和水域外,其他土地利用类型的土地利用重心都有不同程度的偏移。 相似文献
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In mountainous areas, it is the undulant terrain, various types of geomorphic and land use that make the remote sensing images great metamorphism. Moreover, due to the elevation, there are many areas covered with shadow, clouds and snow that make the images more inaccurate. As a result, it would be very difficult to carry out auto-classification of RS images in these areas. The study took Southwest China as the case study area and the TM images, SPOT images as the basic information sources assisted by the a... 相似文献
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本文选用2018年12月至2019年12月共计32景Sentinel-1升轨影像数据,基于PSI技术对贵阳市进行了形变信息提取.结果显示,监测区内共发现较大形变区24处,其中沉降区21处,抬升区3处.通过统计学方法,证明了地铁沿线并无明显形变,对形变区进行分析发现,24处形变区均与城市化建设有关,与地铁施工运行并无关系... 相似文献
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Konstantin Greger 《Transactions in GIS》2015,19(1):129-150
Detailed population information is crucial for the micro‐scale modeling and analysis of human behavior in urban areas. Since it is not available on the basis of individual persons, it has become necessary to derive data from aggregated census data. A variety of approaches have been published in the past, yet they are not entirely suitable for use in the micro‐scale context of highly urbanized areas, due mainly to their broad spatial scale and missing temporal scale. Here we introduce an enhanced approach for the spatio‐temporal estimation of building populations in highly urbanized areas. It builds upon other estimation methodologies, but extends them by introducing multiple usage categories and the temporal dimension. This allows for a more realistic representation of human activities in highly urbanized areas and the fact that populations change over time as a result of these activities. The model makes use of a variety of micro‐scale data sets to operationalize the activities and their spatio‐temporal representations. The outcome of the model provides estimated population figures for all buildings at each time step and thereby reveals spatio‐temporal behavior patterns. It can be used in a variety of applications concerning the implications of human behavior in urban areas. 相似文献
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基于被动微波遥感的青藏高原雪深反演及其结果评价 总被引：21，自引：0，他引：21
采用修正的张氏雪深反演算法，用ＳＳＭ／Ｉ３７ＧＨz和19GHz水平极化亮温值计算了青藏高原及其毗邻地区的积雪深度，对其精度进行了评价，并对误差来源进行了分析，结果显示，此算法能够较好地反映研究区的雪深分布，但局部地区误差较大，总体上雪深被高估，其误差主要来源于冻土，深霜层，植被以及雪层中液态水含量，雪粒的形状和粒径的变化带来的影响，SSM／I数据较低的分辨率和研究区复杂的地形使反演的雪深与观测的雪深缺少可比性，给精度的评价带来影响。 相似文献
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Peter Caccetta Simon Collings Andrew Devereux Kassell Hingee Don McFarlane Anthony Traylen 《International Journal of Digital Earth》2016,9(5):457-475
This paper describes the development of a system for decimetre-scale monitoring of land-surface and land-cover in urban and peri-urban environments. We describe our methodology that comprises the application of highly automated processing and analysis methods to digital aerial photography. The approach described in this paper addresses a monitoring need by providing the ability to generate change information at a spatial resolution suitable for urban, peri-urban and coastal areas, where an increasing percentage of the worlds’ population dwells. These areas are dynamic, with many environmental issues associated with planning, service provision, resource management and allocation, as well as monitoring regulatory compliance. We present a system based on standardised data and methods, which is able to track and communicate changes in features of interest in a way that has not been previously possible. We describe the methodology and then demonstrate its feasibility by applying it to geographic areas of planning and policy relevant size (the order of tens of thousands of square kilometres). We demonstrate the approach by applying it to the problem of urban forest assessment. 相似文献
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GIS中地籍宗地面积的方差分量估计 总被引：2，自引：0，他引：2
探讨在地籍宗地数字化的面积处理问题中,把已知面积数据和数字化坐标同时作为观测值的面积处理方法.采用方差分量估计,解决已知面积数据参与平差时的权的确定.通过实例分析,认为采用条件平差方差分量估计方法来对宗地面积处理,能够更加合理地调整已有面积与由数字化坐标得到的面积值之间的差异. 相似文献
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Satellite Remote Sensing, with both optical and SAR instruments, can provide distributed observations of snow cover over extended and inaccessible areas. Both instruments are complementary, but there have been limited attempts at combining their measurements. We describe a novel approach to produce monthly maps of dry and wet snow areas through application of data fusion techniques to MODIS fractional snow cover and Sentinel-1 wet snow mask, facilitated by Google Earth Engine. The method is demonstrated in a 55,000 km2 river basin in the Indian Himalayan region over a period of ∼2.5 years, although it can be applied to any areas of the world where Sentinel-1 data are routinely available. The typical underestimation of wet snow area by SAR is corrected using a digital elevation model to estimate the average melting altitude. We also present an empirical model to derive the fractional cover of wet snow from Sentinel-1. Finally, we demonstrate that Sentinel-1 effectively complements MODIS as it highlights a snowmelt phase which occurs with a decrease in snow depth but no/little decrease in snowpack area. Further developments are now needed to incorporate these high resolution observations of snow areas as inputs to hydrological models for better runoff analysis and improved management of water resources and flood risk. 相似文献
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B Venkateswara Rao 《Journal of the Indian Society of Remote Sensing》1998,26(1-2):77-93
In order to examine the influence of tectonic and morphological characteristics on the occurrence and movement of ground water in Khondalitic (garnetiferrous sillimanite gneiss) suite of rocks, hydromorphogeological studies were carried out in a typical Khondalitic terrain situated in Viziangaram district of Andhra Pradesh, India. Different land forms have been identified with the aid of visual interpretation of Landsat imagery together with ground truth data in order to prepare hydromorphogeological and lineament maps. Drainage map and topographic slope map have been prepared using toposheets. These maps and other collateral data like well yields and geophysical data have been analysed to evaluate the ground water prospective geomorphic units. Ground water prospect areas are located in shallow buried pediplains and wash plains in such a way that they are identified on gently sloping uplands situated between the lineaments. Non potential areas are those, which are, low-lying areas near the streams and high slope areas near the residual hills. It is found near low lying areas i.e., beneath the streams that the khondalite must have transformed itself into kaoline and acting as barrier evidently preventing lateral movement of ground water forcing it to accumulate in flat upland areas between two streams or lineaments. From the lithologic cross sections it is found that there are four distinct subsurface layers namely (1) top soil, (2) highly weathered khondalite (kaolinised layer), (3) moderately weathered and fractured khondalite (aquifer layer) and (4) basement of granitic gneiss. 相似文献