Terrain radiometric calibration of airborne UAVSAR for forested area     

CHENG Xiaoguang  Naiara PINTO  GONG Jianya 《地球空间信息科学学报》2012,15(4)

  相似文献   

归一化光谱分解模型在城市化信息提取中的应用     

马勇刚  李宏 《地理空间信息》2012,10(4):40-41,44

以2001年7月11日LandsatETM7影像和2009年7月16日TM影像为数据源,基于V-I-S理论模型,采用归一化光谱分解模型提取了乌鲁木齐市区范围内2个时段的植被、土壤、不透水层3个连续地表参数分量。通过对不透水层不同阈值的划分,提取了2时段的乌鲁木齐市城市发展的空间信息,结果较为满意;通过空间叠加计算方式获取了8年来乌鲁木齐市城市化发展的空间信息和主要拓展方向。结果表明,乌鲁木齐城市化发展速度较快,特别是北扩趋势显著。  相似文献   

利用CG-5重力仪标定动态检定场     

肖凡  张宏伟 《地理空间信息》2012,10(4):126-128

介绍了使用CG-5相对重力仪对宝坻重力仪动态精度检定场进行标定的情况,并对观测成果精度进行了分析,实现了对检定场的成功标定。  相似文献   

多时相遥感影像辐射归一化方法综述   总被引：2，自引：0，他引：2  

余晓敏  邹勤 《测绘与空间地理信息》2012,(6):8-12

多时相遥感影像的辐射归一化是进行变化检测或拼接不可缺少的步骤。本文从绝对辐射归一化和相对辐射归一化两个方面对现有的多时相遥感影像辐射归一化方法进行了总结。对各种辐射归一化方法进行了剖析,并指出了这些方法的优缺点和适应性。最后对多时相遥感影像辐射归一化方法未来的发展进行了展望。  相似文献   

一次罕见飑前强降雹超级单体风暴特征分析   总被引：29，自引：14，他引：15  

戴建华  陶岚  丁杨  王元  陈雷 《气象学报》2012,70(4):609-627

2009年6月5日,受一个飑线前超级单体雷暴的影响,上海部分地区出现了直径25—30mm的冰雹,随后,飑线尾随该超级单体扫过上海,造成大风、雷电和强降水天气。基于常规天气观测、多普勒天气雷达、风廓线仪和自动气象站等资料分析发现,该超级单体发生在东北冷涡西南侧的高空强冷平流与低空暖平流形成的强不稳定层结背景下,超级单体风暴发生、发展在飑线前的暖区中,经过由"热岛效应"和海陆风锋共同形成的低空辐合线时明显加强发展;该风暴呈现出"指"状、"楔"状、弱回波区(WER)等超级单体雷达反射率特征,"指"状回波处出现了中气旋的径向速度特征,具有标志大冰雹的三体散射长钉(TBSS)特征回波,通过三体散射长钉多普勒速度发现了大冰雹的下降区和增长区。分析还表明:东北冷涡西南侧横槽南摆导致中空降温,0℃层和-20℃层高度明显下降,为冰雹的空中增长提供较好的温度环境条件,较低的0℃层也保证冰雹在空中下落中融化较少。双风廓线仪对比观测表明,超级单体发展的低空风场环境中具有较大的垂直风切变和风暴相对螺旋度,中尺度对流系统与环境场的相互作用形成了有利于风暴发展和维持的正反馈机制。飑线前超级单体雷暴与飑线主体关系密切,起到类似"箭"与"弓"的引导作用,飑线主体的一部分进入超级单体所遗留下的"冷"区后明显减弱,东侧入海后也逐渐减弱,其余部分仍在发展加强;最终,强风暴逐渐减弱,超级单体特征也开始消失,飑线与之合并形成新的"人"字型中尺度对流系统,新的"弓"形回波带与原回波带相比移动方向发生右偏,因此,飑前超级单体在飑线主体移动和演变的临近预报中有重要指示意义。  相似文献   

A Study of Surface Humidity Changes in China During the Recent 50 Years   总被引：2，自引：1，他引：1       下载免费PDF全文

SONG Yafang  LIU Yanju  DING Yihui 《Acta Meteorologica Sinica》2012,26(5):541-553

This paper analyzes in detail the characteristics of surface humidity changes in China under the background of global warming in the recent 50 years by using the observation data compiled by the National Meteorological Information Center of China. The results reveal that (1) with the increase of temperature,surface saturation specific humidity (qs) shows basically an exponential growth, according to the Clausius-Clapeyron equation. The nationwide average moistening rate in winter is obviously less than the annual average rate and the summer rate. There are some regional differences in qstrends in different regions of China. For example, qsin central and eastern parts of China exhibits a reducing trend in summer, consistent with the weakening trend of temperature in these areas; (2) except parts of South China and Jianghuai Region in eastern China, unanimously increasing trends of annual and winter specific humidity (q) are found in most of China, especially in western China. In summer, except parts of Northeast China, Northwest China, and some areas over the Qinghai-Tibetan Plateau, the decreasing and drying trends are significant in most of China, which is not consistent with the global mean situation; (3) the surface relative humidity(RH) in most of China shows a reducing trend. One of the major reasons for the reduction of RH is that the increasing rates of q are smaller than those of qs. Nonetheless, upward trends of RH in central and eastern China mainly due to the cooling temperature and rising q in these regions are observed in summer, leading to more precipitation. From about 2003 or so, qshas remarkably increased while q has sharply decreased in most parts of China; therefore, RH has reduced to a great extent. This may be closely related to the persistent growth of drought areas in China in the recent 10 years.  相似文献   

一种确定联合反演中相对权比的两步法   总被引：2，自引：1，他引：1  

王乐洋  许才军  张朝玉 《测绘学报》2012,41(1):19-0

提出确定联合反演中相对权比的两步法。第1步是不考虑相对权比,建立两类或多类数据的联合反演模型,通过赫尔墨特方差分量估计使得两类或多类观测数据的单位权方差相等（或单位权方差的比值接近1）,从而理论上确定观测数据合理的权阵,同时对不同种类数据进行归一化;第2步是在获得合理的观测数据权阵之后,建立顾及相对权比的联合反演模型,...  相似文献   

不同强风样本湍流特性参数的计算分析   总被引：1，自引：1，他引：0       下载免费PDF全文

李亚春  武金岗  谢志清  焦圣明  刘聪 《应用气象学报》2008,19(1):28-34

在结构风工程中, 风湍流统计参数计算的正确与否直接影响到风荷载的计算精度。在实际风参数计算与分析中, 多选用风速较大的样本资料, 但过分强调大风可能产生不合理的计算结果。利用超声风速仪瞬时风速观测资料, 分别划分成相对强风和持续强风样本, 计算并比较其湍流统计特性参数, 发现湍流统计参数特性值 (湍流度、阵风因子、摩擦速度等) 与风速大小并不能很好匹配, 有时风速不大但其湍流特性值却很大, 反之也然。研究表明:选取的湍流风资料样本或统计方法不同, 都会影响风特性参数的计算结果, 进而影响到风荷载计算的精度。这一结果对于提高结构风工程中风参数计算与设计的科学性和合理性具有现实意义。  相似文献   

Evaluation of directional normalization methods for Landsat TM/ETM+ over primary Amazonian lowland forests     

《International Journal of Applied Earth Observation and Geoinformation》2017

Biodiversity mapping in extensive tropical forest areas poses a major challenge for the interpretation of Landsat images, because floristically clearly distinct forest types may show little difference in reflectance. In such cases, the effects of the bidirectional reflection distribution function (BRDF) can be sufficiently strong to cause erroneous image interpretation and classification. Since the opening of the Landsat archive in 2008, several BRDF normalization methods for Landsat have been developed. The simplest of these consist of an empirical view angle normalization, whereas more complex approaches apply the semi-empirical Ross–Li BRDF model and the MODIS MCD43-series of products to normalize directional Landsat reflectance to standard view and solar angles. Here we quantify the effect of surface anisotropy on Landsat TM/ETM+ images over old-growth Amazonian forests, and evaluate five angular normalization approaches. Even for the narrow swath of the Landsat sensors, we observed directional effects in all spectral bands. Those normalization methods that are based on removing the surface reflectance gradient as observed in each image were adequate to normalize TM/ETM+ imagery to nadir viewing, but were less suitable for multitemporal analysis when the solar vector varied strongly among images. Approaches based on the MODIS BRDF model parameters successfully reduced directional effects in the visible bands, but removed only half of the systematic errors in the infrared bands. The best results were obtained when the semi-empirical BRDF model was calibrated using pairs of Landsat observation. This method produces a single set of BRDF parameters, which can then be used to operationally normalize Landsat TM/ETM+ imagery over Amazonian forests to nadir viewing and a standard solar configuration.  相似文献   

Soil erosion and sediment transport in Tanzania: Part II – sedimentological evidence of phased land degradation     

Maarten Wynants  Aloyce Patrick  Linus Munishi  Kelvin Mtei  Samuel Bodé  Alex Taylor  Geoffrey Millward  Neil Roberts  David Gilvear  Patrick Ndakidemi  Pascal Boeckx  William H. Blake 《地球表面变化过程与地形》2021,46(15):3112-3126

Soil resources in parts of Tanzania are rapidly being depleted by increased rates of soil erosion and downstream sediment transport, threatening ecosystem health, water and livelihood security in the region. However, incomplete understanding to what effect the dynamics of soil erosion and sediment transport are responding to land-use changes and climatic variability are hindering the actions needed to future-proof Tanzanian land-use practices. Complementary environmental diagnostic tools were applied to reconstruct the rates and sources of sedimentation over time in three Tanzanian river systems that have experienced changing land use and climatic conditions. Detailed historical analysis of sediment deposits revealed drastic changes in sediment yield and source contributions. Quantitative sedimentation reconstruction using radionuclide dating showed a 20-fold increase in sediment yield over the past 120 years. The observed dramatic increase in sediment yield is most likely driven by increasing land-use pressures. Deforestation, cropland expansion and increasing grazing pressures resulted into accelerating rates of sheet erosion. A regime shift after years of progressive soil degradation and convergence of surface flows resulted into a highly incised landscape, where high amounts of eroded soil from throughout the catchment are rapidly transported downstream by strongly connected ephemeral drainage networks. By integrating complementary spatial and temporal evidence bases, this study demonstrated links between land-use change, increased soil erosion and downstream sedimentation. Such evidence can guide stakeholders and policy makers in the design of targeted management interventions to safeguard future soil health and water quality.  相似文献