彩色地形图矢量化算法的设计与实现

提出了一种从彩色扫描地形图中提取等高线的方法。其中,在等高线细化方面采用局部细化的策略,在智能跟踪中提出了方向式搜索,不仅避免了像素点的重复判断,而且保证了追踪过程的正确性。采用了一些有代表性的国家标准地形图进行测试,通过计算具体度量指标对提取结果作了定量分析。实验表明该方法在实际应用中具有很好的实用性。     

基于比值法的假彩色图像增强效果对比研究

通过对遥感图像的不同波段的特征进行研究,选取合适的波段进行比值处理。然后进行比值图像的假彩色合成,从而获得其中含铁比较丰富的区域分布信息,能够为找矿工作提供有效的帮助。通过对比分析,文中论述的混合假彩色比值图像增强显示法的效果比较明显。与传统图像假彩色合成法相比,新的方法生成的合成图像不但能够突出显示出某些特征,而且还保留了详细的地形的细节信息。通过研究,本文提供的方法能够有效地对含铁岩体进行增强显示,在找矿方面具有重要的研究意义。     

基于自分类和颜色空间变换的遥感图像色彩校正方法

提出了一种基于遥感自动分类和lab 颜色空间变换的色彩校正方法, 并用此方法对不同时间的ETM遥感图像进行了多景色彩校正后的拼接实验。实验结果显示, 相对于重叠区域校正、直方图匹配等常规方法, 该方法能够很好地校正不同获取时间所导致的景间颜色、亮度差异, 提高遥感图像后续分类、变化检测的准确性以及多景遥感图像的拼接效果。     

湖北省主体功能区划方法探讨

讨论湖北省主体功能区划方法,认为湖北省主体功能区应分为6类。区划时选择县级行政区为基本分析单元,并遵循“复杂性系统工程—简单化假设处理—合理化分析识别”的总体思路;采用矩阵分类、矩阵分类与标准定位相结合两种路径,基于不同路径的主体功能适宜性评价指标体系既有共性也有差异;区划方法采用综合集成法,包括修正的熵值法和主成分分析法、系统聚类法、矩阵判断、叠加分析和缓冲分析等;区划成果在一定程度上打破了县级行政区界限,但保持乡镇行政区的相对完整性。     

Distribution of Changjiang Diluted Water detected by satellite chlorophyll-a and its interannual variation during 1998–2007

Sea-viewing Wide Field-of-view Sensor (SeaWiFS) chlorophyll-a distribution in summer in the East China Sea during 1998–2007 was analyzed. Statistical analysis with K-means clustering technique allowed us to define the proper satellite chlorophyll-a concentration indicating the Changjiang Diluted Water (CDW). The spatial distributions of the higher satellite chlorophyll-a concentrations (>0.48 mg m⁻³) corresponded well with the distributions of lower salinity CDW (<30–32) every year. Interannual variation of the CDW area, indicated by the high satellite chlorophyll-a, correlated with the interannual variation of the Changjiang summer freshwater discharge. The correlation analysis indicated that the CDW spread eastward in the East China Sea with a time lag of 1 to 2 months after the discharge.     

基于双树复小波变换图像融合方法

基于离敞小波变换的图像融合算法在特征表达上存在不足,将双树复小波变换引入到彩色图像融合中,对彩色图像的3通道分别进行融合,各通道低频取加权平均,高频去较大值的方法.融合效果评价除了使用均方根误差、峰值信噪比和熵外,还使用了通用的主观与客观相结合的方法.实验结果表明,获得的融合图像效果较好,优于离散小波融合算法.     

动态权重约束下的农村机耕路提取方法

宽度窄、路面材质与农田差异性低是农村机耕路的特点,也是导致现有模板匹配方法自动化程度低的主要因素.本文针对这一问题,提出动态权重约束下的农村机耕路提取方法.该方法首先通过改进多尺度线段方向直方图(Multi-Scale Line Segment Orientation Histogram,MLSOH)模型,对机耕路局部...     

长牡蛎壳黑选育系F7代的生长规律和模型

为研究长牡蛎壳黑选育系F7的生长规律,分别采用了线性回归方程和Von Bertalanffy、Gompertz和Logistic 3种非线性模型对长牡蛎(Crassostrea gigas)壳黑选育系F7幼虫期和养成期的生长参数进行生长模型构建,并对长牡蛎壳黑选育系F7养成期的壳高、壳长、壳宽分别与总重进行曲线拟合,以研究长牡蛎壳黑选育系F7的生长规律。研究表明,幼虫期壳高、壳长对日龄的回归方程分别为y=39.723 8+11.697 2x,R^2=0.991;y=31.346 2+9.802 8x,R^2=0.986。壳高与壳长成线性相关,回归方程为y=4.867 0+1.175 0x,R^2=0.989。养成期长牡蛎壳黑选育系F7的总重增长与Von Bertalanffy生长模型最符,R^2=0.955;长牡蛎壳黑选育系F7的总重与壳高、总重与壳长、总重与壳宽分别遵循复合曲线y=0.706×1.055~x,R^2=0.991、y=1.336×1.075~x,R^2=0.983、y=1.287×1.154~x,R^2=0.944。     

Satellite and in situ observations of the bio-optical signatures of two mesoscale eddies in the Sargasso Sea

Satellite ocean-color imagery and field spectroradiometer observations are used to assess the bio-optical signatures of two mesoscale features, a cyclone C1 and an 18°-water anticyclone A4, in the Sargasso Sea. Field determinations of upper layer bio-optical properties, such as the diffuse attenuation coefficient and remote-sensing reflectance spectra, show little statistically significant variations with distance to the eddy center for either eddy. This contrasts field observations showing many-fold higher phytoplankton pigment biomass at depth (and for A4 higher primary production rates at depth) than is typical for this region. The cyclone C1 does show a significant decrease in the depth of the 1% photosynthetically available radiation (PAR) isolume with increasing distance from eddy center while the anticyclone A4 shows no coherent signal vs. distance. Vertical profiles of bio-optical properties show consistent patterns where subsurface maxima are displaced higher inside the core of the cyclone C1 than in the surrounding waters while the highest values of the diffuse attenuation coefficient at 443 nm are observed within the core of anticyclone A4. Satellite observations of near-surface bio-optical properties show signals consistent with eddy physical characteristics, although the magnitude of these variations is very small, barely detectable by typical field measurement protocols. Mean values of bio-optical properties are higher within the cyclone compared with its periphery but not for the anticyclone. For both eddies, significant inverse correlations are observed between time series of bio-optical properties and eddy center sea-level anomaly. Consistent response to wind speed is also noted: following strong wind events, bio-optical parameters are elevated inside the anticyclone and are reduced inside the cyclone. These observations demonstrate that a combination of physical processes, including vertical eddy uplift, eddy horizontal advection, and eddy-scale Ekman pumping, contribute to the bio-optical imprint of mesoscale eddies. The contributions of these forcing mechanisms change over the period of observation, illustrating the limitations of inferring eddy bio-optical dynamics from short-term, field observations. The present analyses provide insights into the potential as well as the drawbacks of bio-optical techniques for probing the biological and biogeochemical impacts of open-ocean eddies.     

水体后向散射系数校正方法研究

后向散射系数是水色反演半分析模型的重要参数,后向散射系数的测量与分析是固有光学测量与分析的重要组成部分。为了更准确的获得后向散射系数数据,根据不同的实际测量情况提出了两种后向散射系数数据的校正方法,即利用散射与后向散射系数模型计算的散射系数替代法和实测数据替代法。结果表明这两种方法在比传统的数据校正方法有明显的优势,是一种符合水体剖面固有光学特性规律的数据校正方法。