基于World Wind的三维地形可视化算法研究

利用SRTM的原始TIFF格式90 m分辨率高程数据,取代World Wind中的BIL格式点阵高程数据,并在World Wind中用改进的算法对原始TIFF高程数据进行精确采样,叠加相应的影像数据,以便更加方便、精确、高效地显示出三维地形.     

大桥几何监测数据去噪方法研究

提出并优化了EMD小波组合去噪法对大桥监测结果进行去噪的过程,并与EMD去噪法、小波阈值去噪法进行比较。结果表明,优化的EMD小波去噪法是一种高效的大桥动态监测信号去噪方法,去噪效果最好。     

青藏高原冷湿地生态系统CH4排放量估算

The areal extent of cold freshwater wetlands on the Tibetan Plateau is estimated to be 0.133×10 6 km 2, suggesting a significant methane potential. Methane fluxes from wet alpine meadows, peatlands, Hippuris vulgaris mires and secondary marshes were 43.18,12.96,-0.28 and 45.90 mg·m -2 ·d -1 , respectively, based on the transection studies at the Huashixia Permafrost Station from July to August 1996. Average CH 4 flux in the thaw season was extrapolated to be 5.68 g·m -2 according to the areal percentage of wetland areas in the Huashixia region. CH 4 fluxes at four fixed sites, representative of similar ecosystems, ranged from -19.384 to 347.15 mg·m -2 ·d -1 , and the average CH 4 fluxes varied from 6.54 to 71.97 mg·m -2 ·d -1 at each site from April to September 1997. CH 4 emissions at each site during the entire thaw season was estimated from 1.21 to 10.65 g·m -2 , displaying strong spatial variations. Seasonal variations of CH 4 fluxes were also observed at the four sites. It is found that CH 4 bursted in the early thaw season, and increased afterwards with rising soil temperatures. Episodic fluxes were observed in summer, which influenced the average CH 4 flux considerably. Annual CH 4 emissions from cold wetlands on the plateau were estimated at about 0.7～0.9 Tg based on the distribution of wetlands, representative CH 4 fluxes, and number of thaw days. The centers of CH 4 releasing are located in the sources of the Yangtze and Yellow Rivers, and Zoige Peatlands.     

耕地质量地球化学综合等级划分研究——以贵阳市南明区为例

针对损失函数为最小一乘,惩罚项由基数函数定义的稀疏回归问题,用SCAD(smoothly clipped absolute deviation)罚来连续逼近基数罚,得到一个连续的松弛问题,研究SCAD罚问题与原基数罚问题之间解的等价性。首先,证明了SCAD罚松弛模型的下界性质,并借助此下界性质分析了原问题与松弛问题之间解的等价性,证明了在一定条件下两个问题具有相同的全局最优解以及最优值。此外,证明了松弛模型的局部最优解是原问题的局部最优解并且在局部极小值点处松弛模型与原问题的目标值相等。