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Given a planar point set,the moving least squaremethod is adopted to denoise and resample it so that the resulting point set is with low noise and uniform sampling density.Then the reliable signed distance field of the preprocessed point set is constructed by using the Level Set method.Finally,an algebraic B-spline function is adopted to fit the signed distance field by solving a linear equation system.

首先给定一个表示封闭曲线、可能带有噪音且分布不均匀的平面点,采用移动最小平方(moving least square,简称MLS)方法对点去噪、重采样,得到一个低噪音、分布均匀的"线状"点,再通过Level Set方法建立该"线状"点的离散几何距离场,最后用一个代数B-样条函数光顺拟合该离散距离场,代数函数的零点集即为重建曲线。

Flanked by the Auspicious Cloud and Mountainous Cloud peaks,the 6.5-meter-high Cloud-Capped Peak, the highest limestone in the classical gardens of Suzhou, is believed to be left behind by the imperial collector of the Northern Song Dynasty,Mass of buildings, including the Old Hermit Scholars' House, the Cloud-Capped Tower,the Cloud-Capped Terrace and the Awaiting Cloud Temple,are put up to give emphasis to the Cloud-Capped Tower, The northern part is now a bonsai garden in which about 500 valuable bonsai are put on display.

该区由吉祥和山区高峰,在650多米高的层覆盖山顶,最高石灰石在苏州古典园林,被认为是不甘落后,由皇室收藏的北宋时期,大规模的建筑物,其中包括旧的隐士学者之家,上限管制塔,帽阳台和等待寺,是付诸行动,以重点抓了层上限大楼北方部分现在是一个盆景园,其中约500个宝贵的盆景放在汇演。

Based on the obtained the temperature, the electron density of the cloud lightning channel by combined with the method of the spectra diagnose and Saha equation.

论文摘要:用无狭缝光栅摄谱仪在西藏地区获得了闪放电通道的光谱,在已经获得闪放电通道温度的基础上,利用光谱诊断方法结合Saha方程得到了闪放电通道的电子密度;将空气等离子体的输运理论应用于闪电放电通道特性的研究,首次计算了三次闪放电通道的电导率、电子的热导率和热扩散系数。

In order to get the strong convective cloud characteristics exhibiting in satellite images, about 20000 hourly gauge data of 333 surface rainfall stations and corresponding 4000 IR digital cloud images of GMS 4 during the period of 1992~1994 in Henan, Hubei and Sichuan provinces were analyzed.

对1992~1994年夏季四川、湖北、河南3省333个地面雨量站2万多个雨量观测数据以及与之相应的4千余幅GMS-4红外数字图资料的分析结果表明,顶温度、温度梯度、团的膨胀、穿透性顶的存在、体相对于团中心的偏离量与的降水强度有着明显的对应关系。

The model results show that the hail embryos are mainly graupel particles.Solid phase precipitation accounts for 46% of ground precipitation amount and graupel-fall is 65% of solid phase precipitation.Graupel particles grow by accretion with rainwater and cloud water.Accumulation zone of supercooled water...

结果表明:玛曲冰雹中冰雹胚胎以霰胚为主;在地面降水中,固态降水占降水总量的46%,而霰占固态降水的65%,霰主要靠撞冻雨水和水增长;雹中存在较弱的过冷雨水累积带,累积带的维持时间也很短,累积带中的过冷雨水有利于雹块的增长,但不起主要作用;雹块的增长主要是通过雹撞冻水,其次是撞冻雨水增长。

Terrain heightened can enhance blocking effect, which lead to strengthen water vapor flux divergence and vertical convection, and cloud water increases but centralizes in the middle-low level. This change intensify accretion of snow by collecting more supercooled cloud water, and rain water converts into graupel by collecting more snow, and dry growth of graupel increase at the same time. Rain water augment because of more graupel melting, and rain water continue to increase by collecting cloud water in the low level.

地形高度增加后,阻挡作用加强,使水汽通量辐合加强,垂直气流增大,中低层水增多,导致雪撞冻过冷水增多,促使了雨水撞冻雪转化为霰和霰干增长过程的加强,霰融化为雨水增多,低层雨水碰并水加强,冷过程得到增强。

Judge clouds' effect on solar radiation by satellite cloud map gray scale values, therefore establish and confirm the relationship between them. Roughly acquire optical depth of clear sky and clouds from radiation station data and routine meteorological data of land surface, and the study the relationship between clouds' physical character and radiation....

通过卫星图的计数值来判断对辐射的作用,以此建立起它们之间的关系;利用地面观测资料和常规资料来粗略求取晴空大气和光学厚度,进而研究的物理属性与辐射关系;简单的获取地表与近地面大气之间的辐射关系,以此估算地表的反照率,和地表的净辐射;分析了卫星可见光、红外及水汽图计数值和地面辐射之间关系,利用辐射传输公式来推倒和分析对辐射的关系,试图建立起卫星测值与地表总辐射和净辐射之间的关系,并将晴空和有的个例分开,分别建立并选出最佳模式,以此来估算地表的净辐射和总辐射。

Lines/mm holographic gratings in ultra low expansion mold plate were replicated onto the cross section of the measured sections in a ball grid array electronic package and a quad flat package.

应用1200线/毫米的纹光栅并结合纹干涉法,电子束纹法,原子力纹法,扫描电镜纹法测量QFP和BGA型电子封装组件的热变形。

The results calculated show that the major contributions for the backscattering cross section come possibly from average cloud diameter, clear-air and humidity turbulence and also from distributions of cloud particles, especially, at higher frequencies.

再分析了的后向散射机理,计算了西安地区的后向散射截面;表明影响的后向散射截面的主要因素为滴平均半径、大气湿度湍流及粒子分布,在较高频率时更显著。

The altostratus base is 2 km high, and cloud top is higher than 5 km. The supercooled water exists abundantly in the cloud, the maximum is up to 0.21 g.m-3 at -11.20℃, but its distribution is not homogeneous, 87%of continuous distribution width are less than 2.4 km, which is disadvantage to the rime increasing of ice crystal in the cloud. Meanwhile, the evaporation effect of subcloud raindrop is very big, the diameter of raindrops which could not arrive the ground is less than 1 mm. Therefore, The cold vortex process produces the weak precipitation.

As底高2 km,顶高大于5 km,中存在比较大的过冷水区,-11.2℃时的过冷水含量0.21 g.m-3,但过冷水的含量分布极不均匀,大于0.05 g.m-3的过冷水区连续分布的宽度87%小于2.4 km,不利于中冰晶的连续凇附增长;同时下雨滴的蒸发效应大,直径小于1.0 mm的雨滴难以落到地面,因此本次过程只产生弱的降水。

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