新月形沙丘迎风坡气流加速模拟

迎风坡气流加速是决定新月形沙丘发育和形态的动力因子，研究这一加速过程的定量关系有利于认识沙丘的发育、沙丘的形态、沙丘的运动等。通过大量的野外实测数据和前人的理论分析，得出沙丘迎风坡气流加速量主要和沙丘坡度、迎风坡前来流风速以及沙丘高度有关，并建立了新月形沙丘迎风坡气流加速和沙丘形态特征的定量关系。根据这一关系得了在风力较强的风沙环境中，沙丘坡度较小；在风力较弱的风沙环境中，沙丘坡度较陡。地表粗糙度越大，迎风坡坡度越陡。沙丘地貌发育高度存在一上限，这一上限与边界层厚度有关。     

地图图斑形状特征的量化及其分形模型研究

运用分形几何原理，提出了量化地图图斑形状特征的分形模型，讨论了模型中的参数──形状因子和分维的意义及求法，给出了制图现象形状特征量化的一种新途径。     

应用随机辐射传输模型反演云南松林分郁闭度

随机辐射传输模型可用于模拟水平分布不均一森林的辐射传输过程。本文以云南松林分为研究对象，提出一种应用随机辐射传输模型的郁闭度反演方法。该方法以随机辐射传输模型中参数与林分郁闭度的定量关系为基础，提出了针对云南松的冠型等效模型，构建了郁闭度和卫星反射率（GF-1和Landsat 8卫星影像）的查找表，并实施了反演。基于野外实测的30个样地进行了郁闭度数据验证，并和基于NDVI回归模型的反演方法进行对比。结果表明，反演结果能够较准确反映云南松林分郁闭状况（R²=0.8345，RMSE=0.0688），通过冠型修正能够降低反演误差，冠型等效模型是合理的。反演方法机理清晰且适用范围广，研究成果可为大面积森林郁闭度反演提供模型和方法支持。     

康定,东川两地段强震活动对比及在川滇强震预测中的意义

本文提出了具有相似活动构造背景的强震多发段康定段和东川段。对两者历史强震迁移和与川滇大地震的紧密联系,作了较有说服力的多次震例证明,因而本文所论及的有关活动特征在川滇未来强震预测中有一定参考价值。     

中国西部岩浆岩型铜镍矿床的元素组合特征及伴生金的赋存状态研究

我国西部岩浆岩型铜镍矿床伴生金与主金属元素组合,Au—Cu组合具有同步富集特征,而Au—Ni组合为不相关;伴生金与微量元素组合,Au—Pt、Au—Pd、Au—Se、Au—Te呈正相关Au—Co、Au—Os、Au—Ru、Au—Ir、Au—Rh为不相关的组合特征.该类型铜镍矿床伴生金以矿物态赋存为主,分散金较少,主要载体为黄铜矿及其它硫化物.     

The importance of grain size and shape in controlling the dispersion of the Vedde cryptotephra

Volcanic ash is dispersed in the atmosphere according to meteorology and particle properties, including size and shape. However, the multiple definitions of size and shape for non-spherical particles affect our ability to use physical particle properties to understand tephra transport. Moreover, although particles are often excluded from operational ash dispersion model setups, ash in tephra deposits 1000 km from source can exceed . Here we measure the shape and size of samples of Vedde ash from Iceland, an exceptionally widespread tephra layer in Europe, collected in Iceland and Norway. Using X-ray computed tomography and optical microscopy, we show that distal ash is more anisotropic than proximate ash, suggesting that shape exerts an important control on tephra dispersion. Shape also impacts particle size measurements. Particle long axis, a parameter often reported by tephrochronologists, is on average greater than geometric size, used by dispersion modellers. By using geometric size and quantifying shape, we can explain the transport of Vedde ash particles more than 1200 km from source. We define a set of best practices for measuring the size and shape of cryptotephra shards and discuss the benefits and limitations of using physical particle properties to understand cryptotephra transport.     

Statistical Revision of the Moment Method

The moment method is a well known technique, which uses a time series ofthe first 3 moments of a spectral line, to estimate the (discrete) modeparameters and m. The method, contrary to Doppler imaging,also yields other interesting(real-valued) parameters such as the inclination angle i, or v sin i,during its identification procedure.In this paper, we are not only interested in the estimation of thesereal-valued parameters themselves but also inreliable estimates for their uncertainty.We designed a statistical formalism for the moment method based on theso-called generalized estimating equations (GEE). This formalismaims to estimate the uncertainty of the real-valued parameters taking intoaccount that the different moments of a line profile are correlated and –more importantly – that the uncertainty of the observed moments depends onthe pulsation parameters. The latter property of the moment method makesthe least-squares technique a poor choice to estimate the uncertainty ofthe real-valued parameters. We implemented the GEE method and presentan application to a high-resolution spectroscopic dataset of the slowly pulsating B star HD181558.     

增强电子地图表现力的几个方面

电子地图是一种新兴的地图产品，正服务于社会的各行各业，提高电子地图的表现力，加大电子地图的服务力度，是人们对它的客观要求。但是，电子地图的设计坂理和方法还远远没有解决，电子地图的制作还没有统一的规范和标准。本文从图形界面、表现内容、功能接口等各方面，对加强电子地图表现力和改善它的制作方法进行了研究，这些具体的措施和方法在笔者制作的各种电子地图中得到了体现，反映很好。     

层积云覆盖的海洋边界层云详细微物理过程的数值模拟

文中建立了一个含显式分档的云微物理模式和辐射传输模式的一维 3阶湍流闭合模式 ,该模式可用于研究海洋边界层云中气溶胶和云的相互作用过程 ,同时提出了一种新的动力模式和微物理模式耦合方法 ,该方法可使动力模式中液态水相关项可以直接由微物理模式变量计算得到。作为模式的初步应用模拟了 2 0 0 1年APEX/ACE Asia在西太平洋上所观测到的一个个例。模拟结果和观测资料比较表明该模式基本上模拟出层积云覆盖的海洋边界层的基本结构