Modelling Regional Scale Surface Energy Exchanges And Cbl Growth In A Heterogeneous, Urban-Rural Landscape

Over the last decade, simple models of theconvective boundary layer (CBL) have beensuggested as an approach to inferring regionallyaveraged land-air exchanges of heat, water and tracegases, because the properties of the CBL respond toan average of the underlying small-scaleheterogeneity. This paper explores the use of anintegral CBL method to infer regionally averagedfluxes in a landscape that has at least three majorsources of heterogeneity – irrigated andnon-irrigated rural land use and a large urban area(Sacramento region, California).The first part of the paper assesses the validity ofthe simple slab model of the CBL – this isintegrated forwards in time using local-scalemeasured heat and water vapour fluxes, to predictmixed-layer depth, temperature and humidity. Of thefour different CBL growth schemes used, the Tennekesand Driedonks model is found to give the bestperformance. Evaluation of the model performancewith different weightings of heat and water vapourfluxes based on the land use characteristics in theregion suggest that the source area for theboundary-layer sonde measurements is larger thanphysically-based estimates would suggest.Finally, measured time series of potentialtemperature are used to infer regionally averagedsensible heat fluxes using an integral CBL (ICBL)method. These ICBL fluxes are compared with thosemeasured at the local scale over the three land usetypes that comprise the region of interest. They arefound to be closest to the heat fluxes calculated byappropriately weighting the measured heat fluxes inthe source area calculated for the ICBL. We concludethat the integral CBL budget method providesadequate estimates of regionally-averaged surfaceheat fluxes in a landscape that is characterised bysurface types with distinctly different surfaceenergy budgets.     

绝对重力与相对重力混合平差的基准及质量控制

绝对重力与相对重力测量混合平差是综合利用各种重力测量资料确定重力网基准，提高重力网综合质量的有效途径，文中首先从重力观测的系统误差入手，讨论重力网平差的函数模型；进而根据两类重力观测信息对重力基准的贡献，分析了不同平差方法所对应的各类基准及基统计意义与可靠性；最后对重力网平差的质量控制方法进行了讨论。     

Gravity field separation, density inversion and crustal tectonics in Kang-Dian region

IntroductionTethys-Himalya tectonic belt extends from west to east across Europe, Asia and Africa, and stops at the longitude of 104(E in China. The famous North-south active tectonic belt located in China is a part of China-Mongolia central-axis strong earthquake belt and the huge crustal thickness undulation belt. The tectonic belt is a strong extrusion, tension and shear region. It is synthesized by topography gradient belt, faults, Cenozoic basin and strong earthquake belt on north-so…     

在实际工程中怎样选择持力层厚度

就《规范》公式确定地基承载力时没限定持力层厚度这一不足提出了自己的看法，描述了各种地层组合关系时，总力与地基承载力之间的关系。     

新世纪广西的区域开发与可持续发展

分析了广西的基本区情条件，揭示了广西区域开发格局的空间变动趋势，提出了广西新世纪实施可持续发展战略的举措，即加强以交通为主的基础设施建设，开发以洪水河为主的水能资源，加快建设成为南中国西南东输的枢纽；调整和优化产业结构，确立主导产业的市场地位，提升优势产业的市场竞争力；加快城乡转型的进程，提高城镇化的水平和质量，控制人口增长、提高人口质量，治理环境污染；制度创新， 优化经济布局的区域结构。     

任意形状重磁异常三度体人机联作反演

作者在文中介绍了一种基于三角形多面体模型的重磁三维反演技术，其特点是既可通过和自动迭代方式来改变反演模型，又可通过过人机交互方式来改变模型，该技术具有较高的实用性。     

球面小波分析技术及在全球重力模型中的应用

在介绍球面小波理论的基础上,推导和比较了几种球面小波,分析了最新地球重力模型-EGM96,以此为依据,把球面小波多分辨分析用于计算全球自由空气异常及重力大地水准面,并对处理结果做出解释。     

地球重力模型及中国大陆重力场的计算

融多颗卫星数据、地面重力值和其它资料一起的地球重力模型EGM 96 ,为研究中国大陆的重力场及相关问题提供了一个高精度 36 0阶的球谐系数。在分析EGM 96的基础上 ,计算并简单解释了中国大陆的自由空气异常和布格重力异常。计算所得重力场的精度和分辨率大大高于常用的1∶140 0 0 0 0 0自由空气异常图及布格重力图     

工程地质工作中几个问题的讨论

本文针对工程地质工作实践中碰到的几个有关工程地质的基本概念与术语以及地质理论的应用问题，结合工程实际工作展开讨论，纠正与澄清有关错误与模糊认识，供工程地质工作者借鉴与参考。