On terrain corrections in terrestrial heat flow     

Tien-Chang Lee 《Pure and Applied Geophysics》1991,135(1):1-13

The theory of heat-flow variation over a Lees-type hill is well known for evaluating terrain effects on terrestrial heat flow. However, a hill cannot be converted into a valley by simply changing the sign of one of the terrain-defining parameters, nor can several Lees' hills be superposed to simulate a series of hills and valleys for correcting a terrain-induced disturbance of heat flow. The proper derivations for a Lees-type valley are presented and the superposition is compared with analytic solutions for two parallel semi-cylindrical valleys and two semi-spherical basins embedded in an otherwise planar ground. Generally, heat flux climaxes over central valleys or basins, and dips toward their margins where rapid change in topography occurs. Variation of heat flux induced by a three-dimensional terrain is relatively large, as compared to two-dimensional features, but its areal extent is relatively limited. The two-dimensional effects also extend relatively deeper. In applying two-dimensional algorithms to a three-dimensional terrain, the correction may be over- or underestimated depending on the distance from a borehole to prominent terrain features in the surrounding area.  相似文献   

土壤地理研究的发展     

龚子同 《地球科学进展》1991,6(3):44-49

作者围绕14届国际土壤科学大会,介绍了国际土壤分类、土壤调查制图、世界土壤和土地数字化数据库、东亚土壤地理和土壤全球变化等方面研究的最新进展,指出我国应把土壤地理研究置于全球变化的总目标下,加强中国土壤系统分类的研究,开展1∶100万土壤—土地数字化数据库的工作、建立土壤地理信息系统以及防治土壤退化保证农业的持续发展。  相似文献   

黄河三角洲水冰险情预警信息系统设计与分析应用探讨     

狄小春  励惠国  陈峰  唐新桥  宫汝俊  田志刚 《遥感学报》1990,(3)

本文探讨了黄河三角洲地区水冰灾情信息系统的建立方法及其应用问题。介绍了该系统的设计原则,数据结构,建立方法和程序,并对其应用进行了分析研究。该方法也适用于其它区域。  相似文献   

Hybrid terrain rendering based on the external edge primitive     

E.G. Paredes  M. Amor  M. Bóo  J.D. Bruguera  J. Döllner 《International journal of geographical information science》2016,30(6):1095-1116

Hybrid terrain models combine large regular data sets and high-resolution irregular meshes [triangulated irregular network (TIN)] for topographically and morphologically complex terrain features such as man-made microstructures or cliffs. In this paper, a new method to generate and visualize this kind of 3D hybrid terrain models is presented. This method can integrate geographic data sets from multiple sources without a remeshing process to combine the heterogeneous data of the different models. At the same time, the original data sets are preserved without modification, and, thus, TIN meshes can be easily edited and replaced, among other features. Specifically, our approach is based on the utilization of the external edges of convexified TINs as the fundamental primitive to tessellate the space between both types of meshes. Our proposal is eminently parallel, requires only a minimal preprocessing phase, and minimizes the storage requirements when compared with the previous proposals.  相似文献   

五台山积雪变化趋势及其影响因素     

范强  刘楠  任天晨 《水文》2023,43(4):111-115

基于MODIS积雪产品与微波遥感数据,分析五台山2000—2019水文年积雪时空分布、变化趋势及与影响因素的Pearson相关性,结果表明：（1）五台山积雪期为10月至翌年4月,年内呈单峰型变化趋势,积雪集中于西北部。（2）积雪面积和积雪日数的年际变化呈显著减少趋势（p<0.05）。（3）积雪面积和积雪日数与海拔正相关,积雪面积在北坡高于南坡。（4）积雪面积与气温相关程度高于降水量,积雪面积在年内与气温和降水量日值呈显著负相关（p<0.05）,在年际与气温年均值呈显著负相关（p<0.05）。  相似文献   

从水汽角度对青藏高原东南侧高空探测布局的分析     

段玮  段旭  徐开  杨家康 《高原气象》2015,34(2):307-317

水汽是大气探测最关心的要素之一。从青藏高原东南侧出发,以NCEP再分析资料为基础,利用水汽气候诊断方法结合区域地形研究了该区域的水汽分布、输送与辐合辐散特征,并讨论了探空站布局。水汽输送分布与大气可降水季节差异均表明,青藏高原东南侧是夏、秋季东亚季风和南亚季风影响的季风过渡区,也是东亚地区最主要的水汽通道之一,尤其在秋、冬、春季此通道的水汽输送更为关键。青藏高原东南侧的大气可降水量比西南侧明显要大,这与低纬高原和青藏高原南侧南凸弧形构成的地形组合有着密切关系。青藏高原东南侧地形对水汽辐合、辐散的影响具有复杂性和特殊性,既有经向、纬向差异也有高低层差异。复杂的水汽分布及输送特征需要加强水汽探测。通过对水汽探测关键区的量化研究表明,滇西北—藏东南—缅北地区、滇东—黔西地区以及滇西南地区是观测需求较为显著的区域。  相似文献   

吉林省地体构造的基本特征   总被引：8，自引：1，他引：8  

毕守业  王德荣 《吉林地质》1995,14(1):1-14

吉林省地体构造的一个显著特征是在早古生代以前，伊舒断裂两侧分属两个不同的大地构造单元，西侧的构造环境与华北大陆板块北缘相似，为受古蒙古洋作用的早生代活动陆缘，东侧为长白山一张广才岭地体添加带（也称联合地体（省内包括吉林－延边古生代增生褶皱带及辽吉台块。其中辽吉台块于新元古代到早寒纪位于赤道附的，以后沿巨型拆离面逐渐北移，于二叠纪末沿辉发河－古洞河拼贴带，与吉林一延边古生代陆缘增生褶皱带拼贴到一起。  相似文献   

Identification of topographic settings conducive to landsliding from dem in Nelson county,Virginia, U.S.A.     

Jay Gao 《地球表面变化过程与地形》1993,18(7):579-591

  相似文献   

Terrain generalization with line integral convolution     

Bernhard Jenny 《制图学和地理信息科学》2021,48(1):78-92

ABSTRACT

Line integral convolution is a technique originally developed for visualizing vector fields, such as wind or water directions, that places densely packed lines following the direction of movement. Geisthövel and Hurni adapted line integral convolution to terrain generalization in 2018. Their method successfully removes details and retains sharp mountain ridges; it is particularly suited for creating generalized shaded relief. This paper extends line integral convolution generalization with a series of enhancements to reduce spurious artifacts, accentuate mountain ridges, control the level of detail in mountain slopes, and preserve sharp transitions to flat areas. The enhanced line integral convolution generalization effectively removes excessive terrain details without changing the position of terrain features. Sharp mountain ridgelines are accentuated, and transitions to flat waterbodies and valley bottoms are preserved. Shaded relief imagery derived from generalized elevation models is visually pleasing and resembles manually produced shaded relief.  相似文献   

基于OpenGL的地形三维可视化研究   总被引：6，自引：0，他引：6  

曾洪云  孙在宏  乔伟峰 《现代测绘》2003,26(3):29-31

本文利用OpenGL开放图形库的200多个函数,在前人对三维可视化研究的基础上,基于实际生产中的需求,提出一种可行的“二次简化法”,实践证明,这种处理方法能够使生产出的三维地形图在兼顾高度逼真的同时,能够实际地处理空间分析操作运算,满足了生产中的需要。  相似文献