高空天气图自动分析系统   总被引：4，自引：0，他引：4  

王新芝  陈必云 《南京气象学院学报》1994,17(4):477-481

介绍高空天气图自动分析系统的设计思路和主要实现技术，该系统集数据处理和图形处理技术为一体，所分析的天气系统完整无遗漏，高低压中心明确，等值线分析客观合理。  相似文献   

散乱离散点数据的三角形网格化快速成图     

李小东  金胜  王阳玲  张加洪  程励辉 《物探与化探》2015,(1):156-160

提出了一种基于三角网格的等值线成图线性插值方法。常规等值线成图都是基于矩形网格进行网格化插值的,三角网格能够更好地逼近地球物理场的形态和散乱离散点数据的边界,得到的等值线图更加光滑。通过搜索边界、三角网格化剖分、线性插值、搜索等值线、Bezier曲线光滑等值线等5个步骤,可以对任意散乱离散点数据进行快速成图。实际数据的成图结果表明:该方法插值效果好,不进行数据外推,得到的等值线图能直接反映散乱离散点数据的空间位置且成图速度快,可大大提高实际工作效率。  相似文献   

三次贝塞尔曲线拼接模型的折线式等值线曲线化应用     

王学春  尚继宏 《测绘科学》2011,36(2):192-194,235

本文通过对曾广鸿等人[1]提出的利用三次Bezier曲线拼接模型实现满足拓扑关系的折线武等值线曲线化的理论方法进行编程实践后,发现仅仅根据文中的方法不能完全正确地实现等值线的绘制,为此作者通过编程实践对该方法进行了补充与完善,文中详细完整地介绍了能完全满足拓扑关系的折线式等值线全参数曲线化的具体实现方法.  相似文献   

中国典型等降水量线年代际空间演变   总被引：3，自引：1，他引：2  

李雪萍  史兴民  王阿如娜 《中国沙漠》2016,36(1):232-238

基于1960-2013年中国573个气象站的月降水量数据,选用普通克里金插值法生成典型等降水量线(200、400,800 mm),从等降水量线移动距离和移动趋势的角度分析了中国近54年典型等降水量线的时空演变特征。结果表明:(1) 200、400,800 mm等降水量线近54年的空间分布大致呈东北-西南走向,且从西北到东南有序排列。(2) 200 mm等降水量线在宁夏平原和西藏中西部波动强烈,且均有向东和向南偏移趋势。200 mm等降水量线在宁夏平原20世纪70、80年代、21世纪初东移,20世纪90年代、21世纪10年代初西移。西藏中西部自20世纪80年代起200 mm等降水量线有西移和北移态势,新疆北部200 mm等降水量线范围不断扩大。(3) 400 mm等降水量线在华北中东部波动强烈,20世纪70年代、21世纪00年代东移,20世纪80、90年代和21世纪10年代初西移,且整体有向东和向南的偏移趋势,但年代际波动大。(4) 800 mm等降水量线在秦岭-淮河一线波动强烈,20世纪80年代、21世纪00年代北移,20世纪70、90年代、21世纪10年代初南移,且纬度降低趋势较明显。  相似文献   

东海海域潜在地震海啸的数值模拟初步研究   总被引：2，自引：0，他引：2       下载免费PDF全文

温燕林  朱元清  宋治平  薛艳  刘双庆  董非非 《地震学报》2008,30(5):456-463

针对东海冲绳海槽地区的地震地质背景,对东海海域潜在的地震海啸进行了预研究. 假设了冲绳海槽在发生8.5级大地震,断层错距高达15 m的极端地震情况引发的海啸对中国东部沿海地区的影响. 初步数值模拟结果表明,该地震引发的海啸的最大初始波高为4.3 m,4小时左右传至浙江沿岸,近岸各处波高为1——2 m,其中局部地区波高为2.4 m;约7——8小时靠近上海海岸线（若震源在中冲绳海槽地区,海啸传到上海最快大约7小时）,近岸波高约为1 m. 近岸区域地形变化复杂,海岛密布,局部地形条件可能会很大地影响实际各地点海啸波高,加上海啸在岸边爬高及港湾效应,估计波高还会升高. 给出了冲绳海槽南、中、北部发生潜在地震海啸的传播等时图. 笔者在东海设置了3个地震及海啸监测站,基于海啸模拟结果绘制了监测站处的海啸随时间演化曲线,分析了预研究成果对海啸预警可能发挥的作用.   相似文献   

煤矿3D GIS中等值线及多分辨率区域填充生成技术     

武强  徐华 《煤田地质与勘探》2004,32(5):4-6

首先建立了一种能够有效地表达矿区地质数据复杂空间分布的超体元数据模型;设计了基于B样条和基于分形的等值线连续性处理方法,以适应不同的应用需要;在此基础上,提出等值线及多分辨率区域填充设计策略,增强了基于复杂数据模型的等值线及区域填充生成方法的健壮性和稳定性,为矿山开发、矿藏评价、采矿规划等提供有效的科学手段。   相似文献   

HAND contour: a new proxy predictor of inundation extent          下载免费PDF全文

Antonio Donato Nobre  Luz Adriana Cuartas  Marcos Rodrigo Momo  Dirceu Luís Severo  Adilson Pinheiro  Carlos Afonso Nobre 《水文研究》2016,30(2):320-333

Tools for accurately predicting environmental risks, such as the location and spatial extent of potential inundation, are not widely available. A dependence on calibration and a lack of available flood data have prevented the widespread application of existing hydrodynamic methods for predicting the extent of inundation. We use the height above the nearest drainage (HAND) terrain model to develop a simple static approach for mapping the potential extent of inundation that does not depend on flood observations and extends beyond methods for mapping low‐lying areas. While relying on the contour concept, the method utilizes drainage‐normalized topography and flowpaths to delineate the relative vertical distances (drop) to the nearest river. The HAND‐delineated relative drop is an effective distributed predictor of flood potential, which is directly related to the river stage height. We validated the new HAND contour approach using a flood event in Southern Brazil for which high‐resolution maps were available. The results indicated that the flood hazard‐mapping method accurately predicted the inundation extent of the channel carrying the flood wave and the channels influenced by flooding. For channels positioned outside of the flood‐wave area, the method overestimated the actual flood extent. As an original static assessment of floodwaters across the landscape, the HAND contour method could be used to map flood hazards in areas with poor information and could promote the development of new methods for predicting hydrological hazards. Copyright © 2015 John Wiley & Sons, Ltd.  相似文献   

A new model for predicting three-dimensional beach changes by expanding Hsu and Evans' equation     

Takaaki Uda  Masumi Serizawa  Takayuki Kumada  Kazuya Sakai 《Coastal Engineering》2010

The empirical bay shape model proposed by Hsu and Evans in 1989 for predicting the static planform of a pocket beach is expanded to enable the calculation of three-dimensional beach changes on a pocket beach with a seawall. The original formulation was developed on the basis of a second-order regression analysis. Unlike the one-line model of shoreline changes, the model of Hsu and Evans does not require repeated calculations of the wave field and shoreline position, because it was derived on the assumption of null sediment movement within a pocket beach in static equilibrium, hence without the need of applying the continuity condition of total sand volume in the calculation. The expanded model proposed by the present authors satisfies the total sand budget on a pocket beach, by taking into account the concept of depth change due to longshore sand transport. Model tests were carried out and the new model was further applied to the beach changes at Kemigawa on the northeast of Tokyo Bay in Chiba Prefecture, as well as at Oarai in Ibaraki Prefecture, Japan. On both locations, seawall has been installed as countermeasures against beach erosion, where wave sheltering effect of the main breakwater and beach changes in front of the seawall has also been observed. With this expansion, the present model can be applied to predict the three-dimensional beach changes on a coast with seawall on a pocket beach.  相似文献   

地貌及等高线表示的分解定理与表现定理   总被引：3，自引：0，他引：3  

王靳辉  邱学绍 《测绘学院学报》2004,21(1):21-23

随着计算机制图和GIS的迅速发展，对于有着广泛应用的地貌形态特征问题，提出了进一步加以科学、系统、深入定量研究的迫切要求，以便获得更科学、合理的应用。作为一个系列研究的开始，首先要解决用2维空间的等高线表示3维空问地貌形态的科学性这一问题。为此，文中引入了地貌截影及截地貌的概念，通过地貌分解定理与表现定理的证明，以及等高线、地貌截影和截地貌三者之间的等价关系的论述，最终从数学上解决了上述基本问题，为今后的深入研究奠定了基础。  相似文献   

Pressure-Temperature Contours and PT Paths of the Early Precambrian Rocks through the Yinshan Area and Their Implication to the Crustal Evolution     

MEI Hualin  WU Changhua Tianjin Institute of Geology  Mineral Resources  CAGS  Tianjin.  JIN Wei Changchun University of Earth Sciences  Changchun  Jilin Hao Zhiguo Liu Xinzhu 《《地质学报》英文版》1998,72(1):14-28

Four distinct lithe-tectonic belts (zones) in the Yinshan area, North China, were identified by pressure-temperature contours and litho-tectonic features, such as the Sanggan granulite belt, Jining metasedimentary belt. Wulashan-Daqingshan front tectonic zone and Se' eratengshan belt. This area witnessed two important thermo-tectonic events. The older one is c. 2.5 Ga while the younger one c. 1.9 Ga. The Se' ertengshan Neoarchaean terrane features a clockwise PT path with the decompression ranging from > 1500 MPa to 800-1000 MPa in the Se' ertengshan belt, which implies an island arc setting. The Sanggan belt is a Mesoarchaean microcontinent reworked by Neoarchaean magma underplating, which shows an counterclockwise PT path. During the Palaeoproterozoic period, two Archaean continent (arc) collided. The Archaean basement of the Sanggan and Wulashan-Daqingshan belts overthrust northwards, the PTt paths of basement show a decompression from 1000-1200 MPa to 500-700 MPa. The PT paths of the Jining and Erda  相似文献