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地形坐标系差微差一致性中尺度方程组
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作者 孙汉群 《南京大学学报(自然科学版)》 CAS CSCD 1992年第2期310-316,共7页
本文根据差微差一致的坐标变换原理,将笛卡尔坐标系中的中尺度方程组变换成为地形坐标系中的中尺度方程组。所得方程组不但克服了山经典坐标变换带来的气压梯度力项计算的困难,而且和通常的差微差一致变换得到的方程组比它不包含有复杂... 本文根据差微差一致的坐标变换原理,将笛卡尔坐标系中的中尺度方程组变换成为地形坐标系中的中尺度方程组。所得方程组不但克服了山经典坐标变换带来的气压梯度力项计算的困难,而且和通常的差微差一致变换得到的方程组比它不包含有复杂的余项,具有计算简便的优点。 展开更多
关键词 地形坐标系 差微差一致性 中尺度
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地形追随坐标系下埃特尔位涡的计算 被引量:1
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作者 李政 费建芳 +1 位作者 黄小刚 程小平 《气象学报》 CAS CSCD 北大核心 2017年第6期1011-1026,共16页
随着数值天气预报模式的日益普及以及位涡在不同天气、气候时、空尺度上的广泛应用,对采用模式输出资料计算的埃特尔(Ertel)位涡的精度提出了更高要求。将气象要素从中尺度模式普遍采用的地形追随坐标系向定义位涡的z或p坐标系的插值过... 随着数值天气预报模式的日益普及以及位涡在不同天气、气候时、空尺度上的广泛应用,对采用模式输出资料计算的埃特尔(Ertel)位涡的精度提出了更高要求。将气象要素从中尺度模式普遍采用的地形追随坐标系向定义位涡的z或p坐标系的插值过程(插值法),是导致埃特尔位涡计算误差的主要原因。文中利用地形追随坐标系与z(p)坐标系的变换关系,导出了z坐标系定义的埃特尔位涡在地形追随坐标系中的表达形式,实现了直接在模式格点上计算埃特尔位涡(直接法),在提高计算精度的同时,保留了其在z坐标系中的物理意义,方便了分析与应用。为了进一步分析直接法在减少计算误差方面的作用,使用WRF模式对2016年7月发生在华北地区复杂地形背景下的一次黄淮气旋爆发过程进行了模拟,利用模式输出资料对此次天气过程中强降水时段插值法计算误差的分布进行了分析。结果表明,利用直接法计算位涡可有效减少插值法引入的计算误差,中低层均方根误差可达0.5 PVU,中高层可达0.3 PVU。将其应用到中小尺度对流性天气精细化结构的分析及气候统计研究中,可以有效减少插值法误差对结果产生的不良影响,提高计算和分析准确度。 展开更多
关键词 地形追随坐标系 Ertel位涡 计算误差
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M—γ尺度G—Chen坐标系中气候模式的研制 被引量:1
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作者 张洪涛 武永利 +1 位作者 胡良温 任爱萍 《山西气象》 2000年第4期17-30,共14页
本文在地形坐标系中完整地推导出三维大气--土壤耦合模式的控制方程组及其参数化方案。模式详细考虑了坡度、坡向、周围地形遮蔽对辐射平衡的影响以及土壤水的冻结、融解、蒸发过程,结合 1985年冬太原地区边界层污染、气象观测资料进... 本文在地形坐标系中完整地推导出三维大气--土壤耦合模式的控制方程组及其参数化方案。模式详细考虑了坡度、坡向、周围地形遮蔽对辐射平衡的影响以及土壤水的冻结、融解、蒸发过程,结合 1985年冬太原地区边界层污染、气象观测资料进行对比模拟试验,取得了令人满意的结果。 展开更多
关键词 地形坐标系 大气-土壤耦合模式 数值模拟 土壤水
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我国大地坐标系的换代问题 被引量:68
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作者 魏子卿 《武汉大学学报(信息科学版)》 EI CSCD 北大核心 2003年第2期138-143,148,共7页
首先指出了我国现有大地坐标系在先进性和实用性方面存在的问题 ,提出了我们面临的选择与采用地心坐标系的建议 ,然后就地心坐标系的定义和实现、参考椭球常数、正常重力公式等问题提出了初步意见 ,并就坐标系改变对旧地形图的影响问题... 首先指出了我国现有大地坐标系在先进性和实用性方面存在的问题 ,提出了我们面临的选择与采用地心坐标系的建议 ,然后就地心坐标系的定义和实现、参考椭球常数、正常重力公式等问题提出了初步意见 ,并就坐标系改变对旧地形图的影响问题进行了研究。我国大地坐标系应由局部坐标系更新为地心坐标系。我国大地坐标系的定义应与IERS(国际地球自转服务)协议相一致 ,采用国际常用的参考椭球和正常重力公式。本文提出的参考椭球和正常重力公式符合这些原则 。 展开更多
关键词 大地坐标系 大地基准 参考椭球 正常重力公式 地形坐标系变化 地心坐标系
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中小地形对局地天气气候的影响 被引量:3
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作者 卢敬华 陈刚毅 《成都信息工程学院学报》 1989年第1期1-9,共9页
本文采用地形活动坐标系,研究在二维运动条件下地形对局地天气气候的影响。指出:地形对气流的影响不仅与地形高度z有关,而且与地形的坡度α,下垫面的热力分布,近地层大气稳定度г,垂直交换系数k以及基流v等诸因素密切相关。其中下垫面温... 本文采用地形活动坐标系,研究在二维运动条件下地形对局地天气气候的影响。指出:地形对气流的影响不仅与地形高度z有关,而且与地形的坡度α,下垫面的热力分布,近地层大气稳定度г,垂直交换系数k以及基流v等诸因素密切相关。其中下垫面温差,地形坡度和基流尤为重要。 展开更多
关键词 动力气象学 地形坐标系 气候影响
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Characteristics of pressure gradient force errors in a terrain-following coordinate 被引量:1
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作者 LI Jin-Xi LI Yi-Yuan WANG Bin 《Atmospheric and Oceanic Science Letters》 CSCD 2016年第3期211-218,共8页
A terrain-following coordinate (a-coordinate) in which the computational form of pressure gradient force (PGF) is two-term (the so-called classic method) has significant PGF errors near steep terrain. Using the ... A terrain-following coordinate (a-coordinate) in which the computational form of pressure gradient force (PGF) is two-term (the so-called classic method) has significant PGF errors near steep terrain. Using the covariant equations of the a-coordinate to create a one-term PGF (the covariant method) can reduce the PGF errors. This study investigates the factors inducing the PGF errors of these two methods, through geometric analysis and idealized experiments. The geometric analysis first demonstrates that the terrain slope and the vertical pressure gradient can induce the PGF errors of the classic method, and then generalize the effect of the terrain slope to the effect of the slope of each vertical layer (φ). More importantly, a new factor, the direction of PGF (a), is proposed by the geometric analysis, and the effects of φ and a are quantified by tan φ.tan a. When tan φ.tan a is greater than 1/9 or smaller than -10/9, the two terms of PGF of the classic method are of the same order but opposite in sign, and then the PGF errors of the classic method are large. Finally, the effects of three factors on inducing the PGF errors of the classic method are validated by a series of idealized experiments using various terrain types and pressure fields. The experimental results also demonstrate that the PGF errors of the covariant method are affected little by the three factors. 展开更多
关键词 Terrain-following coordinatepressure gradient forceerrors direction of pressuregradient slope of eachvertical layer nonlinearvertical pressure gradient pressure gradient alongvertical layer
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Characteristics of a Terrain-Following Sigma Coordinate 被引量:1
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作者 LI Yi-Yuan WANG Bin WANG Dong-Hai 《Atmospheric and Oceanic Science Letters》 2011年第3期157-161,共5页
This study quantifies the main characteristics of a terrain-following, G-coordinate through mathematical analyses of its covariant and contravariant basis vectors as well as the vertical coordinate of σ. A 3-D schema... This study quantifies the main characteristics of a terrain-following, G-coordinate through mathematical analyses of its covariant and contravariant basis vectors as well as the vertical coordinate of σ. A 3-D schematic of the σ-coordinate in a curvilinear coordinate system is provided in this study. The characteristics of the basis vectors were broken down into their "local vector charac- teristics" and "spatial distribution characteristics", and the exact expressions of the covariant; in addition, the con- travariant basis vectors of the G-coordinate used to eluci- date their detailed characteristics were properly solved. Through rewriting the expression of the vertical coordi- nate of G, a mathematical expression of all the cr-coor- dinate surfaces was found, thereby quantifying the so- called terrain-following characteristics and lack of flexi- bility to adjust the slope variation of G-coordinate sur- faces for the classic definition of G. Finally, an analysis on the range value of the vertical coordinate demonstrated that the general value range of G could be obtained by eliminating the G-coordinate surfaces below the Earth's surface. All these quantitative descriptions of the charac- teristics of G-coordinate were the foundation for improv- ing the G-coordinate or creating a new one. 展开更多
关键词 quantitative description sigma coordinate 3-D schematic basis vectors non-orthogonal
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Adaptive preprocessing algorithms of corneal topography in polar coordinate system 被引量:1
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作者 郭雁文 《Journal of Central South University》 SCIE EI CAS 2014年第12期4571-4576,共6页
New adaptive preprocessing algorithms based on the polar coordinate system were put forward to get high-precision corneal topography calculation results. Adaptive locating algorithms of concentric circle center were c... New adaptive preprocessing algorithms based on the polar coordinate system were put forward to get high-precision corneal topography calculation results. Adaptive locating algorithms of concentric circle center were created to accurately capture the circle center of original Placido-based image, expand the image into matrix centered around the circle center, and convert the matrix into the polar coordinate system with the circle center as pole. Adaptive image smoothing treatment was followed and the characteristics of useful circles were extracted via horizontal edge detection, based on useful circles presenting approximate horizontal lines while noise signals presenting vertical lines or different angles. Effective combination of different operators of morphology were designed to remedy data loss caused by noise disturbances, get complete image about circle edge detection to satisfy the requests of precise calculation on follow-up parameters. The experimental data show that the algorithms meet the requirements of practical detection with characteristics of less data loss, higher data accuracy and easier availability. 展开更多
关键词 corneal topography Placido disk polar coordinate self-adoption preprocessing algorithms
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