13大地水准面和参考椭球.docx

1、13大地水准面和参考椭球13大地水准面和参考椭球Unit 13 Geoid and Reference Ellipsoid（大地水准面和参考椭球）The Earths physical surface is a reality upon which the surveying observations are made and points are located.（地球物理表面【或者说，地球自然表面】是一个实体，测量工作【observation观测】在其上进行，点位在其上进行定位。）However, due to its variable topographic surface and ov

2、erall shape, it cannot be defined mathematically and so position cannot be computed on its surface.（然而，由于【due to】它的起伏不定的【variable可变的、不定的，这里按中文习惯译为起伏不定的】地形表面和总的【overall】形状，它不能被数学的定义，因此点位也不能在其上进行计算。）It is for this reason that in surveys of limited extent, the Earth is treated as flat and plane trigono

3、metry used to define position.（正是因为这个原因，在有限范围内的测量中，地球被当成平的，并用平面三角学【trigonometry三角学】来确定位置。）If the area under consideration is of limited extent, orthogonal projection of this area onto a plane surface may result in negligible distortion.（如果在考虑中的【under consideration在考虑中的】区域是有限范围的，该区域在一个平面【plane surfac

4、e】上的正交投影【orthogonal projection】导致的【直译为导致，可以意译为：其结果】是可以忽略的【negligible可以忽略的】变形【distortion】）Plane surveying techniques could be used to capture field data and plane trigonometry used to compute position.（平面测量技术可以被用来获取外业数据，平面三角学用来计算位置坐标）However, if the area extended to a large area beyond limitation and

5、 treated as a flat surface the effect of the Earths curvature will produce unacceptable distortion.（然而，如果该区域延伸【extend】为一个大的区域超过了限度，把它当成一个平面，地球的曲率影响【effect】将产生不可被接收的【unacceptable】变形）It can also be clearly seen that the use of a plane surface as a reference datum for the elevations of points is totall

6、y unacceptable.（同样可以明显的【clearly】看到，用平面作点的高程的参考基准是完全【totally完全地】不可被接受的【不可以的】。）Therefore, to represent horizontal positions and elevations on maps and charts, we need a mathematical model of the Earth which includes a set of numbers for the size and shape of the Earth.（因此，为了在地图和海图【chart海图、图表】上表示【repre

7、sent】出水平和高程位置，我们需要一个地球的数学模型，它包括一系列地球大小和形状的参数【number这里译为参数parameter参数】）We will define a mathematical surface that approximates to the shape of the area under consideration and then fit and orientate it to the Earths surface.（我们将定义一个数学表面接近【approximates接近v.】于被考虑的【under consideration】区域的形状，然后使之与地球表面相符合【

8、fit and orientate：fit是适合的意思；orientate是定向的意思】）Such a surface is referred in surveying as a reference ellipsoid.（这样一个表面在测量里被称为【refer提到、涉及】“参考椭球”）The Geoid （大地水准面）Since the physical surface of the Earth cant be used as a computational surface, a mean sea level surface is instinctively taken into consid

9、eration.（由于【既然】地球的自然表面不能被当作一个计算面来用，平均海平面自然的【instinctively本能地、自然地】被考虑【被考虑作计算面】）Mean sea level (MSL) is defined as the average level of the ocean surface for all it unsuitable mathematical location of planimetric position.（尽管重力位【gravity potential，potential位、电压、潜能】是处处相等的【指的是大地水准面的】，并且该曲面必地球自然表面药平滑的多，它依

10、然包含了许多不规则之处【irregularity】，使得【render】它不适于平面位置【planimetric position】的精确定位【mathematical除有数学的意思，也有精确的意思】These irregularities are thought to be due to mass anomalies throughout the Earth.（这种不规则被认为是由于【due to由于 due应当的】遍及地球【throughout介词：遍及】的质量【mass这里是质量的意思】分布不规则【anomaly异常、不规则】）The geoid remains important to

11、 the surveyor, as it is the surface to which all terrestrial measurements are related.（由于它是对于所有有关的陆地测量的参考面【surface这里译为参考面】，对测量者来说大地水准面依然【remain】重要）As the direction of the gravity vector (termed the vertical) is everywhere normal to the geoid, it defines the direction of the surveyors plumb-bob line.

12、（由于重力矢量（称之为【term称为】垂线【vertical垂线n.、垂直的adj.】）的方向在各处都垂直【normal垂直的、正交的、垂线、法线】于大地水准面，由测量者的铅垂线【plumb-bob line】方向就可以表示【define明确表示】）Thus any instrument which is horizontalized by means of a spirit bubble will be referenced to the local equipotential surface.（因而任何依赖【by means of依赖】水准气泡【spirit bubble】整平【horiz

13、ontalize】的仪器都参考的是局域等位面）Elevations are related to the equipotential surface passing through MSL.（高程就是关于通过平均海平面的等位面的数据）【或者翻译为：高程与过平均海平面的等位面有关or高程参考的是过平均海平面的等位面】Such elevations or heights are called orthometric heights (H) and are the linear distances measured along the gravity vector from a point to t

14、he equipotential surface as a reference datum.（这样的高程或高度被称为正高（H），沿着重力矢量从一个点到作为参考基准的等位面的直线【linear直线的】距离）As such, the geoid is the equipotential surface that best fits MSL and heights in question, referred to as heights above or below MSL.（同样地，大地水准面是最符合MSL的等位面；正被讨论的【in question正在讨论的、正在讨论】高度，指的是【refer t

15、o提到；as当作 合起来可以译为指的是】高于或低于MSL的高度）It can be seen from this that orthormetric heights are datum dependent.（由此可以看出，正高由其基准面决定【dependent由决定的、依靠的】）The Reference Ellipsoid（参考椭球）The ellipsoid is a mathematical surface which provides a convenient model of the size and shape of the Earth.（参考椭球是一个数学曲面，可以提供一个关于地

16、球的大小及形状的方便的【convenient】模型）It is represented by an ellipse rotated about its minor axis and is defined by its semi-major axis a or the flattening f.（由一个椭圆绕它的短轴【minor axis】旋转【rotate】表示，用它的长半轴a和扁率f来定义）The ellipsoid is chosen to best meet the needs of a particular geodetic datum system design.（这个椭球被选择来最

17、满足特定大地基准系统设计的需要【meet ones need满足的需要】）【即在设计一套特定的大地基准系统前首先选择一个满足系统设计的椭球】Although the ellipsoid is a concept and not a physical reality, it represents a smooth surface for which formulas can be developed to compute ellipsoidal distance, azimuth and ellipsoidal coordinates.（尽管参考椭球是一个概念，不是一个物理实体，它却表现出一个光

18、滑的表面，由此公式可以被发展来计算椭球距离，方位和椭球坐标。）Due to the variable shape of the geoid, it is not possible to have a global ellipsoid of reference for use by all countries.（由于【due to】大地水准面的起伏不定的形状，不可能有一个适用于所有国家的全球【global】参考椭球）The best-fitting global geocentric ellipsoid is the Geodetic Reference System 1980(GRS80),

19、which has the following dimensions: semi-major axis is 6378137.0 m and semi-minor axis is 6356752.314 m.（最适合的全球地心【geocentric地心的】椭球是1980大地坐标参考系统【80椭球，注意：我国使用的80坐标系使用的是75椭球】，尺寸【dimension尺寸、元】如下：长半轴为6378137.0 m，短半轴为6356752.314 m）The relationship of all three surfaces which are terrain, geoid and ellips

20、oid is illustrated in this Figure. （所有三个面：地表、大地水准面和椭球面的关系，由这个图图解说明【illustrate图例说明】）We note that the orthometric height H is the height with reference to the MSL, whereas the geodetic height h is the height of anything above the reference ellipsoid.（我们注意到，正高H是参考MSL的高度，而【whereas】大地高h是参考椭球面的高度）The rela

21、tion between the two kinds of heights is shown in the Figure, where the quantity N, the height of the geoid above the reference ellipsoid or the perpendicular distance between the geoid and the reference ellipsoid at a point, is usually called the geoidal height (geoid undulation).（这两种高度之间的关系如图所示，N这

22、个量【quantity】，某个点上大地水准面高于参考椭球面或者说大地水准面和参考椭球面之间的垂直距离【perpendicular distance垂直距离】，通常被称为大地水准面高【geoidal height】（大地水准面差距【geoid undulation；undulation波动】）Thus, the knowledge of the geoid is necessary for transforming the geodetic to orthometric heights and vice versa. （这样，把大地高转换为正高，大地水准面的知识就是必需的，反之亦然【vice v

23、ersa反之亦然】）Once we determine the geoid, we can compute the difference between the two surfaces, the ellipsoid and the geoid anywhere in the country.（一旦我们确定了大地水准面，我们就可以计算这两个面的差距国家的无论何处的椭球面和大地水准面）The expression “ellipsoidal height” for (geodetic) height of anything above the reference ellipsoid is also

24、 used comparing the acceptance of the standard geodetic term of “geoidal height”.（相对于标准的大地测量学术语“大地水准面高”的采用【acceptance接受、认同】，“椭球高”这个表示高于参考椭球面的高度（大地高）的表达【expression】也被采用。）Surveyors used to working with spirit levels have referenced orthometric heights (H) to the “average” surface of the earth, as depi

25、cted by MSL.（测量者习惯于参考【reference to】地球“平均”表面用MSL来描述【depicte】，利用水准测量，获得正高（H）The surface of MSL can be approximated by the geoid.（MSL这个面可以近似的当作大地水准面）The difference between the two surfaces arises from the fact that seawater is not homogeneous and because of a variety of dynamical effects on the seawate

26、r.（这两个面的差别出现在一个事实上海水不均匀并且有各种不断变化的影响在其上）The height of the MSL above the geoid is called the sea surface topography (SST).（MSL高于大地水准面的高度称为海面地形【sea surface topography】【还有一个SST satellite-to-satellite tracking卫星跟踪卫星技术；不要混了】）It is a very difficult quantity to obtain from any measurements; consequently, it

27、 is not yet known very accurately.（这是一个从任何测量工作中都非常难获取的值，因此【consequently】，它尚未【not yet尚未】非常准确的得知）GPS heights are referenced to the ellipsoid, a mathematical model that does not physically exist.（GPS高参考的是椭球面，是一个数学模型，并不物理地存在）This model, does not agree with mean sea level. That means the height of a poin

28、t determined from GPS is not the same as its sea level elevation as determined by leveling. （这个模型，不与平均海平面相吻合。这就意味着一个点由GPS确定的高度与由水准测量确定的海拔高不相同）The summarizing of the relationships among height systems can be illustrated below:（高程系统的关系概述举例说明【illustrate】如下【summarize概述n.】：）MSL elevation is roughly equiv

29、alent to orthometric height (H), the technical name for height above the geoid. The geoid is, for all intents and purposes, the same as MSL.（MSL 高程概略地等同于正高（H）高于大地水准面的高度的技术名词）Geoid height (N)is the separation between the geoid and the ellipsoid (sometimes called Geoidal separation). It can be plus or

30、 minus. A negative geoidal separation indicates that the geoid is below the ellipsoid.（大地水准面高（N）是大地水准面和椭球面之间的差距【separation】（有时也叫大地水准面差距）。它可以是正也可以是负。一个正的大地水准面差距表示【indicate】大地水准面在椭球面下方）Ellipsoid height (h)is the distance above or below the ellipsoid (plus or minus). Ellipsoid height is also called geodetic height.（椭球高（h）是高于或低于椭球的距离（正或负）。椭球高也叫做大地高。）