- •Introduction
- •Chapter 1 History of Geodesy
- •Chapter II Figure of the Earth Part 1
- •Figure of the Earth Part 2
- •Ellipsoid of Revolution
- •Chapter III Geodetic Surveying Techniques
- •Horizontal Positioning
- •Triangulation
- •Text 10
- •Orders of Triangulation
- •Text 11
- •Trilateration
- •Text 12
- •Traverse
- •Text 13
- •Celestial Techniques
- •Text 14
- •Vertical Positioning
- •Text 15
- •Chapter IV Geodetic Systems
- •Text 16
- •Orientation of Ellipsoid to Geoid
- •Text 17
- •Text 18
- •Text 19
- •Text 20
- •Text 21
- •Text 22
- •Text 23
- •Text 24
- •Text 25
- •Text 26
- •Chapter V Physical Geodesy
- •Text 27
- •Text 28
- •Text 29
- •Text 30
- •Text 31
- •Text 32
- •Text 33
- •Text 34
- •Text 35
- •Text 36
- •Chapter VI Satellite Geodesy
- •Text 37
- •Text 38
- •Text 39
- •Text 40
- •Text 41
- •Text 42
- •Chapter VII Other Developments in Geodesy
- •Text 43
- •Text 44
- •Text 45
- •Text 46
- •Text 47
- •Text 48
- •Text 49
- •Chapter VIII The World Geodetic System
- •Text 50
- •Text 51
- •Text 52
Text 18
Выражения:
differ from |
|
отличный от |
in addition |
|
кроме того |
result in |
|
выражаться в |
in view of |
|
учитывая |
regardless of |
|
независимо от |
than ever before |
|
чем когда-либо раньше |
satisfy requirements |
|
удовлетворять требованиям |
launch site |
|
пусковая площадка |
Discrepancies Between Datums
In areas of overlapping geodetic triangulation networks, each computed on a different datum, the coordinates of the points given with respect to one datum will differ from those given with respect to the other. The differences occur because of the different ellipsoids used and the probability that the centers of each datum's ellipsoid are oriented differently with respect to the earth's center. In addition, deflection errors in azimuth cause a relative rotation between the systems. Finally, a difference in the scale of horizontal control may result in a stretch in the corresponding lines of the geodetic nets.
In view of the different orientation of ellipsoid centers, the relative rotation between the systems, and the scale differences; the computation of geodetic information from one datum to another unconnected datum is quite impossible. Regardless of the accuracy of the individual datums for computation within themselves, there is no accurate way to perform distance and azimuth computations between unconnected geodetic systems.
With the development of both intermediate and long range defensive weapon systems, geodetic problems have become more critical than ever before. To satisfy military requirements, it is necessary to provide detailed cartographic coverage of areas of strategic importance and to accomplish geodetic computations between these areas and launch sites which are often on unrelated datums. Both of these requirements necessitate unification of major geodetic datums by one or a combination of existing methods.
Text 19
Выражения:
of a limited scope |
|
с ограниченным обзором |
be restricted to … |
|
ограничиваться ч-н |
to fit each other |
|
подгонять одно к другому |
Datum Connection
There are three general methods by which horizontal datums can be connected. The first method is restricted to surveys of a limited scope and consists of systematic elimination of discrepancies between adjoining or overlapping triangulation networks (Figure 18). This is done by moving the origin, rotating, and stretching networks to fit each other. The method is usually used to connect local surveys for mapping purposes. This method of datum transformation or datum reduction can only be used where control exists for common points in different systems.
In addition to the classic method of datum transformation described above, there is the gravimetric method of Physical Geodesy (Chapter V) and the methods of Satellite Geodesy (Chapter VI). These methods are used to relate large geodetic systems to each other and/or to a world system (Chapter VIII). Both the gravimetric and satellite methods produce necessary "connecting" parameters from reduction of their particular observational data.