Lecture 3: Coordinate systems Flashcards

(53 cards)

1
Q

Geographic figure definition

A

Physical shape given by the terrain

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2
Q

Geoid definition

A
  1. An equipotential surface
  2. Approximates mean sea level
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3
Q

Reference ellipsoid definition

A
  1. A convenient computational surface
  2. Ellipsoid: latitude > longitude
  3. Flattening f = (latitude-longitude)/longitude
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4
Q

Coordinate system transformation process

A

Actual earth - 3D Earth Model (ellipsoid or sphere) - Plane Surface (projection) - Map (e.g cadastral, engineering plan, topo map, chart)

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5
Q

Two datum surfaces and one projection surface in surveying

A

Datum surfaces: Coordinate frame, Reference ellipsoid
Projection surface: Projection

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6
Q

The three primary map types

A
  1. Conic
  2. Azimuthal
  3. Mercator
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7
Q

What are map projections attempts at

A

Attempts to portray the surface of the earth on a flat surface

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8
Q

An implication to projections is that survey measurements (directions, distances) require

A

Observation corrections

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9
Q

Three primary observation corrections

A
  1. Line scale factor
  2. Arc to chord corrections
  3. Reduction to the ellipsoid
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10
Q

The mapping process creates distortion in

A
  1. Shapes and angles
  2. Distance
  3. Direction
  4. Scale
  5. Area
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11
Q

The larger the map, the greater the

A

Distortion

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12
Q

The four coordinate types

A
  1. 3D Cartesian coordinates
  2. 3D Geodetic coordinates
  3. 2D Grid coordinates
  4. 1D Geodetic coordinates
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13
Q

What parameters do 3D Cartesian Coordinates use

A

XYZ

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14
Q

What parameters do 3D Geodetic coordinates use

A

Latitude, longitude and height (ellipsoid parameters)

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15
Q

What parameters do 2D grid coordinates use

A

Northing and Easting (projection parameters)

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16
Q

What parameters do 1D geodetic coordinates use

A

Height and elevations (MSL, geoid ellipsoid seperation relationships)

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17
Q

3D geodetic coordinates require the definition of

A

An ellipsoid

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18
Q

Whats required to define an ellipsoid

A
  1. Semi-axis major (m)
  2. Inverse flattening (1/f)
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19
Q

3D cartesian coordinates assume earth is

A

Centred and fixed

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20
Q

Both cartesian and geodetic coordinates are geometrically

A

Consistent

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21
Q

When are 3D Cartesian coordinates commonly used

A
  1. GNSS positioning - satellite orbits, SPP (pseudorange positions), RTK (carrier-phase vectors)
  2. Remote imagery
  3. Lidar data sets
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22
Q

When are 3D Geodetic coordinates commonly used

A
  1. Navigation - sea and air
  2. Global and navigation survey networks
23
Q

Most common/relevant examples of 2D dimensional coordinates

A
  1. Transverse Mercator
  2. Lambert
  3. NZ map grid
24
Q

The projection parameters required in 2D Dimensional coordinates

A
  1. Latitude and longitude of origin
  2. False Easting and Northing
  3. Central meridian scale factor
25
When are 2D dimensional coordinates commonly used
1. Most field surveying 2. Topographical maps - e.g NZTM, Topo50 (1:50,000) 3. Bathymetric charts (also often used in geodetic coordinates) 4. Cadastral maps - e.g meridional circuits 5. Engineering projects - typically based on a local grid and can be plane grid if project is not too large
26
In 1D dimensional coordinates, the Ellipsoid/geodetic height is calculated how
Orthometric height (approx mean sea level) + Geoid and ellipsoid height difference
27
Coordinates are mathematically ____
Related to each other
27
By defining a coordinate frame, we can give the point ____ coordinates
Cartesian coordinates
28
By defining an ellipsoid, we can give the point ____ coordinates
Geodetic coordinates
29
By defining a projection, we can give the point ____ coordinates
Grid/Projection coordinates
30
From lines of latitude, parallels are
East/west lines which are parallel with the equator
31
From lines of longitude, parallels are
North/South lines that converge through the poles and are perpendicular to the equator
32
What is the origin for parallels
The pole of rotation
33
What is the origin for Meridians
The centre of the earth
34
Accessing and downloading geodetic mark data is available at
LINZ geodetic database
35
3D equals 2D plus 1D. True or false
False
36
A geodetic datum is
A customized reference and computational surface for 2D and/or 3D coordinates
37
The worlds geodetic datum
WGS84
38
New zealands terrestrial triangulation (2d) geodetic datum
NZGD1949
39
New zealands space based (3d) geodetic datum
NZGD2000
40
A vertical datum is
A customized reference surface for 1D coordinates
41
Dunedins vertical datum
DunedinVD1958 - classical mean sea level (MSL) based on levelling
42
New Zealands vertical datum
NZVD2016 - equipotential surface based on gravity
43
Global datum characteristics
1. Geocentric 2. Global network 3. Reference ellipsoid 4. Defined using space-based technology e.g GNSS
44
Local datum characteristics
1. Non-geocentric 2. Single origin station (usually) 3. Reference ellipsoid 4. Defined using triangulation methodology
45
Most common ellipsoids
1. International 1924 2. WGS72 3. WGS84 4. GRS80
46
The geoid is a representation of the surface of the earth that it would assume if
The sea covered the earth (i.e no topography
47
Geoids are thought of as a surface of equal
Gravitational potential and mean sea level, however sea level isnt flat and has topography
48
Geoids can be defined as
The shape a fluid earth would have if it had the gravity field of the earth
49
Geoids are roughly the mean sea level surface, excluding
Dynamic effects such as waves and tides
50
Geoid highs are gravity ____
Highs (and vice versa)
51
Vector/vertical gravity is perpendicular to
The geoid
52
Gravity will be deflected towards a dense body because
Fluid is attracted toward a denser body and therefore raises its surface