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January 7, 2021 Lecture Notes 1
COORDINATE SYSTEM
Introduction:
 Coordinates: Set of numbers representing the
position of points in space/map with respect to
a certain coordinate system.
 Coordinate system: A system whereby the
location/position of points are referred to.
January 7, 2021 Lecture Notes 2
Characteristics of coordinate system
 They have reference axes
 The reference axes meet at a point
known as origin
 The references axes are in a fixed
known orientation.
January 7, 2021 Lecture Notes 3
Coordinate system used in
Land surveying
 The coordinate system used in surveying
are;
 2D-Plane coordinate system
 3D-Spatial coordinate system
2D-Plane coordinate is divided into two types
namely;
 2D-cartesian coordinate system
 2D-polar coordinate system
January 7, 2021 Lecture Notes 4
2D-cartesian coordinate system
 A coordinate system where by a point is
referred to by two offsets from two mutually
perpendicular axes.
 In surveying, we have primary axis (X- axis)
that points towards the North and secondary
axis (Y-axis) that points towards the East.
January 7, 2021 Lecture Notes 5
2D-cartesian coordinate system cont….
2D-cartesian
Coord. system
Origin E (y)
N (x)
P (NP, EP)
∆NP
∆EP
The intersection of the X- and Y-axis forms the origin.
January 7, 2021 Lecture Notes 6
2D-cartesian coordinate system cont….
Also known as “Rectangular” coordinates
 Locates “XY” values on a flat plane
 Consist of four quadrants: I, II, III, IV
 Origin is at the center
 Distances measured “Horizontally” from the Origin
are “Easting” values
 Right of Origin are positive
 Left of Origin are negative
 Distances measured “Vertically” from the Origin
are “Northing” values
 Above Origin are positive
 Below Origin are negative
January 7, 2021 Lecture Notes 7
2D-cartesian coordinate system cont….
 Specifying “XY” values or “Coordinates
 Both values positive = Quadrant “I”
 Both values negative = Quadrant “III”
 “X”value negative,“Y” value positive = Quadrant “II”
 “X” value positive,“Y”value negative = Quadrant “IV”
January 7, 2021 Lecture Notes 8
2D-cartesian coordinate system cont….
Origin
Quadrant III Quadrant II
Quadrant IV Quadrant I
N (x)
E (y)
“X” positive, “Y” positive
“X” Negative, “Y” positive
“X” positive, “Y” Negative
“X” Negative, “Y” Negative
January 7, 2021 Lecture Notes 9
2D-polar coordinate system
 A system that involve the distance
SP from the origin to the point
concerned and the angle δ
between a fixed (or zero) direction
and the direction to the point.
 A point is referred to by a distance
and the angle from a known fixed
control point.
 The angle called azimuth or
bearing is measured in a
clockwise direction (i.e. from the
North direction
N P(SP, δP)
O
δ
δ is called Azimuth
or bearing.
SP
January 7, 2021 Lecture Notes 10
3D-Spatial coordinate system
 These are classified as;
 3D-Geographical coordinate system: A point is
referred to on the surface of the earth by its latitude,
longitude and height (Φ,λ, h)
 3D-cartesian coordinate system: A point is referred
to by its X, Y, Z coordinates measured with respect
to 3-mutually perpendicular axes with the origin at
the center of the earth.
 Astronomical coordinate system: A position of an
object in space is defined by its Right ascension
and declination, or by Hour angle and altitude.
January 7, 2021 Lecture Notes 11
3D-Geographical coordinate system
 The ellipsoidal height (h) of a point is the vertical
distance of the point above the ellipsoid. It is
measured in distance units along the ellipsoidal
normal from the point to the ellipsoid surface
 The latitude are measured with respect to the equator
at the center of the earth to observer parallel.
 Longitude are measured along the equatorial plane
from the Greenwich meridian to the observer's
meridian.
January 7, 2021 Lecture Notes 12
3D-Geographical coordinate system cont….
The latitude (Φ) and longitude (λ) angles and
the ellipsoidal height (h) represent the 3D geographic coordinate
January 7, 2021 Lecture Notes 13
3D-cartesian coordinate system
 The system has its origin at the mass-centre of the
Earth with the X- and Y-axes in the plane of the
equator.
 The X-axis passes through the meridian of Greenwich,
and the Z-axis coincides with the Earth's axis of
rotation.
 The three axes are mutually orthogonal and form a
right-handed system.
 All distances are measured from the origin.
January 7, 2021 Lecture Notes 14
3D-cartesian coordinate system cont….
Geocentric coordinates can be used to define a position
on the surface of the Earth (point P in figure above).
CIO: Conversion International of the Origin
January 7, 2021 Lecture Notes 15
Relationship between 2D-cartesian
and 2D-Polar coordinate systems
 Let consider the
plane below.
P (NP, EP)∆EP
∆NP
E
N
δP SP
∆NP = SP CosδP
∆EP = SP SinδP
SP = {∆NP
2 + ∆EP
2}
TanδP = ∆EP/∆NP
Taking the ratio from the two
equation above, we get
O )(tan 1






N
E

2D-Plane coordinate system
 Let consider the
plane below.
January 7, 2021 Lecture Notes 16
2D-cartesian and 2D-Polar
coordinate systems cont…
 The system used to define a direction is called the
whole circle bearing system (WCB). A bearing is
the direction measured clockwise from 00 full circle
to 3600.
 From the figure above, if is the forward bearing,
then the back bearing is given as;
Back bearing = forward bearing + 1800 or
= forward bearing – 1800
If FB is > 1800, then
Back bearing = Forward bearing – 1800
If the FB is < 1800, then
Back bearing = Forward bearing + 1800

Quadrants cont…








 
AB
AB
AB
N
E1
tan 







 
AB
AB
AB
E
N1
tan90








 
AB
AB
AB
N
E1
tan180
1st Quadrant 2nd Quadrant
4th Quadrant3rd Quadrant








 
AB
AB
AB
E
N1
tan270
January 7, 2021 Lecture Notes 18
Fundamental Calculations in Surveying
 There are two most fundamental calculations
in surveying namely;
 Join computations
 Polar computations
 When computing, the positive sign and
negative sign provided in quadrants should be
put into consideration for increasing the point.
January 7, 2021 Lecture Notes 19
Join computation method
 This involves computing the horizontal
distance (S) and bearing (δ) from the
difference in coordinates (∆E, ∆N) of a
line.
 Example
Given the point A(-275342.45,14758.02)
and B(322446.10,-92751.99). Calculate
distance and bearing of AB.
January 7, 2021 Lecture Notes 20
Join computation method cont…
Solution
 First calculate the increments
 The bearing is in the fourth quadrant, then
 
  EEE
  0
270











E
1
tan
January 7, 2021 Lecture Notes 21
Join computation method cont…
STN N E
A -275342.45 14758.02
B 322446.10 -92751.99
∆N,∆E 597788.55 -107510.01
25.607379S
''1648349 '0

 secSCheck
January 7, 2021 Lecture Notes 22
Polar computation method
 This involves calculating ∆E and ∆N
given the horizontal distance (S) and
Bearing (δ) of the line.
 Given :i) coordinate of a control point A &
ii) The bearing(δAP ) and
distance (SAP ) to the unknown point P )
 Required: coordinate of the unknown
point , P i.e (NP,EP).
 Consider the figure below
January 7, 2021 Lecture Notes 23
Polar computation method cont…
E(y)
N(x)
P (NP, EP)
A (NA, EA)
SAP
C ∆EP
∆NP
δAP
2D-Plane coordinate system
January 7, 2021 Lecture Notes 24
Polar computation method cont…
 Then, unknown point P can be calculate as
  cosSAC
  sinSEPC
  sinSEE
  cosSNN

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Coordinates system engineering

  • 1. January 7, 2021 Lecture Notes 1 COORDINATE SYSTEM Introduction:  Coordinates: Set of numbers representing the position of points in space/map with respect to a certain coordinate system.  Coordinate system: A system whereby the location/position of points are referred to.
  • 2. January 7, 2021 Lecture Notes 2 Characteristics of coordinate system  They have reference axes  The reference axes meet at a point known as origin  The references axes are in a fixed known orientation.
  • 3. January 7, 2021 Lecture Notes 3 Coordinate system used in Land surveying  The coordinate system used in surveying are;  2D-Plane coordinate system  3D-Spatial coordinate system 2D-Plane coordinate is divided into two types namely;  2D-cartesian coordinate system  2D-polar coordinate system
  • 4. January 7, 2021 Lecture Notes 4 2D-cartesian coordinate system  A coordinate system where by a point is referred to by two offsets from two mutually perpendicular axes.  In surveying, we have primary axis (X- axis) that points towards the North and secondary axis (Y-axis) that points towards the East.
  • 5. January 7, 2021 Lecture Notes 5 2D-cartesian coordinate system cont…. 2D-cartesian Coord. system Origin E (y) N (x) P (NP, EP) ∆NP ∆EP The intersection of the X- and Y-axis forms the origin.
  • 6. January 7, 2021 Lecture Notes 6 2D-cartesian coordinate system cont…. Also known as “Rectangular” coordinates  Locates “XY” values on a flat plane  Consist of four quadrants: I, II, III, IV  Origin is at the center  Distances measured “Horizontally” from the Origin are “Easting” values  Right of Origin are positive  Left of Origin are negative  Distances measured “Vertically” from the Origin are “Northing” values  Above Origin are positive  Below Origin are negative
  • 7. January 7, 2021 Lecture Notes 7 2D-cartesian coordinate system cont….  Specifying “XY” values or “Coordinates  Both values positive = Quadrant “I”  Both values negative = Quadrant “III”  “X”value negative,“Y” value positive = Quadrant “II”  “X” value positive,“Y”value negative = Quadrant “IV”
  • 8. January 7, 2021 Lecture Notes 8 2D-cartesian coordinate system cont…. Origin Quadrant III Quadrant II Quadrant IV Quadrant I N (x) E (y) “X” positive, “Y” positive “X” Negative, “Y” positive “X” positive, “Y” Negative “X” Negative, “Y” Negative
  • 9. January 7, 2021 Lecture Notes 9 2D-polar coordinate system  A system that involve the distance SP from the origin to the point concerned and the angle δ between a fixed (or zero) direction and the direction to the point.  A point is referred to by a distance and the angle from a known fixed control point.  The angle called azimuth or bearing is measured in a clockwise direction (i.e. from the North direction N P(SP, δP) O δ δ is called Azimuth or bearing. SP
  • 10. January 7, 2021 Lecture Notes 10 3D-Spatial coordinate system  These are classified as;  3D-Geographical coordinate system: A point is referred to on the surface of the earth by its latitude, longitude and height (Φ,λ, h)  3D-cartesian coordinate system: A point is referred to by its X, Y, Z coordinates measured with respect to 3-mutually perpendicular axes with the origin at the center of the earth.  Astronomical coordinate system: A position of an object in space is defined by its Right ascension and declination, or by Hour angle and altitude.
  • 11. January 7, 2021 Lecture Notes 11 3D-Geographical coordinate system  The ellipsoidal height (h) of a point is the vertical distance of the point above the ellipsoid. It is measured in distance units along the ellipsoidal normal from the point to the ellipsoid surface  The latitude are measured with respect to the equator at the center of the earth to observer parallel.  Longitude are measured along the equatorial plane from the Greenwich meridian to the observer's meridian.
  • 12. January 7, 2021 Lecture Notes 12 3D-Geographical coordinate system cont…. The latitude (Φ) and longitude (λ) angles and the ellipsoidal height (h) represent the 3D geographic coordinate
  • 13. January 7, 2021 Lecture Notes 13 3D-cartesian coordinate system  The system has its origin at the mass-centre of the Earth with the X- and Y-axes in the plane of the equator.  The X-axis passes through the meridian of Greenwich, and the Z-axis coincides with the Earth's axis of rotation.  The three axes are mutually orthogonal and form a right-handed system.  All distances are measured from the origin.
  • 14. January 7, 2021 Lecture Notes 14 3D-cartesian coordinate system cont…. Geocentric coordinates can be used to define a position on the surface of the Earth (point P in figure above). CIO: Conversion International of the Origin
  • 15. January 7, 2021 Lecture Notes 15 Relationship between 2D-cartesian and 2D-Polar coordinate systems  Let consider the plane below. P (NP, EP)∆EP ∆NP E N δP SP ∆NP = SP CosδP ∆EP = SP SinδP SP = {∆NP 2 + ∆EP 2} TanδP = ∆EP/∆NP Taking the ratio from the two equation above, we get O )(tan 1       N E  2D-Plane coordinate system  Let consider the plane below.
  • 16. January 7, 2021 Lecture Notes 16 2D-cartesian and 2D-Polar coordinate systems cont…  The system used to define a direction is called the whole circle bearing system (WCB). A bearing is the direction measured clockwise from 00 full circle to 3600.  From the figure above, if is the forward bearing, then the back bearing is given as; Back bearing = forward bearing + 1800 or = forward bearing – 1800 If FB is > 1800, then Back bearing = Forward bearing – 1800 If the FB is < 1800, then Back bearing = Forward bearing + 1800 
  • 17. Quadrants cont…           AB AB AB N E1 tan           AB AB AB E N1 tan90           AB AB AB N E1 tan180 1st Quadrant 2nd Quadrant 4th Quadrant3rd Quadrant           AB AB AB E N1 tan270
  • 18. January 7, 2021 Lecture Notes 18 Fundamental Calculations in Surveying  There are two most fundamental calculations in surveying namely;  Join computations  Polar computations  When computing, the positive sign and negative sign provided in quadrants should be put into consideration for increasing the point.
  • 19. January 7, 2021 Lecture Notes 19 Join computation method  This involves computing the horizontal distance (S) and bearing (δ) from the difference in coordinates (∆E, ∆N) of a line.  Example Given the point A(-275342.45,14758.02) and B(322446.10,-92751.99). Calculate distance and bearing of AB.
  • 20. January 7, 2021 Lecture Notes 20 Join computation method cont… Solution  First calculate the increments  The bearing is in the fourth quadrant, then     EEE   0 270            E 1 tan
  • 21. January 7, 2021 Lecture Notes 21 Join computation method cont… STN N E A -275342.45 14758.02 B 322446.10 -92751.99 ∆N,∆E 597788.55 -107510.01 25.607379S ''1648349 '0   secSCheck
  • 22. January 7, 2021 Lecture Notes 22 Polar computation method  This involves calculating ∆E and ∆N given the horizontal distance (S) and Bearing (δ) of the line.  Given :i) coordinate of a control point A & ii) The bearing(δAP ) and distance (SAP ) to the unknown point P )  Required: coordinate of the unknown point , P i.e (NP,EP).  Consider the figure below
  • 23. January 7, 2021 Lecture Notes 23 Polar computation method cont… E(y) N(x) P (NP, EP) A (NA, EA) SAP C ∆EP ∆NP δAP 2D-Plane coordinate system
  • 24. January 7, 2021 Lecture Notes 24 Polar computation method cont…  Then, unknown point P can be calculate as   cosSAC   sinSEPC   sinSEE   cosSNN