Estimating Geometric Aspects of Relative Satellite Motion ...
Orbital Aspects of Satellite Communications
-
Upload
lee-robine -
Category
Documents
-
view
613 -
download
2
Transcript of Orbital Aspects of Satellite Communications
GMU - TCOM 507 - Spring 2001 Class: Jan-25-2001
(C) Leila Z. Ribeiro, 2001 1
1
ORBITAL MECHANICS
A Compilation by: M.LENIN BABU,M.Tech.,
Lecturer,Dept. of ECE, Bapatla Engineering College
2
Topics covered according to
syllabus
• Kepler’s laws of motion
• Locating the satellite in the orbit
• Locating the satellite w.r.t earth.
• Orbital elements
• Look angle determination
GMU - TCOM 507 - Spring 2001 Class: Jan-25-2001
(C) Leila Z. Ribeiro, 2001 2
3
Kinematics & Newton’s Law
• s = ut + (1/2)at2
• v2 = u2 + 2at
• v = u + at
• F = ma
s = Distance traveled in time, t
u = Initial Velocity at t = 0
v = Final Velocity at time = t
a = Acceleration
F = Force acting on the object
Newton’s
Second Law
4
FORCE ON A SATELLITE : 1
• Force = Mass Acceleration
• Unit of Force is a Newton
• A Newton is the force required to accelerate 1 kg by 1 m/s2
• Underlying units of a Newton are therefore (kg) (m/s2)
• In Imperial Units 1 Newton = 0.2248 ft lb.
GMU - TCOM 507 - Spring 2001 Class: Jan-25-2001
(C) Leila Z. Ribeiro, 2001 3
5
ACCELERATION FORMULA • a = acceleration due to gravity = / r2 km/s2
• r = radius from center of earth
• = universal gravitational constant G multiplied by the mass of the earth ME
• is Kepler’s constant and = 3.9861352 105 km3/s2
• G = 6.672 10-11 Nm2/kg2 or 6.672 10-20 km3/kg s2 in the older units
6
FORCE ON A SATELLITE : 2
Inward (i.e. centripetal force)
Since Force = Mass Acceleration
If the Force inwards due to gravity = FIN
then
FIN = m ( / r2)
= m (GME / r2)
GMU - TCOM 507 - Spring 2001 Class: Jan-25-2001
(C) Leila Z. Ribeiro, 2001 4
7
Reference Coordinate Axes 1:
Earth Centric Coordinate
System
Fig. 2.2 in text
The earth is at the
center of the coordinate
system
Reference planes
coincide with the
equator and the polar
axis
8
Reference Coordinate Axes
2: Satellite Coordinate
System
Fig. 2.3 in text
The earth is at the
center of the
coordinate system and
reference is the plane
of the satellite’s orbit
GMU - TCOM 507 - Spring 2001 Class: Jan-25-2001
(C) Leila Z. Ribeiro, 2001 5
9
Balancing the Forces - 2
Inward Force
r
mGME
F 3
r
Equation (2.7)
F
G = Gravitational constant = 6.672 10-11 Nm2/kg2
ME = Mass of the earth (and GME = = Kepler’s
constant)
m = mass of satellite
r = satellite orbit radius from center of earth
r= unit vector in the r direction (positive r is away from earth)
10
Balancing the Forces - 3
Outward Force F
2
2
dt
dmF
r
Equation (2.8)
Equating inward and outward forces we find
2
2
3 dt
d
r
rr
Equation (2.9), or we can write
032
2
rdt
d rr Equation (2.10)
Second order differential
equation with six unknowns:
the orbital elements
GMU - TCOM 507 - Spring 2001 Class: Jan-25-2001
(C) Leila Z. Ribeiro, 2001 6
11
• We have a second order differential
equation
• See text p.21 for a way to find a solution
• If we re-define our co-ordinate system into
polar coordinates (see Fig. 2.4) we can re-
write equation (2.11) as two second order
differential equations in terms of r0 and 0
THE ORBIT - 1
12
THE ORBIT - 2
• Solving the two differential equations leads to six constants (the orbital constants) which define the orbit, and three laws of orbits (Kepler’s Laws of Planetary Motion)
• Johaness Kepler (1571 - 1630) a German Astronomer and Scientist
GMU - TCOM 507 - Spring 2001 Class: Jan-25-2001
(C) Leila Z. Ribeiro, 2001 7
13
KEPLER’S THREE LAWS
• Orbit is an ellipse with the larger body (earth) at one focus
• The satellite sweeps out equal arcs (area) in equal time (NOTE: for an ellipse, this means that the orbital velocity varies around the orbit)
• The square of the period of revolution equals a CONSTANT the THIRD POWER of SEMI-MAJOR AXIS of the ellipse
14
Review: Ellipse analysis
• Points (-c,0) and (c,0) are the foci.
•Points (-a,0) and (a,0) are the vertices.
• Line between vertices is the major axis.
• a is the length of the semimajor axis.
• Line between (0,b) and (0,-b) is the minor
axis.
• b is the length of the semiminor axis.
12
2
2
2
b
y
a
x
222 cba
Standard Equation:
y
V(-a,0)
P(x,y)
F(c,0) F(-c,0) V(a,0)
(0,b)
x
(0,-b)
abA
Area of ellipse:
GMU - TCOM 507 - Spring 2001 Class: Jan-25-2001
(C) Leila Z. Ribeiro, 2001 8
15
KEPLER 1: Elliptical Orbits
Figure 2.6 in text
Law 1
The orbit is an
ellipse
e = ellipse’s eccentricity
O = center of the earth
(one focus of the ellipse)
C = center of the ellipse
a = (Apogee + Perigee)/2
16
KEPLER 1: Elliptical Orbits (cont.)
Equation 2.17 in text:
(describes a conic section,
which is an ellipse if e < 1)
)cos(*1 0
0e
pr
e = eccentricity
e<1 ellipse
e = 0 circle
r0 = distance of a point in the
orbit to the center of the earth
p = geometrical constant (width
of the conic section at the focus)
p=a(1-e2)
0 = angle between r0 and the
perigee
p
GMU - TCOM 507 - Spring 2001 Class: Jan-25-2001
(C) Leila Z. Ribeiro, 2001 9
17
KEPLER 2: Equal Arc-Sweeps
Figure 2.5
Law 2
If t2 - t1 = t4 - t3
then A12 = A34
Velocity of satellite is
SLOWEST at APOGEE;
FASTEST at PERIGEE
18
KEPLER 3: Orbital Period
Orbital period and the Ellipse are related by
T2 = (4 2 a3) / (Equation 2.21)
That is the square of the period of revolution is equal to a
constant the cube of the semi-major axis.
IMPORTANT: Period of revolution is referenced to inertial space, i.e.,
to the galactic background, NOT to an observer on the surface of one
of the bodies (earth).
= Kepler’s Constant = GME
GMU - TCOM 507 - Spring 2001 Class: Jan-25-2001
(C) Leila Z. Ribeiro, 2001 10
19
Numerical Example 1
The Geostationary Orbit: Sidereal Day = 23 hrs 56 min 4.1 sec
Calculate radius and height of GEO orbit:
20
LOCATING THE SATELLITE
IN ORBIT: 1
Start with Fig. 2.6 in Text o is the True
Anomaly
See eq. (2.22)
C is the
center of
the orbit
ellipse
O is the
center of
the earth NOTE: Perigee and Apogee are on opposite sides of the orbit
GMU - TCOM 507 - Spring 2001 Class: Jan-25-2001
(C) Leila Z. Ribeiro, 2001 11
21
LOCATING THE SATELLITE
IN ORBIT: 2 • Need to develop a procedure that will allow
the average angular velocity to be used
• If the orbit is not circular, the procedure is to
use a Circumscribed Circle • A circumscribed circle is a circle that has a
radius equal to the semi-major axis length of
the ellipse and also has the same center
22
LOCATING THE SATELLITE
IN ORBIT: 3 Fig. 2.7 in the text
= Average angular velocity
E = Eccentric Anomaly
M = Mean Anomaly
M = arc length (in radians) that
the satellite would have traversed
since perigee passage if it were
moving around the
circumscribed circle with a mean
angular velocity
GMU - TCOM 507 - Spring 2001 Class: Jan-25-2001
(C) Leila Z. Ribeiro, 2001 12
23
ORBIT CHARACTERISTICS
Semi-Axis Lengths of the Orbit
21 e
pa
where
2hp
and h is the magnitude
of the angular
momentum
See eq. (2.18)
and (2.16)
2/121 eab where
Che
2
See eqn.
(2.19)
and e is the eccentricity of the
orbit
24
ORBIT ECCENTRICITY
• If a = semi-major axis,
b = semi-minor axis, and
e = eccentricity of the orbit ellipse,
then
ba
bae
NOTE: For a circular orbit, a = b and e = 0
GMU - TCOM 507 - Spring 2001 Class: Jan-25-2001
(C) Leila Z. Ribeiro, 2001 13
25
It is related to the radius ro by
ro = a(1-ecosE)
Thus
a - ro = aecosE
We can develop an expression that relates eccentric anomaly E to the average angular velocity η, which yields
η dt = (1-ecosE) dE
Let tp be the time of perigee. This is simultaneously the time of closest approach to the earth; the time when the satellite is crossing the xo axis; and the time when E is zero. Integrating both sides of the equation we obtain
η (t – tp) = E – e sin E
The left side of the equation is called the mean anomaly, M. Thus
M =η (t – tp) = E – e sin E
26
Time reference:
• tp Time of Perigee = Time of closest approach to the earth, at the same time, time the satellite is crossing the x0 axis, according to the reference used.
• t- tp = time elapsed since satellite last passed the perigee.
GMU - TCOM 507 - Spring 2001 Class: Jan-25-2001
(C) Leila Z. Ribeiro, 2001 14
27
ORBIT DETERMINATION 1:
Procedure: Given the time of perigee tp, the eccentricity e
and the length of the semimajor axis a:
• Average Angular Velocity (eqn. 2.25)
• M Mean Anomaly (eqn. 2.30)
• E Eccentric Anomaly (from eqn. 2.30)
• ro Radius from orbit center (eqn. 2.27)
• o True Anomaly ( eq. 2.22)
• x0 and y0 (using eqn. 2.23 and 2.24)
28
ORBIT DETERMINATION 2:
• Orbital Constants allow you to determine coordinates (ro, o) and (xo, yo) in the orbital plane
• Now need to locate the orbital plane with respect to the earth
• More specifically: need to locate the orbital location with respect to a point on the surface of the earth
GMU - TCOM 507 - Spring 2001 Class: Jan-25-2001
(C) Leila Z. Ribeiro, 2001 15
29
LOCATING THE SATELLITE
WITH RESPECT TO THE EARTH
• The orbital constants define the orbit of the
satellite with respect to the CENTER of the earth
• To know where to look for the satellite in space,
we must relate the orbital plane and time of
perigee to the earth’s axis
NOTE: Need a Time Reference to locate the satellite. The
time reference most often used is the Time of Perigee, tp
30
GEOCENTRIC EQUATORIAL
COORDINATES - 1
• zi axis Earth’s rotational axis (N-S poles
with N as positive z)
• xi axis In equatorial plane towards FIRST
POINT OF ARIES
• yi axis Orthogonal to zi and xi
NOTE: The First Point of Aries is a line from the
center of the earth through the center of the sun at
the vernal equinox (spring) in the northern
hemisphere
GMU - TCOM 507 - Spring 2001 Class: Jan-25-2001
(C) Leila Z. Ribeiro, 2001 16
31
GEOCENTRIC EQUATORIAL
COORDINATES - 2
Fig. 2.8 in text
To First Point of Aries
RA = Right Ascension
(in the xi,yi plane)
= Declination (the
angle from the xi,yi plane
to the satellite radius)
NOTE: Direction to First Point of Aries does NOT rotate
with earth’s motion around; the direction only translates
32
LOCATING THE SATELLITE - 1
• Find the Ascending Node
–Point where the satellite crosses
the equatorial plane from South to
North
–Define and i
–Define
Inclination
Right Ascension of the Ascending
Node (= RA from Fig. 2.6 in text)
See next slide
GMU - TCOM 507 - Spring 2001 Class: Jan-25-2001
(C) Leila Z. Ribeiro, 2001 17
33
DEFINING PARAMETERS
Orbit passes through
equatorial plane here
First Point
of Aries
Fig. 2.9 in text
Center of earth
Argument of Perigee
Right Ascension Inclination
of orbit
Equatorial plane
34
DEFINING PARAMETERS 2
GMU - TCOM 507 - Spring 2001 Class: Jan-25-2001
(C) Leila Z. Ribeiro, 2001 18
35
36
LOCATING THE SATELLITE - 2
• and i together locate the Orbital
plane with respect to the
Equatorial plane.
• locates the Orbital coordinate
system with respect to the
Equatorial coordinate system.
GMU - TCOM 507 - Spring 2001 Class: Jan-25-2001
(C) Leila Z. Ribeiro, 2001 19
37
LOCATING THE SATELLITE - 2
• Astronomers use Julian Days or Julian Dates
• Space Operations are in Universal Time
Constant (UTC) taken from Greenwich Meridian
(This time is sometimes referred to as “Zulu”)
• To find exact position of an orbiting satellite at a
given instant, we need the Orbital Elements
38
ORBITAL ELEMENTS (P. 29)
• Right Ascension of the Ascending Node
• i Inclination of the orbit
• Argument of Perigee (See Figures 2.6 &
2.7 in the text)
• tp Time of Perigee
• e Eccentricity of the elliptical orbit
• a Semi-major axis of the orbit ellipse (See
Fig. 2.4 in the text)
GMU - TCOM 507 - Spring 2001 Class: Jan-25-2001
(C) Leila Z. Ribeiro, 2001 20
39
Numerical Example 2: Given a Space Shuttle Circular orbit (height = h = 250
km). Use earth radius = 6378 km. Determine:
a. Period = ?
b. Linear velocity = ?
40
Numerical Example 3: Elliptical Orbit: Perigee = 1,000 km, Apogee = 4,000 km
a. Period = ?
b. Eccentricity = ?