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Satellite Orbits & Trajectories
Chapter-2
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Satellites orbits
Satellite Orbits
GEO
LEO
MEO
HEO
HAPs
LEO 500 -1000 km
GEO 36,000 km
MEO
5,000 15,000 km
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Geostationary Earth Orbit (GEO)
These satellites are in orbit 35,863 km
Objects in Geostationary orbit revolve aroundthe earth at the same speed as the earth
rotates. This means GEO satellites remain in the same
position relative to the surface of earth.
now over 200 active commercialcommunications satellites in geostationaryorbit.
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Low Earth Orbit (LEO)
LEO satellites are much closer to the earth
than GEO satellites, ranging from 500 to 1,500
km above the surface.
LEO satellites dont stay in fixed positionrelative to the surface, and are only visible for
15 to 20 minutes each pass.
A network of LEO satellites is necessary for
LEO satellites to be useful
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LEO (cont.)
Disadvantages
A network of LEO satellites is needed, which can
be costly
LEO satellites have to compensate for Doppler
shifts cause by their relative movement.
Atmospheric drag effects LEO satellites, causing
gradual orbital deterioration.
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Medium Earth Orbit (MEO)
A MEO satellite is in orbit 8,000 km -18,000
km
MEO satellites are visible for much longerperiods of time than LEO satellites, usually
between 2 to 8 hours.
MEO satellites have a larger coverage area
than LEO satellites.
A.k.a. Intermediate Circular Orbits (ICO),
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Highly Elliptical Orbit (HEO)
Known as Molniya Orbit Satellites
Used by Russia for decades.
Molniya Orbit is an elliptical orbit. The satellite
remains in a nearly fixed position relative to earth
for eight hours.
A series of three Molniya satellites can act like a
GEO satellite. Useful in near polar regions.
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Other Orbits (cont.)
High Altitude Platform (HAP)
One of the newest ideas in satellitecommunication.
A blimp or plane around 20 km above the earthssurface is used as a satellite.
HAPs would have very small coverage area, butwould have a comparatively strong signal.
Cheaper to put in position, but would require a lotof them in a network.
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Orbiting Satellites: Basic Principles
The motion of natural and artificial satellitesaround earth is governed by two forces-
One of them is Centripetal force directed
towards the center of the Earth due togravitational force of Earth.
Other is Centrifugal force is the force exerted
during circular motion, by the moving objectupon the other object around which it is
moving.
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Here Satellite is
exertingcentrifugal force.
The force that is
causing circular
motions is
centripetal force.
These two forces
are explained
from Newtons
Law of motionand Gravitation.
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Newtons Laws of Motion
1st Law An object at rest will stay atrest, and an object in motion will stay inmotion at constant velocity, unless actedupon by an unbalanced force.
2nd Law Force equals mass timesacceleration.
3rd Law For every action there is anequal and opposite reaction.
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Newton's Law of Gravity
In the Principia, Newton defined the force ofgravity in the following way (translated from
the Latin):
Every particle of matter in the universe attractsevery other particle with a force that is directly
proportional to the product of the masses of the
particles and inversely proportional to the
square of the distance between them.
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Fg = The force of gravity (typically in newtons)
G = The gravitational constant, which adds the proper level of
proportionality to the equation. The value ofG is 6.67259 x 10-11 N * m2 / kg2, although the value will change if other units
are being used.
m1 & m1 = The masses of the two particles (typically in
kilograms) r= The straight-line distance between the two particles
(typically in meters)
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Newtonss 1st Law and You
Dont let this be you. Wear seat belts.
Because of inertia, objects (including you) resist changesin their motion. When the car going 80 km/hour is stopped
by the brick wall, your body keeps moving at 80 m/hour.
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Newtons 2nd Law
The net force of an object is
equal to the product of its mass
and acceleration, or F=ma.
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3rd Law
There are two forces
resulting from this
interaction - a force on
the chair and a force on
your body. These two
forces are called action
and reaction forces.
For every action,there is an equaland oppositereaction.
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German astronomer (1571 1630)
Spent most of his career tediouslyanalyzing huge amounts of observational
data (most compiled by Tycho Brahe) on
planetary motion (orbit periods, orbit radii, etc.)
Used his analysis to develop Laws ofplanetary motion.
Laws in the sense that they agree
with observation, but not true
theoretical laws, such as Newtons
Laws of Motion & Newtons Universal
Law of Gravitation.
Johannes Kepler
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Keplers Laws are consistent with & are obtainable fromNewtons Laws
Keplers First Law All planets move in elliptical orbits with the Sun at one
focus
Keplers Second Law The radius vector drawn from the Sun to a planet
sweeps out equal areas in equal time intervals Keplers Third Law
The square of the orbital period of any planet isproportional to the cube of the semimajor axis of theelliptical orbit
Keplers Laws
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The points F1 & F2 are each a focusof the ellipse
Located a distance c from the center Sum ofr1and r2 is constant
Longest distance through center isthe major axis, 2a
a is called the semimajor axis
Shortest distance through center isthe minor axis, 2b
b is called the semiminor axis
Math Review: Ellipses
Typical Ellipse
Theeccentricity is defined as e = (c/a) For a circle, e = 0
The range of values of the eccentricity for ellipses is 0 < e < 1
The higher the value ofe, the longer and thinner the ellipse
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The Sun is at one focus Nothing is located at the other focus
Aphelionis the point farthest away from the Sun The distance for aphelion is a + c
For an orbit around the Earth, this point is called theapogee
Perihelionis the point nearest the Sun The distance for perihelion is a c
For an orbit around the Earth, this point is called theperigee
Ellipses & Planet Orbits
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All planets move in elliptical orbits
with the Sun at one focus
A circular orbit is a special case of an elliptical orbit
The eccentricity of a circle is e = 0.
Keplers 1st Lawcan be shown (& was by Newton) to be a direct resultof the inverse square nature of the gravitational force. Comes out ofNs 2ndLaw + Ns Gravitation Law + Calculus
Elliptic (and circular) orbits are allowed for bound objects A bound object repeatedly orbits the center
An unbound object would pass by and not return These objects could have paths that are parabolas
(e = 1) and hyperbolas (e > 1)
Keplers 1st Law
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Orbital Parameters
The satellite orbit which in general is elliptical, is
characterized by a number of parameters. The following
are orbital elements and parameters.
Ascending and Descending Node
Equinoxes
Solstices
Apogee
Perigee
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Eccentricity Semi-Major Axis
Right Ascension of Ascending Node
Inclination Argument of the Perigee
True Anomaly of Satellite
Angles Defining Direction of Satellite
Orbital Parameters
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Ascending and Descending Nodes
The satellite orbit cutsthe equatorial plane at two points,
the first called the descending
node (n1), where satellite passes
From northern hemisphere to theSouthern hemisphere, and second
Called ascending node (n2), where
Satellite passes from southern to northern
Hemisphere.
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Equinox
An equinox occurs twice a year (around 20 March and 22 September), when the tilt of
the Earth's axis is inclined neither away from nor towards the Sun, the center of theSun being in the same plane as the Earth's equator. The term equinoxcan also be usedin a broader sense, meaning the date when such a passage happens. The name"equinox" is derived from the Latin aequus (equal) and nox(night), because aroundthe equinox, night and day are about equal length.
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Solstices
Solstices are the
times when theinclination angle is
at its maximum
(i.e 23.4 deg).
These also occurtwice a year on 21
June, called the
summer solstice
and21 December
called the wintersolstice.
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Apogee
Apogee is a pointon the satelliteorbit that is at thefarthest distancefrom the center ofthe Earth. The
apogee distance Acan be computedfrom the knownvalues of orbiteccentricity e and
the semi-majoraxis a as A=a(1+e)
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Perigee
Perigee is the
point on theorbit that is
nearest to the
centre of the
earth . The
perigee
distance P can
be computedby
P=a(1-e)
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The orbit eccentricity e is ratio of the distance between
the center of the ellipse and the center of the Earth tosemi-major axis of the ellipse. It can be computed by
e=
+
e=
2
e=
Where a and b are semi-major and semi-minor axes,
respectively.
Eccentricity
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Right Ascension of Ascending Node
The Right Ascension of the Ascending Node
(aW
) indicates the geocentric Right Ascension
(R.A. or a) of a satellite as it intersects the
Earth's equatorial plane traveling northward
(ascending). Its value can range anywhere
from 0 to 360 degrees.
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Inclination
A satellite orbit's Inclination (i) indicates the angle of the
satellite orbit plane measured from the Earth's equatorialplane. Inclination can range anywhere from 0 to 180 degrees.An orbit inclination of 0 to 90 degrees is called a progradeorbit. An orbit inclination of 90 to 180 degrees is called aretrograde orbit.
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Argument of the Perigee
The Argument of Perigee
(w) is defined as the anglewithin the satellite orbitplane that is measuredfrom the Ascending Node
(W) to the perigee point(p) along the satellite'sdirection of travel.
The value of the Argumentof Perigee can beanywhere from 0 to 360degrees.
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True Anomaly of Satellite
This parameter is used
to indicate the positionof the satellite in its
orbit. This is done by
defining the angle ,
called the true anomalyof the satellite, formed
by the line joining the
perigee and center of
the earth with the line
joining the satellite and
the center of the earth.
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Angles defining Direction of Satellite
The direction of the
satellite is defined bytwo angles, the first by
angle y between the
direction of the
satellite velocity vectorand its projection in
the local horizontal and
second by Angle Az,
between the north and
the projection of the
satellites velocity
vector on the local
horizontal.
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