J. Peraire
16.07 Dynamics
Fall 2004
Version 1.1
Lecture D11 - Relative Motion using Translating Axes
In the previous lectures we have described particle motion as it would be seen by an observer standing still
at a fixed origin. This type of motion is called absolute motion. In many situations of practical interest,
we find ourselves forced to describe the motion of bodies while we are simultaneously moving with respect
to a more basic reference. There are many examples were such situations occur. The absolute motion of
a passenger inside an aircraft is best described if we first consider the motion of the passenger relative to
the aircraft, and then the motion of the aircraft relative to the ground. If we try to track the motion of
aircraft in the airspace using satellites, it makes sense to first consider the motion of the aircraft relative to
the satellite and then combine this motion with the motion of the satellite relative to the earth’s surface. In
this lecture we will introduce the ideas of relative motion analysis.
Types of observers
For the purpose of studying relative motion, we will consider three different types of observers (or reference
frames) depending on their motion with respect to a fixed frame:
? observers who do not accelerate or rotate, i.e. those who at most have constant velocity.
? observers who accelerate but do not rotate
? observers who accelerate and rotate
In this lecture we will consider the relative motion involving observers of the first two types, and defer for
the next lecture the study of relative motion involving rotating frames.
Relative motion using translating axes
Consider two particles, A and B, which may have different curvilinear motions. We consider a fixed reference
frame xyz with origin O and with unit vectors i, j and k, as before, and call the motion relative to this
frame absolute. In addition, we consider another translating reference frame attached to particle B, x′y′z′,
with unit vectors i′, j′ and k′. Translating means that the angles between the axes xyz and x′y′z′ do not
change during the motion.
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In the figure, we have chosen, for convenience, the axes xyz to be parallel to the axes x′y′z′, but it should
be clear that one could have non-parallel translating axes.
The position vector rA/B defines the position of A with respect to point B in the reference frame x’y’z’.
The subscript notation“A/B” means “A relative to B”. The positions of A and B relative to the absolute
frame are given by the vectors rA and rB, respectively. Thus, we have
rA = rB +rA/B .
If we derive this expression with respect to time, we obtain
˙rA = ˙rB + ˙rA/B or vA = vB +vA/B ,
which relates the absolute velocities vA and vB to the relative velocity of A as observed by B. Differentiating
again, we obtain an analogous expression for the accelerations,
¨rA = ¨rB + ¨rA/B or aA = aB +aA/B .
If we reverse the roles of A and B and attach the reference frame x′y′z′ to A, then we can observe B from
A.
The same arguments as before will give us,
rB = rA +rB/A, vB = vA +vB/A, aB = aA +aB/A .
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Comparing these expressions with those above, we see that
rB/A = ?rA/B, vB/A = ?vA/B, aB/A = ?aA/B ,
as expected.
One important observation is that, whenever the moving system, say A, has a constant velocity relative
to the fixed system, O, then the acceleration seen by the two observers is the same, i.e., if aA = 0, then
aB = aB/A. We shall see that this broadens the application of Newton’s second law to systems which have
a constant absolute velocity.
Example Glider in cross wind
Consider a glider flying at the edge of a cloud. The glider is flying horizontally, and the cloud, which is
below the glider, is stationary with respect to the ground. At the altitude of the glider flight, there is a wind
velocity, vw, of magnitude 52 knots, as shown in the sketch.
NorthEdge of Cloud
Cloud
The glider, on the other hand, is flying at a speed vG/w relative to the local wind. In order to determine the
speed of the glider with respect to the ground, we consider a reference frame moving with the wind speed
and write
vG = vw +wG/w,
or graphically,
By looking at the scaled diagram below, we can verify the following situations. If the glider flies with a
heading of 330o and a speed (relative to the wind) of 90 knots, it will stay at the edge of the cloud with a
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ground speed of 104 = (26 + 78) knots north. If, on the other hand, the glider flies with a heading of 210o
at 90 knots, the glider will stay at the edge of the cloud with a ground speed of 52 knots south. If the glider
flies into the wind at 240o, with a speed equal to 52 knots, it will remain stationary with respect to the
ground. Finally, the lowest speed at which the glider can fly to stay at the edge of the cloud is 45 knots and
this will be possible for a heading of 270o. The ground speed in this case will be 24 knots.
Example Aircraft towing glider (Merriam)
Airplane A is flying horizontally with a constant speed of 200km/h, and is towing a glider B. The glider is
gaining altitude. The tow cable has a length r = 60m, and θ is increasing at a constant rate of 5 degrees per
second. We want to determine the magnitude of the velocity, vG, and the acceleration, aG, of the glider for
the instant when θ = 15o.
The velocity of the glider will be vG = vA +vG/A. The velocity of the glider relative to A is best expressed
using a polar coordinate system. Thus, we write,
vG/A = ˙rer + r ˙θeθ .
Since the length of the cable is constant, vr = ˙r = 0, and ˙θ = 5(2pi/360) = 0.0874 rad/sec, which gives
vθ = r ˙θ = 5.236 m/s. We can now transform the velocity vector to cartesian coordinates to obtain,
vG/A = 5.236eθ = 5.236sin15oi+ 5.236cos15oj = 1.3552i+ 5.0575j m/s ,
or,
vG = ((200/3.6)+ 1.3552)i+ 5.0575j m/s, vG = 57.135 m/s = 205.7 km/h .
For the acceleration aG = aG/A, since aA = 0. We also know that ¨θ = 0, and, obviously, ¨r = 0, thus,
aG/A = ?r˙θ2er = ?4.57er m/s2, aG/S = 4.57 m/s2 .
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Example Aircraft collision avoidance
Consider two aircrafts, A and B, flying horizontally at the same level with constant velocities vA and vB.
Aircraft B is capable of determining by measurement the relative position and velocity of A relative to B,
i.e., rA/B and vA/B. We want to know whether it is possible to determine from this measurement whether
the two aircraft are on a collision course.
Take the origin O at the hypothetical point of collision where the two trajectories intersect. If collision is to
occur, the time taken for both aircraft to reach O will be the same. Therefore,
rA
vA =
rB
vB .
Now consider the velocity triangle formed by vA = vB +vA/B.
Clearly, vA is parallel to rA, and vB is parallel to rB. In addition, if collision is to occur, vA/B will be
parallel to rA/B, since the position and velocity triangles will, in this case, be similar. We see, therefore,
that the condition for the two planes to collide is that the relative velocity between them is parallel to the
relative position vector. If aircraft B uses a polar coordinate system (common for radar measurements),
then the relative position of A with respect to B will be of the form rA/B = rer. Therefore, the velocity
also has to be of that form, which implies that vθ = r ˙θ = 0, or θ = constant. That is, the angle under which
B sees A (sometimes called the bearing angle) should not change.
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ADDITIONAL READING
J.L. Meriam and L.G. Kraige, Engineering Mechanics, DYNAMICS, 5th Edition
2/8
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