Everyone should answer Question #1 (25 pts)
ATMO/ECE 489 students should then answer 3 of the remaining 6
questions (20 pts each)
ATMO/ECE 589 students should answer any 4 of the remaining
questions (20 pts each)
1.
Please answer any 5 of the following short answer questions
(a) What
two parameters of the lightning return stroke current
waveform are responsible for producing high voltages on a
grounded down conductor connected to a lightning
rod? Give typical values for these two parameters.
(b) A cloud-to-ground discharge has a
duration that is usually less than 1 second. Why
does the thunder last much longer than that?
(c) Explain how the Optical Transient
Detector and the Lightning Imaging Sensor on satellites
are able to detect lightning optical signals during the
day against the very bright background of sunlight
reflected by the top of the thunderstorm cloud.
(d) Explain why a series of lightning
rods installed on the roof of a building might adequately
protect against high current amplitude return strokes but
not against the lower current amplitude strokes.
(e) Why would two down conductors in the
lightning protection system sketched below be preferable
to just a single down conductor?
(f) What do you think is the simplest and
most effective way of protecting sensitive home electronics
from damage during a lightning storm?
(g) A two station network of magnetic
direction finders would not do a very good job locating
lighting that strikes on the baseline between the two
stations. Why is this? What two ways are there
that the magnetic direction finder data could be used to
improve the accuracy of locations on the baseline.
(h) Where are the highest lightning flash
densities found in the world? Is there more lightning
over the land or over the ocean? When during the year
does the peak lightning activity occur?
(i) Describe the sequence of events that
occur during a rocket triggered lightning discharge. In
what way(s) is a triggered discharge different from a natural
cloud-to-ground discharge? In what way(s) are the two
kinds of discharges similar?
(j) Describe how lightning return stroke
currents can be measured directly and remotely.
2.
Assume that a return stroke is propagating upward at a constant
speed v. Show that the height of the visible channel, H(t),
that an observer a distance R away would see at time t is
3.
In our Friday
April 3 class we looked at some of the characteristics of
lightning striking aircraft. Many of the aircraft in those
research studies made measurements of the thunderstorm electric
fields. In particular, they wanted to determine what field
amplitudes were needed for an aircraft to initiate
lightning. Field mills were mounted at multiple locations on
the aircraft body and a complex analysis procedure was used to
determine the 3-dimensional field surrounding the aircraft and
also to account for any charge that might have built up on the
aircraft. The locations of 5 field mills on the Convair
CV580 and the Transall C160 are shown below
This question will make use of a much simpler geometry, a
conducting sphere, and will assume the sphere is placed in a
uniform, vertically oriented, ambient electric field (the aircraft
studies generally assume that the field is uniform but of unknown
orientation).
In our January
30 lecture we derived the potential function,
Φ(r,θ) in the space surrounding the sphere
The problem geometry is shown above. The
potential function that we ended up with is shown below
One of the boundary conditions that we used when working out
the problem was that the potential was constant on the surface
of the sphere, that is the case above when r = a. Now we
will imagine that the sphere is charged. The potential
function for a point charge is
We'll add this expression to the equation above for
the uncharged sphere (here's
a reference that convinced me this is a valid approach)
(the Φo term was dropped in this
expression). Note that Φ is constant on the
surface of the sphere in this case also (r = a in the
expression above).
The Final Exam question has three parts:
(a) The charge on the sphere is clearly not positioned
at the center of the sphere. Rather it is spread out
over the surface of the sphere. Using the expression
above show that the surface charge density on the surface of
the sphere is
(b) Integrate this expression for surface charge
density over the surface of the sphere
(c) Imagine you were able to measure the electric field at the
top and bottom surfaces of the sphere (just as field mills are
able to measure the electric field at various locations on an
aircraft). Show how you could use the measurements of Etop
and Ebottom to determine both the ambient field, Eo,
and the charge on the conducting sphere, q.
The exam question has 3 parts:
(a) Would you have expected the higher conductivity in
May 1986 to have increased or decreased the strength of the fair
weather electric field at the ground?
(b) Use the positive conductivity values in the figure
above to determine the positive small ion concentrations, n+,
before and after the arrival of the radioactive plume.
(c) Assuming steady state conditions and neglecting small
ion to particle attachment, determine the small ion production
rate, q, before and after the arrival of the plume. You
may assume the numbers of positive and negative small ions are
equal.
The charge on an electron is 1.6 x 10-19 C, you may
used the values given for 0 km altitude on the "Summary
of Electric Parameters vs Altitude" handout for any other
constants that you might need.
5.
Assume that there are N strikes per kilometer per year to a long
power line. What is the probability that the nearest strike
is between x and x + dx. Basically you are being asked to
derive a one-dimensional version of the nearest neighbor
probability density function. You can assume that the point
of reference is on the left end of the line (0 in the sketch
below) and that the line extends to the right without limit.
6.
Assume that a cloud-to-ground discharge occurs 250 km from one
of the sensors in the National Lightning Detection Network.
Before being used to estimate the peak currents for the strokes in
the discharge, the measured peak B field amplitudes would be range
normalized to 100 km and a correction for attenuation of the
signal by propagation would be made. Discuss how these are
both done. What relation would then be used to determine the
peak current values?
7. The sensors in the National Lightning
Detection Network use measurements of the two perpendicular
components of the horizontal magnetic field radiated by a
lightning discharge to determine a bearing angle to the strike
point. The location of a strike could then be determined by
finding the intersection of vectors from as few as two stations
(accuracy is better when vectors from multiple stations are
used).
The NLDN sensors also measure the time of arrival (TOA) of the
lightning signal at each sensor. TOA data serve as an
additional, independent, way of locating a lightning
discharge. In this case a single TOA difference measurement,
Δt, for a pair of stations isn't enough to locate a
strike. All you can say for a single TOA difference is that
the strike point was located somewhere on a hyperbola. This
is in fact the definition of a hyperbola: "the set of points in a
plane whose distance to fixed points in the plane have a constant
difference." The object of this problem is to demonstrate
the validity of that statement.
We'll consider the geometry shown below. Sensors are located
a Points 1 & 2 located at (-c, 0) and (+c, 0). The
hyperbola crosses the x-axis at x = a. Point
(x, y) is just an arbitrary point on the hyperbola and is a
distance d1 from Point 1 and a distance d2
from Point 2. The values of d1
and d2
will change
depending on x and y but the difference d1-
d2 will remain the same for any point on the hyperbola.
The problem has three parts:
(a) Show that d1- d2=
2a (hint: since d1-
d2 remains constant, you can choose any
point on the hyperbola to determine d1-
d2 )
(b) Demonstrate that the expression above after some
manipulation leads to
(c) Show that at large values of x and y the hyperbola
becomes a straight line