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Since this is a real-world problem, it is not sufficient to check to
see if our answer satisfies the equations, we must also verify that it
is a reasonable answer to the original problem. Since the time correction,
D, is related to the number of time zones crossed, our computed
value Now let's consider the variable T. Since we have used the same variable in both equations, we have assumed that the travel time in both directions is the same. In reality, it takes longer to travel from Geneva to New York (east to west) than from New York to Geneva (west to east). Professor Tapia chose to make the simplifying assumption that the travel times for both legs of the trip are the same. Scientists often make this kind of assumption because it makes the problem easier (or possible) to solve. Sometimes the real problem is too difficult because the additional information needed to formulate it correctly is too complicated or is not available. Whenever we make a simplifying assumption, however, we must consider the effect that simplifying the model has on the solution. In this case, Professor Tapia felt that he could ignore the difference in travel time because he expected it to be small compared to the total travel time.
Professor Tapia initially built a model that didn't assume
equal travel time.
He defined T1 to be the time in flight from New York to Geneva,
T2 to be the time in flight from Geneva to New York, and D
to be the correction for time zones crossed.
Then the equations for the trip out and the trip home are
So far, we have specified two conditions on three unknowns. So, this model is not complete as it stands; it would have an infinite number of solutions. A third equation relating T1, T2, and D is needed.
It seems plausible that the difference in travel times should
be proportional to the number of time zone boundaries crossed.
Recall that D has units of time and is increased by one hour
as soon as a time zone boundary is crossed.
So a reasonable form for the third equation is
It says that the difference in travel times is obtained by multiplying the time correction, D, by some constant, a. Now we have three conditions relating our three variables, but we can't use them to determine an answer to our problem until we have a value for a. This constant depends on factors such as prevailing winds and the rotation of the earth, and it will be difficult to calculate even if that data is known. So Professor Tapia made the reasonable assumption that a=0, which is equivalent to assuming T1 = T2 and leads to the simplified model (2.2). Recall that D, the time correction, is determined by the number
of time zone boundaries crossed and must be a whole number. The simple
model provided the value We were unable to specify a value for the constant a in (2.4),
so we assumed that a = 0. Now that we have values for T1,
T2, and D, we can substitute this information
into Equation (2.4) and compute that the corresponding value for
a is
Due to the rotation of the earth and prevailing winds. |
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Updated: February 21, 2001
Copyright © 2001 Richard Tapia and Cynthia Lanius