Hmmm, ok... 4times, are you still here? Elassowipo? WilsonJo? Or any other statisticians who would care to give me a hand? :arf:
Until one of those guys gets here, I'll try my best to explain how a faulty interpretation of the data led them to order a launch, even though they shouldn't have.
First off, here's a summary of the decision to launch in cold weather, including a description of the joint erosion experienced by O-rings:
https://en.wikipedia.org/wiki/Space_Shuttle_Challenger_launch_decision
There's no doubt that the failure of the O-ring was the physical cause of the disaster; the real question is
why the launch was ordered in a lower temperature than was prudent, given that the NASA people knew the O-rings were sensitive to drops in temperature.
And here's a graph showing the distribution (temperature on the X axis, erosion on the Y) from the prior launches they had data for:
The limited data was viewed as having a negative linear distribution (erosion goes down as temperature goes up, and vice-versa, along a fairly predictable line; that's the straight line you see in the middle of the graph, between the two semi-curved confidence interval lines). However, that model was incorrect; the proper model would have been curvilinear (starting out like the straight line, but curving further up as it goes further to the left, until it's almost vertical around the 40-degree mark) meaning that, as temperature drops, erosion increases significantly more for each degree colder that it gets.
Linear: Y = (X - 2)
Curvilinear: Y = 2(X - 2)
(I really suck at algebra, hopefully one of you math whizzes can fix this for me if I'm getting it wrong... it's meant to be illustrative rather than accurate).
In plain English, a linear model suggests that a drop in temperature has a cumulative effect on erosion; for each 1-degree drop in temperature, the erosion is increased by a factor of 2 units. A curvilinear model has a multiplicative effect on erosion; for each 1-degree drop in temperature, the erosion is
multiplied by a factor of 2 units (again, not real numbers, meant to be illustrative rather than accurate).
Now, if the spread of the data for temperature is only 2 degrees, then nobody notices a difference;
2 + 2 = 4
2 x 2 = 4
It's only when you get farther away from the mean temperature that the differences start to show up. Here's what happens if the spread is increased to 4 degrees:
Linear model: (2 + 2 + 2 + 2 = 8)
Temperature drops by 4 degrees; erosion increases by 8 units
Curvilinear model: (2 x 2 x 2 x 2 = 16)
Temperature drops by 4 degrees; erosion increases by 16 units
The temperature on the day of the launch was around 31 degrees (F). The people at NASA only had data from 23 launches, none of which had occurred at such a low temperature, so they had to extrapolate the limited data into uncharted territory. Because they thought the linear model was the best fit, they assumed the O-rings would hold (around 80 on the Y axis, which, as the graph suggests, would have been within the 95% confidence interval). However, because the distribution was actually curvilinear, the appropriate data point was actually around 135 on the Y axis, which is outside this interval, suggesting catastrophic failure of the O-ring was likely to occur. Sadly, they didn't consider this possibility, and the shuttle exploded during launch.
Here's the more complicated explanation:
The Presidential Commission on the Space Shuttle Challenger Accident (1986) established that the loss of the space shuttle Challenger on 28 January 1986 occurred because "a combustion gas leak through the right Solid Rocket Motor aft field joint initiated at or shortly after ignition eventually weakened and/or penetrated the External Tank initiating vehicle structural breakup". Engineers at Morton Thiokol, the makers of the solid rocket motors, and experts at the National Aeronautics and Space Administration (NASA) debated the possibility of field-joint failure due to primary and secondary O-ring failure the night before the ill-fated launch. The point of contention was the effect of the temperature at the time of launch on the O-ring performance. The engineers were in disagreement about the implication of data from 23 previous shuttle launches on the thermal distress to the field-joint primary O-rings. Despite some objections, at the conclusion of their discussion the engineers at Morton Thiokol transmitted a facsimile to NASA stating that "temperature data [are] not conclusive on predicting primary O-ring blowby". On the morning of 28 January 1986 the estimated temperature of the primary O-rings on the Challenger solid rocket motors was 31 ◦F (−0.6 ◦C). This was 22◦F (12.2 ◦C) lower than the minimum temperature recorded in all previous shuttle launches [◦C = (◦F − 32)5/9]. The Presidential Commission on the Space Shuttle Challenger Accident (1986) found that "a careful analysis of the flight history would have revealed the correlation of O-ring damage in low temperature".
The Challenger disaster has thus become a paradigm for improving risk analysis of the space shuttle (Paté-Cornell and Dillon, 2001). In particular, Dalal et al. (1989) present a procedure for assessing the probability of catastrophic failure at launch due to a failure of 6 at least one of the six field joints. A key input is the probability of primary O-ring damage, conditional on the temperature at the time of launch. They calculate this probability at 31◦F using logistic regression and, admitting uncertainty about the logistic regression parameter estimates, they also construct a 90% bootstrap confidence interval around the calculated probability. But as Lavine (1991) points out, this approach presumes that the logistic regression is the correct model whereas, in fact, it is possible to fit the Challenger O-ring data equally well using other model forms from the class of generalized linear models. He shows that these other models provide vastly different probabilities of O-ring damage at 31 ◦F. Dalal and Hoadley (1991) defend the generalized linear models by stating that a detailed analysis should involve experts who would assign a probability to each of the possible models and then combine the response probabilities.
Lavine (1991) correctly identifies the problem of determining the probability of O-ring damage at 31 ◦F as an extrapolation problem. Assuming a monotone relation between probability and temperature, he computes nonparametric bounds on the probability of O-ring damage at 31 ◦F; these bounds give the interval [1/3,1]. Yet, his suggestion of using the lower bound of 1/3 as the probability of O-ring damage at 31 ◦F in a risk assessment falls short of providing a theoretically justified forecast. First, the proposed approach does not extract all information from data and ignores expert judgment. Second, the proposed lower bound on the probability underestimates the risk of the catastrophic failure. When it is recognized that in order to solve this forecasting-extrapolation problem, the empirical evidence from previous shuttle flights must be combined with subjective input from experts, Bayesian approach is not only structurally optimal, but also practically advantageous. The purpose of this paper is to present a Bayesian forecasting model for the probability of primary O-ring damage, conditional on the temperature at the time of launch, and to compare that model with the generalized linear models and nonparametric approach advocated in earlier risk analyses of the Challenger O-ring data.
Hence, the Challenger disaster is now used as an example in all university-level statistics textbooks. A terrible shame that seven people had to die as a result of faulty data analysis, and today, this debacle serves as a potent warning against assuming too much from a small sample of data.