Under certain conditions, tsunami waves encountering land will develop into bores. A bore is a surge of water much like what would be expected if a dam failed suddenly and emptied a reservoir into a river bed. In the case of a bore traveling from the ocean into a dry river bed, one research study shows that the velocity V of the tip of the bore is proportional to the square root of its height H. The power function formula is given below, where k is a constant. VKH0.5 (a) A bore travels up a dry river bed. By how much does the wave velocity change when its height is reduced to a third of its initial height? The velocity changes by a factor of (b) By how much does the bore height change when the velocity of the tip is reduced to a quarter of its initial velocity? The height is reduced to of the initial height. (c) If the tip of one bore surging up a dry river bed is two times the height another, how do their velocities compare? The velocity of the first is times that of the other.
Continuous Probability Distributions
Probability distributions are of two types, which are continuous probability distributions and discrete probability distributions. A continuous probability distribution contains an infinite number of values. For example, if time is infinite: you could count from 0 to a trillion seconds, billion seconds, so on indefinitely. A discrete probability distribution consists of only a countable set of possible values.
Normal Distribution
Suppose we had to design a bathroom weighing scale, how would we decide what should be the range of the weighing machine? Would we take the highest recorded human weight in history and use that as the upper limit for our weighing scale? This may not be a great idea as the sensitivity of the scale would get reduced if the range is too large. At the same time, if we keep the upper limit too low, it may not be usable for a large percentage of the population!
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