. Criteria for the classification of hydrographic positioning Oceanography. occurrence, and is given by P(v) . -<£* () The plot of this equation yields the normal distrifcuticn curve (Fig. ). The height cf the curve above the vertical axis is proportional to the probability of a particular error occurring. The probability of a residual falling between asy two residuals v and v can be computed by integrating 1 2 Equation as P(v) = -ffir dv (). Figure The Normal Distribution This integral is difficult to evaluate analytically so tables have been compiled to aid in c
. Criteria for the classification of hydrographic positioning Oceanography. occurrence, and is given by P(v) . -<£* () The plot of this equation yields the normal distrifcuticn curve (Fig. ). The height cf the curve above the vertical axis is proportional to the probability of a particular error occurring. The probability of a residual falling between asy two residuals v and v can be computed by integrating 1 2 Equation as P(v) = -ffir dv (). Figure The Normal Distribution This integral is difficult to evaluate analytically so tables have been compiled to aid in computations. Fcr v = *a and v = -a, it can be shown that P(v) = In 1 2 ether words, the probability that a particular observation will fall within + 1a of the mean is percent. 29. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original Perugini, Nicholas Monterey, California: U. S. Naval Postgraduate School
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