. Criteria for the classification of hydrographic positioning Oceanography. An error circle with a radius of one d can be rms constructed about the intersecting LOP's (Fig. ). Two d is the radius cf the error circle obtained using two rms times the values of a and a in Equation For an x y elliptical error distribution, the probability associated with a specific value of d varies as a function of the rms eccentricity of the error ellipse (Table II). The prob- ability associated with one d varies from percent rms percent, while the probability associated with twc d vari
. Criteria for the classification of hydrographic positioning Oceanography. An error circle with a radius of one d can be rms constructed about the intersecting LOP's (Fig. ). Two d is the radius cf the error circle obtained using two rms times the values of a and a in Equation For an x y elliptical error distribution, the probability associated with a specific value of d varies as a function of the rms eccentricity of the error ellipse (Table II). The prob- ability associated with one d varies from percent rms percent, while the probability associated with twc d varies between percent and Figure The d Error Circle s rms NOS uses d_â, as an accuracy specification. rms â * fc Umbach [Eef. 14, p. 4-25] states that super high freguency direct distance measuring systems would be used only when the value cf dTms is less than or egual to: 41. 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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