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S4X = -63A. X . See also:tanA S4L = +54A. Y.tanA S,A = +S4L .Z The calculations described so far suffice to make the angles of the several trigonometrical figures consistent inter se, and to give preliminary values of the lengths and azimuths of the sides and the latitudes and longitudes of the stations. Reduction The results are amply sufficient for the requirements of See also:Principal of the topographer and See also:land surveyor, and they are published in preliminary charts, which give full numerical tion. details of See also:latitude, See also:longitude, See also:azimuth and See also:side-length, and of height also, for each portion of the triangulation—secondary as well as principal—as executed See also:year by year. But on the completion of the several chains of triangles further reductions became necessary, to make the triangulation everywhere consistent inter se and with the verificatory See also:base-lines, so that the lengths and azimuths of See also:common sides and the latitudes and longitudes of common stations should be identical at the junctions of chains and that the measured and computed lengths of the base-lines should also be identical. As an See also:illustration of the problem for treatment, suppose a See also:combination of three meridional and two See also:longitudinal chains comprising seventy-two single triangles with a base-See also:line at each corner as shown in the accompanying c e See also:diagram (fig. 2) ; suppose the three angles of every triangle to have been measured and made consistent. Let A be the origin, with its latitude and longitude given, and also the length and azimuth of the adjoining base-line. With these data processes of calculation are carried through p the triangulation to obtain the lengths and azimuths of the FIG. 2. sides and the latitudes and longitudes of the stations, say in the following See also:order: from A through B to E, through F to E, through F to D, through F and E to C, and through F and D to C. Then there are two values of side, azimuth, latitude and longitude at E—one from the right-See also:hand chains via B, the other from the See also:left-hand chains via F; similarly there are two sets of values at C; and each of the base-lines at B, C and D has a calculated as well as a measured value. Thus eleven See also:absolute errors are presented for See also:dispersion over the triangulation by the application of the most appropriate correction to each See also:angle, and, as a preliminary to the determination of these corrections, equations must be constructed between each of the absolute errors and the unknown errors of the angles from which they originated. For this purpose assume X to be the angle opposite the flank side of any triangle, and Y and Z the angles opposite the sides of continuation; also let x, y and z be the most probable values of the errors of the angles which will satisfy the given equations of See also:condition. Then each See also:equation may be expressed in the See also:form [ax+by+cz] =E, the brackets indicating a summation for all the triangles involved. We have first to ascertain the values of the coefficients a, b and c of the unknown quantities. They are readily found for the side equations on the circuits and between the base-lines, for x does not enter them, but only y and z, with coefficients which are the cotangents of Y and Z, so that these equations aresimply[cot Y.y—cot 'Z.z] E. But three out of four of the See also:circuit equations are See also:geodetic, corresponding to the closing errors in latitude, longitude and azimuth, and in them the coefficients are very complicated. They are obtained as follows. Additional information and CommentsThere are no comments yet for this article.
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