The latitude and departure are the rectangular components of a survey line when resolved along the true north-south and east-west axes respectively. For a line AB of length l and reduced bearing (or azimuth) θ, the components are
L = +l cos θ
D = l sin θ

Latitude: Projection of a line on the north-south direction.
Departure: Projection of a line on the east-west direction.
The sign of latitude and departure depends on the quadrant in which the line lies. The algebraic signs for L and D must be applied consistently when summing components for a traverse. Diagrams that show the four quadrants and the corresponding signs of latitude and departure are given below.


Here, l1, l2, l3 and l4 are the lengths of OA, OB, OC and OD respectively.

When a traverse is computed by resolving each line into latitudes and departures and summing those components, the coordinates of stations are obtained independently in northing and easting. If the algebraic sums of latitudes or departures for a closed traverse are not zero, a closing error exists.
The closing error in latitude and departure may be shown symbolically (see figures or formula images below).





When a closing error is present it must be distributed among the traverse sides. Common methods are described below.
The Bowditch method (also called the Compass rule) distributes the total linear error in latitude and departure to each line in proportion to the length of that line. It is based on the practical observation that the error in linear measurement is proportional to √l and the error in angular measurement is proportional to 1/√l, so the dominant source of coordinate error is proportional to length.

Notation used in the formula image:
The transit rule distributes the total error in latitude and departure to each line in proportion to the absolute value of its latitude and departure respectively.
Corrections are given by
CL = (L / LT) × ∑L
CD = (D / DT) × ∑D
Where
The axis method adjusts traverse coordinates by projecting the network onto chosen axes and applying corrections so that the final coordinates meet closure conditions. The formula images below show corrections to a particular length or coordinate produced by axis adjustments.



Definition: Horizontal control for geodetic surveys is often established either by triangulation or by a precise traverse. In triangulation a network of inter-connected triangles is observed: the length of only one line (the base line) is measured directly and the angles of the triangles are measured precisely to obtain the remaining sides by trigonometry.

The strength of figure is a measure used when designing a triangulation network; it indicates how well the figure will withstand observational errors and still permit required precision in computed sides. Quantitative expressions are used to estimate probable errors in computed sides based on the number of directions observed and the angular precision.
A relation given in some treatments expresses the square of a probable error in the logarithm of a side in terms of observational quantities:
L2 = (4/3) d2 R

Where
A signal is a device or mark erected to define the exact position of an observed station in triangulation. Signals and towers must be designed to be visible at the required sighting distance and to minimise errors of bisection (phase).
where D is the distance of sight in kilometres.
Phase correction when the observation is made on the bright portion is illustrated below. Symbols used in the figure are explained thereafter.

Where

When the observation is made on the bright line (edge) of the illuminated part of the signal, the appropriate correction diagram is shown below.

The general routine in a triangulation survey normally includes the following operations in order:
D = √(2Rh + h²) where R is the mean radius of the Earth.
For usual heights small compared with the Earth's radius the term h² is negligible and
D ≈ √(2Rh).
With h in metres and D in kilometres the practical approximate relation is
D ≈ 3.57 √h
which is useful for quick checks of intervisibility (assuming standard refraction conditions).
is the elevation required at B so that the line of sight is tangent to the Earth at some intervening point, the relation (using practical constants) may be written as:
h = 0.06728 D² (with D in km gives h in metres)
Accordingly, if D1 is the distance from A to the tangency point and D2 = D - D1 is the distance from B to that point then
h1 = 0.06728 D1²
h2 = 0.06728 D2²



Here D1 and D2 are in kilometres and h1, h2 are in metres. These relations include the customary reduction factor for the combined effect of curvature and average atmospheric refraction used in field practice.
This method provides a practical formula to compute the height of the line of sight at an intervening obstruction point C between two stations A and B. It accounts for the geometry of the problem and the curvature/refraction reductions used in triangulation practice.
Let

The formula for the height h of the line of sight at the obstruction is given by the relation illustrated below.

When x, s and R are substituted in miles and h1, h2, h are in feet, appropriate numerical factors for curvature and refraction are used. When x, s and R are in kilometres and heights are in metres, the factor commonly used for combined curvature and refraction reduction is approximately 0.06728 (that is, 1 - 2m/2R ≈ 0.06728 under the standard assumptions used in the method).
Notes and practical points:
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