"Azimuth and Elevation" is a way of locating a geostationary satellite in the sky, based on your latitude & longitude. For the Seattle, Washington area, for example, the basic bird for Dish Network installs is at Azimuth 150, Elevation 34. So to locate the point in the sky where the bird is, you start with a compass heading of 150 degrees (which is 30 degrees East of due South) and then point up 34 degrees above the horizon.
Given coordinates of two points and directions (bearings or azimuths) from those two points, find the coordinates of the point of intersection, assuming that the lines do intersect and are not parallel. Use the Cantuland method to calculate the coordinates of the northing and the easting. This is a simplification of a process that came from the use of simultaneous equations from matrix algebra that employed a trigonomic identity for tangent functions.Northing of the point of intersection:1. Convert the azimuth of the first line to degrees and decimal degrees.2. Find the tangent of the azimuth of the first line.3. Step-two, times the northing of the point on the first line.4. Step-three, minus the easting of the point on the first line.5. Convert the azimuth of the second line to degrees and decimal degrees.6. Find the tangent of the azimuth of the second line.7. Step-six, times the northing of the point on the second line.8. Step-seven, minus the easting of the point on the second line.9. Step-four, minus step-eight.10. Step-two, minus step-six.11. Step-nine, divided by step-ten. That's the northing of the intersection.Now let's find the easting. Most of the steps are the same, except a little bit is added into the process. See steps 4A, 8A and 9.Easting of the point of intersection:1. Convert the azimuth of the first line to degrees and decimal degrees.2. Find the tangent of the azimuth of the first line.3. Step-two, times the northing of the point on the first line.4. Step-three, minus the easting of the point on the first line.4A. Step-four, times step-six.5. Convert the azimuth of the second line to degrees and decimal degrees.6. Find the tangent of the azimuth of the second line.7. Step-six, times the northing of the point on the second line.8. Step-seven, minus the easting of the point on the second line.8A. Step-eight, times step-two.9. Step-4A, minus step-8A.10. Step-two, minus step-six.11. Step-nine, divided by step-ten. That's the easting of the intersection.This works unless the azimuth of one of the lines is 90 degrees or 270 degrees. Tangent of the azimuth of 90 degrees or 270 degrees will result in "undefined", and the above will not work. In this case, swap all calls for "easting" to "northing"; and swap all calls for "northing" to "easting"; and swap the calls for the Tangent function to replace them with Cotangent functions. This adjustment to the process will work for all intersections except when the azimuth of one of the lines is zero degrees or 180 degrees. In those cases, use the unmodified steps as outlined above to take care of those issues.
It is read off the azimuth scale, possibly magnified with a so-called microscope. say, 32 degrees, ll minutes. finer degrees of reading-out are possible with some types. This type of theodolite operation is not too different in principle than taking bearings on objects with a magnetic compass, and reading off the direction in degrees.
A BACK AZIMUTH IS A PROJECTION OF THE AZIMUTH FROM THE ORIGIN TO THE OPPOSITE SIDE OF THE AZIMUTH CIRCLE. i.e. THERE ARE 360 DEGREES IN AN AZIMUTH CIRCLE, THUS THE OPPOSITE DIRECTION IS 180 DEGREES.
An azimuth thruster is an engine and ship's propeller in a pod which is azimuth adjustable.
To convert a magnetic azimuth to grid azimuth, subtract G-M angle.” If you have a magnetic azimuth of 270 degrees, and the G-M angle is 8 degrees, your grid azimuth will be 262 degrees.
The point from where an azimuth originates is the center of an imaginary circle.
Azimuth Systems was created in 2002.
RBG-Azimuth was created in 2006.
Azimuth - album - was created in 1977-03.
The point from where an azimuth originates is the center of an imaginary circle.
Astronomical azimuth is measured from true north, while geodetic azimuth is measured from the north-south line of a geodetic datum. In other words, astronomical azimuth uses the Earth's axis as reference, while geodetic azimuth is corrected for the Earth's shape and gravity. This difference leads to variations in azimuth readings, especially over long distances.
The point from where an azimuth originates is the center of an imaginary circle.
The point from where an azimuth originates is the center of an imaginary circle.
The point from where an azimuth originates is the center of an imaginary circle.