Azimuth between points on sphere or ellipsoid
az = azimuth(lat1,lon1,lat2,lon2)
az = azimuth(lat1,lon1,lat2,lon2,ellipsoid)
az = azimuth(lat1,lon1,lat2,lon2,units)
az = azimuth(lat1,lon1,lat2,lon2,ellipsoid,units)
az = azimuth(track,...)
az = azimuth(lat1,lon1,lat2,lon2) calculates the great circle azimuth from point 1 to point 2, for pairs of points on the surface of a sphere. The input latitudes and longitudes can be scalars or arrays of matching size. If you use a combination of scalar and array inputs, the scalar inputs will be automatically expanded to match the size of the arrays. The function measures azimuths clockwise from north and expresses them in degrees or radians.
az = azimuth(lat1,lon1,lat2,lon2,ellipsoid) computes the azimuth assuming that the points lie on the ellipsoid defined by the input ellipsoid. ellipsoid is a referenceSphere, referenceEllipsoid, or oblateSpheroid object, or a vector of the form [semimajor_axis eccentricity]. The default ellipsoid is a unit sphere.
az = azimuth(lat1,lon1,lat2,lon2,units) uses the input string units to define the angle units of az and the latitude-longitude coordinates. Use 'degrees' (the default value), in the range from 0 to 360, or 'radians', in the range from 0 to 2*pi.
az = azimuth(lat1,lon1,lat2,lon2,ellipsoid,units) specifies both the ellipsoid vector and the units of az.
az = azimuth(track,...) uses the input string track to specify either a great circle or a rhumb line azimuth calculation. Enter 'gc' for the track string (the default value), to obtain great circle azimuths for a sphere or geodesic azimuths for an ellipsoid. (Hint to remember string name: the letters "g" and "c" are in both great circle and geodesic.) Enter 'rh' for the track string to obtain rhumb line azimuths for either a sphere or an ellipsoid.
Find the azimuth between two points on the same parallel, for example, (10ºN, 10ºE) and (10ºN, 40ºE). The azimuth between two points depends on the track string selected.
% Try the 'gc' track string. az = azimuth('gc',10,10,10,40) % Compare to the result obtained from the 'rh' track string. az = azimuth('rh',10,10,10,40)
Find the azimuth between two points on the same meridian, say (10ºN, 10ºE) and (40ºN, 10ºE):
% Try the 'gc' track string. az = azimuth(10,10,40,10) % Compare to the 'rh' track string. az = azimuth('rh',10,10,40,10)
Rhumb lines and great circles coincide along meridians and the Equator. The azimuths are the same because the paths coincide.
If you are calculating both the distance and the azimuth, you can call just the distance function. The function returns the azimuth as the second output argument. It is unnecessary to call azimuth separately.
An azimuth is the angle at which a smooth curve crosses a meridian, taken clockwise from north. The North Pole has an azimuth of 0º from every other point on the globe. You can calculate azimuths for great circles or rhumb lines.
A geodesic is the shortest distance between two points on a curved surface, such as an ellipsoid.
A great circle is a type of geodesic that lies on a sphere. It is the intersection of the surface of a sphere with a plane passing through the center of the sphere. For great circles, the azimuth is calculated at the starting point of the great circle path, where it crosses the meridian. In general, the azimuth along a great circle is not constant.
A rhumb line is a curve that crosses each meridian at the same angle. For rhumb lines, the azimuth is the constant angle between true north and the entire rhumb line passing through the two points.
For more information on the distinction between great circles and rhumb lines, see Great Circles, Rhumb Lines, and Small Circles in the Mapping Toolbox™ documentation.
Azimuth calculations for geodesics degrade slowly with increasing distance and can break down for points that are nearly antipodal or for points close to the Equator. In addition, for calculations on an ellipsoid, there is a small but finite input space. This space consists of pairs of locations in which both points are nearly antipodal and both points fall close to (but not precisely on) the Equator. In such cases, you will receive a warning and az will be set to NaN for the "problem pairs."
Geodesic azimuths on an ellipsoid are valid only for small eccentricities typical of the Earth (for example, 0.08 or less).