Aspects of this topic are discussed in the following places at Britannica.
...of the Earth’s Equator.) Angle i is the inclination of the orbital plane to the reference plane. The line of nodes is the intersection of the orbit plane with the reference plane, and the ascending node is that point where the planet travels from below the reference plane (south) to above the reference plane (north). The ascending node is described by its angular position measured...
...elements. Among these are three angles that define the spatial orientation of the orbit: i, the inclination of the orbital plane to the plane of the ecliptic; Ω, the longitude of the ascending node measured eastward from the vernal equinox; and ω, the angular distance of perihelion from the ascending node (also called the argument of perihelion). The three most frequently...
...called the nodes, shown as M and N. V is the vernal equinox, a point on the ecliptic from which several celestial coordinates are measured. The angle VSN, in degrees of arc, is the longitude of the ascending node, i.e., of the point where the moving planet passes north of the plane of Earth’s orbit. M, the descending node, is where the planet passes from north to south. The sum of the...
...the Moon can pass well above or below the Sun. The line of intersection of the planes is called the line of the nodes, being the two points where the Moon’s orbit intersects the ecliptic plane. The ascending node is the point where the Moon crosses the ecliptic from south to north, and the descending node is where it crosses from north to south. The nodes move along the ecliptic from east to...
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