SRTERMS.TXT Dictionary of TERMS used in Solar Radiation 2008/06/09 Aphelion Time and location when the Earth is furthest from the Sun in its annual revolution about the Sun. Autumnal Equinox Time and location of the Earth when the Sun is directly over the equator and is heading into the southern hemisphere. Axis Axis of rotation of the Earth; line that passes through the center of the Earth and each pole. Climatic Precession Equal to eccentricity times sine of longitude of Parameter perihelion. Declination Angle Latitude above which the Sun is directly over head. Eccentric Anomaly Spatial angle measured along the eccentric circle of the Earth's orbit from perihelion to the Earth's absisca (where the absisca is directed from the center of the eccentric circle to perihelion). Eccentric Circle Circle that circumscribes an ellipse. Eccentricity Eccentricity of the Earth's orbital ellipse about the Sun. One of the three orbital parameters. Its symbol is e = sqrt(a²-b²)/a. Greenwich Meridion Longitude line that passes through the observatory at Greenwich, England. It is the 0° longitude line. Insolation Energy per square meter of sun light incident at top-of-atmosphere. The square meter should be perpendicular to a vertical ray from the Earth's center. Insolation = S cos(Z) a² / r² , where S = Solar Constant (W/m²), Z = Zenith angle, a = semi-major axis of the Earth's orbital ellipse, r = distance from Earth to Sun. cos(Z) = sin(D) sin(J) + cos(D) cos(J) cos(T) , D = Declination angle, J = latitude, T = local time in temporal radians, T = 0 at noon. Insolation used to mean sun light incident on the surface should be called "surface insolation". Longitude of Spatial angle from moving vernal equinox to Perihelion perihelion with Sun as angle vertex. One of the three orbital parameters. Its symbol is a small omega with a tilda above it. Mean Anomaly Temporal angle from perihelion to current time in units of 2*pi per tropical year. Obliquity Dihedral angle between the Earth's equatorial plane and its orbital plane. One of the three orbital parameters. Its symbol is a small epsilon. Orbital Ellipse An inverse square force field, such as the Sun's gravitational force field, allows stable elliptical orbits of point masses or planets. The center of the force field, the Sun, is located at one of the two foci of the ellipse. Orbital Energy Energy of the Earth due to its orbit about the Sun: E = .5*Me*v² - G*Ms*Me/r = -.5*G*Ms*Me/a , where G is the universal gravitational constant, Ms is the mass of the Sun, Me is the mass of the Earth, v is the speed of the Earth in its orbit, r is the distance between the Earth and Sun, a = semi-major axis of the Earth's orbital ellipse. The zero reference level for geopotential energy of the Earth with respect to the Sun is at infinity. Perihelion Time and location when the Earth is closest to the Sun in its annual revolution about the Sun. Precession Short name for the climatic precession parameter. Revolution Cyclic movement of the Earth through its orbit about the Sun. One revolution takes one tropical year. Rotation Cyclic movement of the Earth around its axis. One rotation takes about 23 hours, 56 minutes. Each year, the Earth rotates about its axis once more than the number of days in a year. Semi Major Axis One half of the major axis of the Earth's orbital ellipse. Its symbol is a. Semi Minor Axis One half of the minor axis of the Earth's orbital ellipse. Its symbol is b. Solar Constant Mean annual incident solar radiation the Earth receives from the Sun divided by cross sectional area of the Earth; apprxoximately 1367 W/m². Spring Equinox Same as vernal equinox. Summer Solstice Time and location of the Earth when the Sun is directly overhead the most northerly latitude in the annual cycle. Tropical Year Average time from one vernal equinox to the next; approximately 365.2425 days. True Anomaly Spatial angle from perihelion to current location with Sun as angle vertex. Vernal Equinox Time and location of the Earth when the Sun is directly over the equator and is heading into the northern hemisphere. Winter Solstice Time and location of the Earth when the Sun is directly overhead the most southerly latitude in the annual cycle. Zenith Angle Angle between an upward vertical ray from a point on the surface of the Earth and a ray from that point to the Sun. Many of the terms used here come from "Basic Physics of the Solar System", by V.M. Blanco and S.W. McCuskey, 1961, Addison-Wesley.