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Published byDominick Grant Modified over 8 years ago
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Radiation Solar radiation drives the atmosphere. The amount of radiation the Earth’s surface and atmosphere receives is dependent on: l The angle at which the sun’s rays strike the Earth’s surface at various latitudes. –Latitude — Time of year –Elevation-Zenith angle— Refraction of radiation –Declination angle— Altitude of site above sea level The time of day& year. Length of day. l Depleting effects of the atmosphere. l Depletion by particles between Sun and Earth.
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The planets Planets orbits
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Kepler’s Laws 1. The orbits of the planets are ellipses with the Sun at one focus of the ellipse. l Most have nearly circular orbits.
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a = 1/2 longest axis = semi-major axis b = 1/2 shortest axis = semi-minor axis c = distance of foci from center Eccentricity, e = c/a Always less than 1. Earth: e = 0.0167
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2. The line joining the planet to the Sun sweeps out equal areas in equal times as the planet travels around the ellipse.
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3. The ratio of the squares of the revolutionary periods for two planets is equal to the ratio of the cubes of their semi-major axes. If period is given in Earth years and distance in Astronomical units, AU, then: and, If period is given in Earth days and distance in gigameters, Gm, then:
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So, the time for one orbit is given by: where, Y = period of planet in years, a = 0.1996days/Gm -3/2 R = Distance planet is from Sun in Gm A Gigameter = 10 6 km = 10 9 meters
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Earth Satellites Also move in elliptical orbits which are nearly circular. Consider a satellite moving in a circular orbit.
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Acceleration is: In diagram, v points toward the orbit center, so acceleration also points toward orbit center. Called centripital “center seeking” acceleration, a c. The vectors, v, v o, and v form a triangle geometrically similar to triangle ABC. The angle is equal to the angle between CA and CB. Then,
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Or, Then, Since, Then, satellites moving in a circular orbit are moving with an acceleration: which is directed toward the center of their orbit.
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The force giving the satellite the acceleration it has (directed toward the center of its orbit is gravity). The force of gravity is given by: Then, since F=ma, G = Gravitational Constant
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Let t orbit be the time to complete one orbit of the earth. The distance that satellite travels in one orbit is 2 r. Since, Then, and, Substituting into the force equation gives:
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Rearranging gives: For a satellite moving in a circular orbit.
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Season Effects
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Amount of incoming solar radiation (insolation) received at the Earth’s surface is dependent on: l Angle at which sun’s rays strike the Earth. l Time of day l Depleting effects of atmosphere. l Length of day.
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Determining Elevation angle of Sun at noon. Must know solar declination angle. d = Julian date of year. d r = 173 r = 23.45 o d y = 365 or 366 C = 360 or 2
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Graphically: Equation: = latitude, e = longitude, t UTC = Universal Coordinated Time, t d = 24 hours, = elevation angle, s = solar declination angle.
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Azimuth angle: Angle of Sun’s position relative to north is: where, = azimuth angle, s = solar declination angle, = latitude, = zenith angle = (C/4)- C = 360 or 2
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Sunrise, Sunset & Twilight Geometric sunrise/sunset: Center of sun has zero elevation angle. Apparent sunrise/sunset: Top of sun crosses horizon as viewed by observer. Center at elevation angle of -0.833 o. Civil twilight: Sun center no lower than -6 o. Military twilight: Sun center no lower than - 12 o. Astronomical twilight: Sun center no lower than -18 o.
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Corresponding times: where, t d = 24 hours (length of day) e = longitude = latitude, s = solar declination angle, = elevation angle C = 360 or 2
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Flux Flux density: Rate of transfer of a quantity across a unit area (perpendicular to the flow) per unit time. l Mass flux: kg/m 2 s l Heat flux: J/m 2 s or W/m 2
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Kinematics: The branch of mechanics dealing with the description of the motion of bodies or fluids without reference to the forces producing the motion.
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Propagation of radiation Speed of light varies with the medium through which it passes. In a vacuum: c o = 299, 792, 458m/s Wavelength:, in units meters/cycle or m, where, v = frequency, in units of Hz = cycles/s, and m = 1 x 10 -6 m. Wavenumber: , number of waves per meter, = 1/ cycles/m. Circular (angular) frequency = radians/s = 2 v
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Emission Any object with temperature above absolute zero emits energy. Blackbody: a perfect emitter. Emits the maximum possible radiation for its temperature.
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