Astronomy 1010-H Planetary Astronomy Fall_2015 Day-19 Course Announcements • How is the sunset/sunrise observing going? • Dark Sky nights – Wed. 10/7 starting at 7:30pm – at the Observatory. • Exam-2 will be Friday, Oct. 9; Ch. 3, 4, & 5 • SW-chapter 5 posted: due Fri. Oct. 9 • No lab next week – Fall Break Emitted Light Luminosity: amount of light leaving a source. The amount and type of light leaving a source changes as an object heats up or cools down. The hotter an object is, the more luminous it is. The hotter an object is, the bluer it is. Dense objects emit a blackbody (or Planck) spectrum. Continuous. Gives light at all wavelengths. Example: incandescent light bulb. For two objects of the same size, the hotter one will: • Emit more total light at all wavelengths. • Emit more total energy every second. • Emit light at shorter wavelengths, on average. Stefan’s Law Flux is the total amount of energy emitted per square meter every second (the luminosity per area). Then: F T 4 where T is the temperature, F is the flux, and (sigma) is called the StefanBoltzmann constant. Hotter objects emit much more energy (per square meter per second) than cool objects. Wien’s Law The peak wavelength of a blackbody is inversely proportional to its temperature. 2 , 900 , 000 nm K peak T Peak wavelength peak : the wavelength of light of a blackbody that is emitted the most. Here the wavelength is in nanometers and the temperature is in kelvin. “Hotter means bluer.” L B 2 4r Brightness is the amount of light arriving at a particular place. Decreases as the distance from a light source increases, obeying an inverse square law. The light spreads out over a greater area. Temperature is a measure of the average speed of the motions of atoms. Kelvin scale: Water freezes/boils at 273 K / 373 K. Absolute zero is when thermal motion stops. Equilibrium Temperature Balance between absorbed and radiated energy. Albedo (reflectance) of a planet. a = 1: 100% reflection a = 0 : 100% absorption Energy absorbed = R2 * L/4d2 * (1 – a) Energy Radiated = 4R2 * T4 Radiation laws help figure out the equilibrium temperatures of the planets. Distant planets are cold mainly because of the inverse square law of light. Balance of heating and cooling. CONNECTIONS 5.1 A stable equilibrium is a balance that is unlikely to change, while an unstable equilibrium can easily be nudged away from its balance point. Static equilibrium involves a situation where forces are balanced and opposing each other, so nothing changes. Dynamic equilibrium involves a situation that is always changing, but remains in balance. MATH TOOLS 5.3 With the Stefan-Boltzmann law, you can find Earth’s flux using its average temperature of 288 K. Using Wien’s law, you can find the Sun’s surface temperature using the fact that its peak wavelength is around 500 nm. MATH TOOLS 5.4 The equilibrium temperature of a planet depends on the energy it receives and its albedo (a), its reflectivity. MATH TOOLS 5.4 The equilibrium temperature of a planet depends on the energy it receives and its albedo (a), its reflectivity. Simplifying: PROCESS OF SCIENCE Confirmation of an idea from different fields of science can be a strong indication of the truth of that idea. Exam-2 To Here! Telescopes & Instruments The telescope is the astronomer’s most important tool. Purpose: to gather light of all kinds. Two kinds of optical telescopes: reflecting and refracting. Invented in 1608 by Hans Lippershey. Telescopes come in three general types Reflectors use mirrors to reflect the light to a focus Refractors use lenses to bend the light to a focus Catadioptric telescopes use both lenses and mirrors Telescopes Telescopes have three functions: 1. Gather light 2. Resolve objects 3. LGP ∝ Area = πR2 Θ = 2.06 X 105 (λ/D) Magnify EXTENDED objects The most important property of any telescope is to gather large amounts of light and concentrate it to a focus. Light Gathering Power Area radius 2 Refraction is the bending of light when it goes from one medium to another “n” is the index of refraction. c n v Refraction is governed by Snell’s Law: n1 sin 1 n2 sin 2 If we curve the surface and make a lens, we can get the light to concentrate to a point Refracting telescopes use lenses. Objective lens: refracts the light. Aperture: size of the objective lens (larger aperture gathers more light). The objective lens is placed in the aperture.