Velocity (example: 60 miles/hour in the negative direction)
Acceleration (example: 10 m/s² downward)
Acceleration
Linear acceleration: when you speed up or slow down along a straight line.
Centripetal acceleration: when you move in a circle (direction of v changes).
Acceleration caused by Earth’s gravity is about 10 m/s² (pointing down). All objects accelerate at this rate as they fall.
Newton’s Laws
1st law of motion (the law of inertia): objects maintain a constant velocity unless acted upon by an outside force.
2nd law of motion: F = ma
3rd law of motion: for every force that acts on one object, an equal yet opposite reaction force is exerted upon another object.
Law of gravity: F = G \frac{m1m2}{r^2}, that is, every mass gravitationally attracts every other mass, but the strength of the gravitational pull decreases as the distance between them grows.
Misconception: There Is No Gravity in Space
THIS IS A FALSE STATEMENT.
The fact that Earth’s gravity keeps the moon in orbit around us proves there is plenty of gravity in space!
Astronauts in orbit experience weightlessness due to the fact that they are falling around the Earth, not due to a lack of gravity.
Tides
Caused by the moon’s gravitational pull being stronger on the near side of the Earth than the far side.
Spring tide: sun and moon work together to enhance the tides.
Neap tide: sun and moon work against each other to decrease the tides.
Angular Momentum
Conserved quantity for a spinning object. That is, momentum cannot be created or destroyed for an object, only transferred to/from another object.
Chapter 5: Light and Matter
Light
Light has both particle-like and wave-like properties.
Waves
Wavelength: distance from max-to-max or min-to-min.
Frequency: how many cycles (max to min to max again) a wave goes through in a given time interval. Measured in hertz (Hz = 1/second).
Wave speed = wavelength x frequency
Wave energy increases with higher frequency
Electromagnetic Spectrum
In order of increasing energy and frequency / decreasing wavelength: radio waves, microwaves, infrared, visible, ultraviolet, x-rays, gamma-rays
Radio waves: low energy, low frequency, long wavelength
Gamma-rays: high energy, high frequency, short wavelength.
All of the above are forms of light; visible light is only special to humans because that’s the part of the spectrum we use to see.
The speed of light is constant in vacuum and nothing can go faster than the speed of light in vacuum. In non-vacuum, light travels more slowly. How much light is slowed down in a transparent material is defined by its index of refraction, n = \frac{c}{v}.
Energy
Mass energy: the energy contained in physical objects.
Kinetic energy: the energy of motion
Thermal energy: the energy of heat
Gravitational potential energy: the energy of objects lifted high above the ground.
Radiant (or radiative) energy: the energy of light
Energy is conserved: it can be transformed into other types or transferred to other objects, but the total amount of energy in the universe is constant.
Wein’s law: hotter objects emit the most intense light (that is, brighter light) at shorter wavelengths and higher frequencies (that is, hotter objects emit more blue light) than cooler objects. However, a hotter object will emit more light at all wavelengths than a cooler one. There’s a formula for this on the equation sheet.
Light/Matter Interactions
Emission (hot matter converts thermal energy into radiant energy)
Absorption (matter absorbs the radiant energy of light and heats up)
Transmission (light passes through matter, like a window). Note that light always refracts (changes speed and direction) when it is transmitted.
Reflection (light “bounces off” of matter, like a mirror)
Spectra
Spectra: split light into its individual wavelengths to create a rainbow band.
Spectrographs (prisms) and diffraction gratings are used to create spectra.
Types of spectra:
Continuous spectra: caused by a hot, dense object.
Emission spectra: caused by a hot gas
Absorption spectra: caused by the light from a hot, dense object passing through a cool gas.
Spectra Tell Us
The chemical composition of an object.
Due to the Doppler Effect:
Blueshift: object is moving toward us
Redshift: object is moving away from us
Spectral line broadening: object is rotating
Matter
Atomic number: # of protons in an atom. Defines the element of the atom.
Atomic mass number: # of protons + neutrons in an element. Defines the isotope of the atom.
Molecules: multiple atoms held together by the attraction of positive and negative electric charges.
Just like light, matter has both wave-like and particle-like properties.
Chapter 6: Telescopes
Curved Lenses
Curved lenses use refraction to gather light rays to a focal point
Human eyes are lens-based. They focus light to the retina. The iris controls how much light is allowed to enter the pupil of the eye and reach the retina.
Digital cameras mimic the structure of the eye in many ways.
Basic Properties of a Telescope
Angular resolution: the ability to see fine detail. Better angular resolution allows smaller angles to be seen.
Larger telescopes have better angular resolution.
Angular resolution can also be improved with Adaptive Optical (AO) systems that compensate for atmospheric blurring (the “twinkle” of stars)
Angular resolution can also be improved with interferometry, in which multiple telescopes work together to produce a single image.
Light gathering area: the ability to collect more light and therefore see fainter objects. Larger telescopes have better light gathering power.
Magnification: the ability to make an image appear larger than normal. This depends on the size of the telescope + the eyepiece used.
Telescopes are either refracting (lens-based) or reflecting (mirror-based). Common reflecting telescope designs include the Cassegrain, Newtonian, and Nasmyth/Coude focus models. (note: you DON’T need to be able to sketch them)
Good Observing Sites
Dark (to minimize light pollution)
High (to minimize atmospheric blurring)
Calm (low winds also minimize atmospheric blurring)
Dry (to reduce cloud cover)
Earth’s Atmosphere vs. the EM Spectrum
Radio, visible, the near-infrared, and the near-ultraviolet can pass through Earth’s atmosphere and reach the ground. Most of the infrared, most of the ultraviolet, gamma-rays, microwaves, and x-rays are absorbed or scattered as they pass through Earth’s atmosphere; we need space telescopes to make observations at these wavelengths.
Famous Non-Visible Light Telescopes
Radio: Arecibo and Greenbank
Infrared: SOFIA and James Webb
Visible and ultraviolet: Hubble
X-rays: Chandra and XMM-Newton
Satellite TV dishes are miniature radio telescopes
Other than light, astronomers observe gravity waves in addition to particles such as neutrinos and cosmic rays.