Light is completely reflected back at a boundary between two mediums
Occurs when light meets a less dense medium at an angle of incidence larger than the critical angle
Critical angle:
The angle of incidence which causes the angle of reflection to be 90 degrees
Colour of visible light waves is determined by the wavelength and frequency of the light waves
Colour of visible light with the highest frequency is blue
Colour of visible light with the largest wavelength is red
Specular reflection:
Rays are reflected from a smooth surface in a single direction
Diffuse reflection:
Reflection from a rough surface which causes scattering
Red colour filter works by:
Absorbing all wavelengths of light other than those in the red range of the spectrum
Allowing only red light to pass through the filter
Opaque means not see-through
Colour of an opaque object is governed by:
Different objects reflect different wavelengths of light by different amounts
The wavelengths that are most strongly reflected determine the colour
Wavelengths of light that aren't reflected by an opaque object are absorbed by the object
Object appears white if all wavelengths are reflected by equal amounts
Object appears black if all wavelengths are absorbed
All bodies (objects) emit and absorb infrared radiation
The hotter the object, the more infrared radiation it will emit
The hotter the body, the shorter the wavelength of radiation released (e.g., X rays and gamma rays)
For a body to be at a constant temperature, it needs to emit radiation at the same rate it absorbs it - it needs to radiate at the same average power that it absorbs
Intensity and wavelength distribution of any emission depends on temperature
Intensity is the power transferred per unit area; it is a measure of the energy transferred by a wave
If the average power that an object radiates is less than it absorbs, the temperature of the object will decrease
For a body increasing in temperature, it is absorbing radiation faster than it is emitting it
Factors that affect the temperature of the Earth:
The Earth’s rate of absorption and emission of radiation
The amount of reflection of radiation into space
The Earth’s atmosphere largely absorbs or reflects radiation from the sun, preventing it from reaching Earth. Some radiation, however, is allowed to pass through and warms the earth
Radiation emitted from the Earth is absorbed and re-emitted in all directions by greenhouse gases, resulting in the greenhouse effect which warms the earth
Electromagnetic waves are transverse waves
Electromagnetic waves transfer energy (not matter)
Electromagnetic waves form a continuous spectrum
Order of the electromagnetic spectrum in increasing wavelength:
Gamma
X Ray
UV
Visible
Infrared
Microwaves
Radio
Highest frequency electromagnetic wave: Gamma waves
Highest energy electromagnetic wave: Gamma waves
Properties shared by all electromagnetic waves:
They are all transverse waves
They all travel at the same speed (3x10^8 m/s)
They can travel through a vacuum
Range of frequencies of electromagnetic waves detected by the human eye: 400-700 nanometres
Speeds of EM radiation are the same in a vacuum and in air
When radiation strikes an object, it can be:
Transmitted
Reflected
Absorbed
Radio waves can be produced by oscillations in an electrical circuit
Radio waves can create an alternating current in a circuit by inducing oscillations with the same frequency as the waves themselves
Gamma rays originate from changes in the nuclei of atoms