Radiation Flashcards

1
Q

Five fundamental components of the Earth system.

A

Biosphere, Geosphere, Atmosphere, Cryosphere, Hydrosphere

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2
Q

Major components of the em spectrum.

A
  • stream of photons each traveling in a wave-like pattern carrying energy in the form of heat
  • wavelength(m), frequency(hz or s-1), and energy(eV)
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3
Q

What is the order of EM spectrum from smallest wavelength to largest? Highest frequency to lowest? Highest energy to lowest?

A

Gamma rays, X-rays, UV, Visible, IR, Microwaves, Radio waves

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4
Q

What is the formula for frequency?

A

f= c (2.9 x 10^-8)/lamda

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5
Q

What is solar flux? What are its units?

A

Amount of energy per unit area per unit time measured perpendicular to the beam (W/m^2)

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6
Q

What physical law describes the manner in which the intensity of sunlight changes as the observer moves away from the Sun?

A

Inverse Square Law
- solar flux decreases as the distance from the sun increases
- S = So(ro/r)^2
where So is solar flux at Earth’s surface
ro is the distance between the earth and the sun
r is the distance between the planet and Earth

  • So is 1370 W/m^2
  • ro is 1AU
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7
Q

What is a blackbody?

A

Emits or absorbs EM radiation with 100% efficiency at all wavelengths

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8
Q

What are the three physical laws that govern blackbody radiation?

A

Planck’s Function (radiation emitted by a blackbody is a function of wavelength; thus hotter bodies emit radiation at short wavelengths)
Wien’s Law (objects of different temperatures emit spectra that peak at different wavelengths)
Stefan-Boltzmann Law (flux emitted by a blackbody is proportional to the fourth power of the body’s absolute temperature)

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9
Q

Wien’s Law equation

A

lamda max = 2898/T

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10
Q

Stefan-Boltzmann Function

A

E = roT^4
where ro is 5.67 x 10^-8 W/m^2/K^4

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11
Q

What are the main differences between the emission spectra of the Sun and the Earth?

A
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12
Q

How does reduced or increased solar luminosity could affect the Earth?

A
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13
Q

How to calculate the effective radiating temperature of planets and of Earth.

A

Te = (S/4ro(1-A))^(1/4)

Earth: Te = (S/4ro(1-A))^(1/4)
where S = 1370 W/m^2
ro = 5.67 x 10^-8 W/m^-2/K^-4
A = 0.3

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