the sun Flashcards

1
Q

What’s the solar cycle

A

11 year cycle of the number of sun spots per year. The sun spots have a leading and following magnetic field. the polarity of the leading field (emerging from the surface) is opposite to that of the following field (submerging)

The leading field polarity is opposite in the northern and southern hemispheres. this swaps every cycle so its actually a 22 year cycle

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2
Q

whats the corona

A

the outer atmosphere of the sun. its can be seen during solar eclipses

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3
Q

what’s solar wind

A

a stream of energized charged particles (mostly electrons and protons) it travels at 900 km/s and is 1 million kelvin

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4
Q

what’s PP-1

A

the proton-proton chain one. most of the energy in the sun is produced this way.

  1. two protons –> Deuterium nucleus + positron + neutrino
  2. Deuterium + proton –> Helium-3 nucleus + gamma photon
  3. 2 He-3 nuclei –> Helium-4 nucleus + 2 protons

step 1 takes 10^10 years.
step 2 takes 1 second
step 3 takes 10^6 years

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5
Q

what’s the coulomb barrier

A

the electrostatic repulsion between protons that must be overcome for fusion to occur.

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6
Q

what’s a neutrino oscillation

A

neutrinos have mass so they can change between types (electron-, muon, tau- neutrinos). this results in only seeing 1/3 what is actually emitted from the sun of a given type.

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7
Q

what are the origins of planetary atmospheres

A
  1. The primordial solar nebular (that formed the sun). this is where most of the gas giants atmospheres came from
  2. Outgassing. Volcanoes emit large amounts of gas. this is where most of earths atmosphere comes from
  3. Accretion. asteroids/comets impacting may have brought atmospheric constituents
  4. Life. on Earth, photosynthesis produced lots of oxygen
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8
Q

what’s the optical depth equation

A

I = I₀ e^(-T)
I: intensity
T: optical depth (tau symbol)

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9
Q

what’s the albedo

A

the fraction of incident light that is reflected.

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10
Q

derive the equilibrium temp

A

F = L / 4πd² (incident flux)
Fₐ = (1-w) L / 4πd² (absorbed flux, w: albedo)
Lₚ = πR² * Fₐ

πR² * (1-w)L / 4πd² = 4πR²σT⁴
rearrange for T

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11
Q

equation of hydrostatic equilibrium

A

dp/dr = -Gm(r)ρ(r)/r²

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12
Q

how do some gasses leak away

A

Temperature gives a Maxwell-Boltzmann distribution of the velocities of particles. there is a high-energy tail in which the particles have sufficient energy to escape. when they are gone the rest of the particles re-equilibrate so the high energy tail can leak again

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