The Sun
The Sun
★ Basic characteristics
The Sun
★ Luminosity: the total amount of energy a star radiates per
second
★ The Sun's luminosity is 4×10²⁶ (400 trillion trillion)
Watts
★ At the distance of the Earth from the Sun, the Sun's light
is being spread out over 2.8x10²³ m²
○ Intensity: I = L/(4πR²) = 1400 W/m²
The Nature of Light
The Inverse Square Law
I = L/(4πR²)
The Sun
★ The Sun from the outside
has some notable features
○ Corona
○ Sun Spots
★ More complex than meets
the eye
The Sun
★ Core
★ Radiative Zone
★ Convective Zone
★ Photosphere
★ Corona
Top Hat Question
The Sun
★ The core is where nuclear
fusion takes place
○ All energy generation
occurs there
The Sun
★ The radiative and convective
zones carry energy outward
○ Radiative: via light
○ Convective: via boiling-like
motions
★ The photosphere is the
apparent surface of the Sun
(what we see)
The Sun
★ The radiative zone is
relatively transparent
★ The cooler, outer convective
zone is completely opaque
★ As a result, energy moves
outward from the core
differently in different
regions
The Sun
★ Radiative heat transfer (Radiation)
The Sun
★ Radiative heat transfer (Radiation)
○ It takes 170,000 years for energy (photons) to randomly pass
from atom to atom via photons and out of the zone
○ High energy X-ray and gamma ray photons from the core tend to
lose energy when scattering
The Sun
★ Convective heat transfer (Convection)
○ Hot, less dense material rises up, then transfers energy to its
surroundings, cooling down and becoming more dense, and then
sinking
The Sun
★ Convective heat transfer (Convection)
○ Convection is much more efficient than radiation
○ Only takes about a week to transport energy from bottom to top
of the convective zone
The Sun
★ Conduction: when heat is transmitted through a substance
when there is a difference of temperature between adjoining
regions
○ No actual flow of material, unlike convection
○ Common form of heat transfer in our lives though it does NOT
occur in the Sun
The Sun
The Sun
Top Hat Question
The Sun
★ Evidence of convective heat
transfer in the Sun
○ Granulation: hotter regions
(about the size of Texas) are
brighter
○ Cooler regions are darker
○ Following Stefan's Law: the
intensity of a fixed area of
ideal thermal emitter rises
quickly with temperature
The Sun
★ Why doesn’t heat transfer work the same way throughout the
Sun?
○ Farther from the core, the temperature goes down
○ As the temperature gets lower, the plasma (gas made of ions)
inside gets more opaque (not see through)
○ Far enough from the center of the Sun, energy can't get anywhere
radiatively
The Sun
★ Due to hydrostatic equilibrium,
if energy can't get out at a
certain place:
1) Temperature goes up
2) Pressure goes up
3) Gravity isn't enough to hold
material in place anymore and
pressure wins
The Sun
★ The temperature of the
photosphere - the outermost
opaque layer is 5800 K
★ Because it is opaque and an
excellent absorber, we can
treat the photosphere like an
ideal thermal emitter
The Sun
★ The photosphere can be
approximated as a blackbody
★ Cooler atoms in outer
layers absorb light at
particular wavelengths
★ This spectrum has
absorption from 67
different elements
The Sun
★ The photosphere can be
approximated as a blackbody
★ Cooler atoms in outer
layers absorb light at
particular wavelengths
★ This spectrum has
absorption from 67
different elements
The Sun
★ The photosphere can be
approximated as a blackbody
★ Cooler atoms in outer
layers absorb light at
particular wavelengths
★ This spectrum has
absorption from 67
different elements
The Sun
★ The spectrum of the Sun
is further modified by
absorption in our
atmosphere when we
observe it from the
surface of Earth
The Sun
★ The Corona
○ >3 million degrees, but
extremely low density
○ Extends to 10 million km
from the Sun
○ Visible during a solar
eclipse
○ Some material flows outward
("solar wind")
The Sun
★ The Corona
○ Traces out the Sun’s
magnetic field
The Sun
★ Density is 150x higher than water
at the Sun’s core
★ Density is 6000x lower than air
at the photosphere
★ This occurs because the Sun is in
Hydrostatic Equilibrium
The Sun
★ Hydrostatic equilibrium:
○ Inward gravitational force must
be balanced by outward pressure
○ Otherwise the Sun would
expand/explode contract/implode
○ Pressure depends on temperature
& density of gas
The Sun
The Sun
★ All of the energy produced in
the core is eventually
transferred all the way to
the surface
★ The light in the radiative
zone is much higher energy
than the light radiated from
the photosphere
The Sun
★ Sun Spots
○ First discovered by Galileo
○ Dark spots come and go,
following the rotation of
the Sun
○ Evidence against the
classical picture of objects
beyond the Earth all being
perfect and unchanging
The Sun
★ The Sun has a powerful magnetic
field running through it
★ Magnetic fields resist being
bent or compressed and interact
with ionized gas
○ The gas will move with the
field, and the field will move
with the gas
The Sun
★ Sunspots come and go,
typically in a few days
★ They are linked in pairs
by the Sun's magnetic
field
The Sun
★ Sunspots appear dark because they
are slightly cooler than their
surroundings: 4500 K vs. 5800 K for
typical photosphere (remember
Stefan’s Law!)
★ Magnetic 'pressure' keeps them from
being squashed, even though they
are cooler than surroundings
The Sun
★ Sunspots originate when magnetic field lines are distorted
by Sun’s varying rotation rate
○ To limit twisting, field bursts out of surface
The Sun
★ We observe an 11-year sunspot cycle, during which sunspot
numbers rise, fall, and then rise again
○ We are near maximum now
★ Every 11 years the Sun's north and South magnetic poles swap
positions!
The Sun
The Sun
The Sun
★ Solar Flares
○ Large explosions on Sun’s surface lasting seconds or minutes
○ Associated with the Sun's magnetic field suddenly adjusting its
configuration
○ Sometimes associated with large outflows of particles (Coronal
Mass Ejections)
The Sun
★ Solar Wind
○ Particles escape the Sun where its magnetic field extends
outward
○ Particles fly out at 400-800 km/sec (900,000 miles per hour)
○ The Sun loses 2 million tons per second this way
■ Only ~.01% of its mass
mass over its lifetime
The Sun
★ Sun-Earth magnetic interactions
The Sun
★ Aurora Borealis
The Sun
★ The Sun is powered by nuclear fusion
○ This is when particles (often nuclei) collide
○ In general: nucleus 1 + nucleus 2 → nucleus 3 + energy
The Sun
★ Atoms and nuclei
○ Atom: a bound state of protons, neutrons and electrons
○ Nucleus: the center of an atom made up of protons and neutrons
○ Bohr model (1913): electrons orbit the nucleus of an atom
○ Modern models say that the electron doesn’t orbit but is in a
cloud of possible locations (quantum mechanics)
The Sun
★ Components of atoms
○ Electrons: light, negatively charged particles
○ Protons: ~2000x more massive than electrons, positively charged
○ Neutrons: about as massive as protons, no electric charge
★ Atoms have an equal # of protons and electrons so they are
neutral (not net charge)
★ Ions/plasma have electrons stripped away due to collisions
and therefore have some net charge
Next Time
★ Wrap up the Sun
○ More on nuclear fusion
○ Observations of the Sun