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THE SUN

THE SUN. The star we see by day. The Sun, Our Star. The Sun is an average star. From the Sun, we base our understanding of all stars in the Universe. No solid surface. Interior Properties. Core = 20 x density of iron Surface = 10,000 x less dense than air Average density = Jupiter

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THE SUN

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  1. THE SUN The star we see by day

  2. The Sun, Our Star • The Sun is an average star. • From the Sun, we base our understanding of all stars in the Universe. • No solid surface.

  3. Interior Properties • Core = 20 x density of iron • Surface = 10,000 x less dense than air • Average density = Jupiter • Core = 15,000,000 K • Surface = 5800 K

  4. Scientific Method • How do we know this stuff? • Three examples: • Fusion in the core (core temperature). • Different zones in interior. • Solar activity and Earth

  5. 1. The Core • Scientific Method: • Observations • Make hypothesis (a model) • Models make predictions • Test predictions • Compare results of predictions with observations • Revise model if necessary.

  6. Testing the Core • Observe Sun’s: • Mass (how?) • Composition (how?) • Radius • Luminosity (total energy output) • Use physics to make a model Sun. • Predict: • Surface temp/density (how do you test?) • Surface Luminosity (how do you test?) • Core temp/density  Fusion Rate  neutrino rate (test?)

  7. Density = 20 x density of Iron Temperature = 15,000,000 K Hydrogen atoms fuse together. Create Helium atoms. In The Core

  8. 2. Helioseismology • Continuous monitoring of Sun. • Ground based observatories • One spacecraft (SOHO) • Surface of the Sun is ‘ringing’ • Sound waves cross the the solar interior and reflect off of the surface (photosphere).

  9. Solar Interior • Core • Only place with fusion • Radiation Zone • Transparent • Convections Zone • Boiling hot

  10. Convection • A pot of boiling water: • Hot material rises. • Cooler material sinks. • The energy from the pot’s hot bottom is physically carried by the convection cells in the water to the surface. • Same for the Sun.

  11. Solar Cross-Section • Progressively smaller convection cells carry the energy towards surface. • See tops of these cells as granules.

  12. The Photosphere • This is the origin of the 5,800 K thermal radiation we see. l = k/T = k/(5800 K)  l = 480 nm (visible light) • This is the light we see. • That’s why we see this as the “surface.”

  13. 3. Solar Activity and Earth • Is there a connection between Solar Activity and Earth’s Climate? • Observation: • Little Ice Age • Maunder Minimum

  14. What is Solar Activity? • Sunspots • Magnetic Fields • Coronal Mass Ejections • Solar Wind • Magnetic Storms • Aurora • Other effects?

  15. 11-year sunspot cycle. • Center – Umbra: 4500 K • Edge – Penumbra: 5500 K • Photosphere: 5800 K Sunspots

  16. Magnetic fields and Sunspots • At kinks, disruption in convection cells. • Sunspots form.

  17. Magnetic fields and Sunspots • Where magnetic fields “pop out” of Sun, form sunspots. • Sunspots come in pairs.

  18. Prominences Hot low density gas = emission lines

  19. Stereo

  20. Corona and Solar Wind • Hot, low density, gas emits the radiation we see as the Corona: 1,000,000 K • Solar Wind: Like steam above our boiling pot of water, the gas ‘evaporates’. • Carries away a million tons of Sun’s mass each second! • Only 0.1% of total Sun’s mass in last 4.6 billion years.

  21. Solar Cycle • Increase in solar wind activity - Coronal Mass Ejections • Increase in Auroral displays on Earth • Increase in disruptions on and around Earth. Courtesy of SOHO/LASCO/EIT consortium.

  22. Aurora • The solar wind passes out through the Solar System. • Consists of electrons, protons and other charged particles stripped from the Sun’s surface. • Magnetic fields herd charged particles into atmosphere at poles. • Charged particles excite electrons in atoms.  Light!

  23. 2003 CME Oklahoma 10/29/2003 Credit: E. Woldt

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