“THE SUN”
- Presentation by Sanjok Chettri
INTRODUCTION
The Sun is the star at the center of the Solar System. It is a nearly perfect ball of hot plasma, heated to incandescence by nuclear fusion reactions in its core. The Sun radiates this energy mainly as light, ultraviolet, and infrared radiation, and is the most important source of energy for life on Earth.
Surface Temperature : 5,772 K
Radius: 696,340 km
Age: 4.603 billion years
Distance to Earth: 149.6 million km
Mass: 1.989 × 10^30 kg
STRUCTURE OF SUN
“ STRUCTURE & FUSIONS “
TEMPERATURE AND TRANISTION
REGIONS | TEMPERATURE (IN KELVINS) |
Core | 15 Million Kelvin |
Radiative zone | 100,000 Kelvin |
Convection Zone | 100,000 kelvin |
Photosphere (Surface) | 5800 Kelvin |
Chromosphere (Lower Atmosphere) | 10,000 Kelvin |
Corona (Outermost Atmosphere) | 1,000,000 or 1 Million Kelvin |
We can see the Temperature cools down as we move from Core to Surface, and it again increases as we move outwards from the Surface towards Outermost Atmosphere.
Temperature & Compositions of the Sun’s Interior (from Core to Surface)
PHOTOSPHERE
The visible surface of the Sun, the photosphere, is the layer below which the Sun becomes opaque to visible light. Photons produced in this layer escape the Sun through the transparent solar atmosphere above it and become solar radiation, sunlight. The change in opacity is due to the decreasing amount of H− ions, which absorb visible light easily. The photosphere is tens to hundreds of kilometers thick, and is slightly less opaque than air on Earth. Because the upper part of the photosphere is cooler than the lower part, an image of the Sun appears brighter in the center than on the edge or limb of the solar disk, in a phenomenon known as LIMB DARKENING. The photosphere has a particle density of ~1023 m−3. The photosphere is not fully ionized—the extent of ionization is about 3%, leaving almost all of the hydrogen in atomic form.
SOLAR GRAULATION
THE CHROMOSPHERE
The lower region of the Sun's atmosphere is called the chromosphere. It was named after the Greek root chroma (meaning color). The chromosphere appears bright red because the hydrogen in the Sun emits a reddish-colored light at high temperatures. The chromosphere is a thin layer of plasma that lies between the Sun’s Visible surface (the photosphere) and the corona (the Sun’s upper atmosphere). It extends for at least 2,000 km above the surface
SOLAR CORONA
PROMINENCES
IMAGE OF SOLAR PROMINENCE
SUNSPOTS
Sunspots are visible as dark patches on the Sun's photosphere and correspond to concentrations of magnetic field where the convective transport of heat is inhibited from the solar interior to the surface. As a result, sunspots are slightly cooler than the surrounding photosphere, so they appear dark. At a typical solar minimum, few sunspots are visible, and occasionally none can be seen at all. Those that do appear are at high solar latitudes. As the solar cycle progresses towards its maximum, sunspots tend to form closer to the solar equator, a phenomenon known as Sporer’s Law. The largest sunspots can be tens of thousands of kilometers across.
FACULAE
Solar faculae are bright spots in the photosphere that form in the canyons between solar granules, short-lived convection cells several thousand kilometers across that constantly form and dissipate over timescales of several minutes. Faculae are produced by concentrations of magnetic field lines. Strong concentrations of faculae appear in solar activity, with or without sunspots.
Solar Facula (Brighter Zones)
SOLAR FLARES
A solar flare is an intense localized eruption of electromagnetic radiation in the Sun’s atmosphere. Flares occur in active regions and are often, but not always, accompanied by coronal mass ejections, and other solar phenomena. The occurrence of solar flares varies with the 11-year solar cycle.
Solar flares are thought to occur when stored magnetic energy in the Sun's atmosphere accelerates charged particles in the surrounding plasma. This results in the emission of electromagnetic radiation across the electromagnetic spectrum.
SOLAR CYCLE
The solar cycle, also known as the solar magnetic activity cycle, sunspot cycle, or Schwabe cycle, is a nearly periodic 11-year change in the sun's activity measured in terms of variations in the number of observed sunspots on the Sun’s surface. Over the period of a solar cycle, levels of solar radiation and ejection of solar material, the number and size of sunspots, solar flares, and coronal loops all exhibit a synchronized fluctuation from a period of minimal activity to a period of maximal activity and back to a period of minimum activity.
The magnetic field of the Sun flips during each solar cycle, with the flip occurring when the solar cycle is near its maximum. After two solar cycles, the Sun's magnetic field returns to its original state, completing what is known as a Hale cycle.
SOLAR WIND
The corona extends far out into space. From it comes the solar wind that travels through our solar system. The corona's temperature causes its particles to move at very high speeds. These speeds are so high that the particles can escape the Sun's gravity. The Solar winds have speed about 400Km/S or (1 Million Mph)
SOLAR CYCLES OVER THE YEARS
THE SOLAR MAGNETIC FIELDS
It is widely believed that the Sun's magnetic field is generated by electrical currents acting as a magnetic dynamo inside the Sun. These electrical currents are generated by the flow of hot, ionized gases in the Sun's convection zone.
The Sun rotates differentially, that is, different parts of the surface of the Sun rotate at different rates; the rotation period ranges from 27 days near its equator to more than 30 days near its poles. This uneven spin winds up the magnetic field lines of the Sun (as shown to the left). This has the same effect as one winds up a rubber band. As the winding becomes tighter, the field (rubber band) is stressed. This stress leads to the formation of Sunspots, prominences, and an active corona. When the field snaps (locally) to release the tension, flares can result. Eventually after ~ 11 years, the stress causes a global relaxation of the field which also leads to a polarity reversal. The winding process then starts over leading to another relaxation after 11 years with another polarity reversal to return to the Sun to its original state. Sunspots vary on the relaxation time scale while the total cycle seems to be twice this relaxation time.
SUN’S MAGNETIC FIELD LINE
CONCLUSION
BIBLIOGRAPHY�
THANK YOU!