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The Sun Chapter 29 Composition of the Sun • spectrograph – device scientists use to break up the sun’s light into a spectrum. • Dark lines form in the spectra of stars when gases in the stars’ outer layers absorb specific wavelengths of the light that passes through the layers. • By studying the spectrum of a star, scientists can determine the amounts of elements that are present in a star’s atmosphere. • Both hydrogen and helium occur in the sun. About 75% of the sun’s mass is hydrogen, and hydrogen and helium together make up about 99% of the sun’s mass. • The sun’s spectrum reveals that the sun contains traces of almost all other chemical elements. Nuclear Fusion • nuclear fusion - the process by which nuclei of small atoms combine to form a new, more massive nucleus; the process releases energy • Nuclear fusion occurs inside the sun. • The energy released during the three steps of nuclear fusion causes the sun to shine and gives the sun its high temperature. Nuclear Fusion • The sun’s energy comes from fusion, and the mass that is lost during fusion becomes energy. • In 1905, Albert Einstein proposed that a small amount of matter yields a large amount of energy. This proposal was part of Einstein’s special theory of relativity. • This theory included the equation: E = mc2 The Core • Careful studies of motions on the sun’s surface have supplied more detail about what is happening inside the sun. • The parts of the sun include: – core – radiative zone – convective zone • At the center of the sun is the core. The core makes up 25% of the sun’s total diameter of 1,390,000 km. The temperature of the core is about 15,000,000 kmºC. • The core is made up entirely of ionized gas, and is 10 times as dense as iron. radiative zone - the zone of the sun’s interior that is between the core and the convective zone and in which energy moves by radiation – surrounds the core. – The temperature of the radiative zone ranges from about 2,000,000ºC to 7,000,000 ºC . – energy moves outward in the form of electromagnetic waves, or radiation. Convective zone - the region of the sun’s interior that is between the radiative zone and the photosphere and in which energy is carried upward by convection – surrounds the radiative zone. The temperature of the convective zone is about 2,000,000ºC. – Energy produced in the core moves through this zone by convection. • Convection is the transfer of energy by moving matter • The sun’s atmosphere surrounds the convective zone of the sun’s core. • Because the sun is made of gases, the term atmosphere refers to the uppermost region of solar gases. • The sun’s atmosphere has three layers: – photosphere – chromosphere – corona photosphere - the visible surface of the sun – means “sphere of light.” – the innermost layer of the sun’s atmosphere. – made of gases that have risen from the convective zone. – the temperature is about 6,000ºC. • Much of the energy given off from the photosphere is in the form of visible light. chromosphere - the thin layer of the sun that is just above the photosphere and that glows a reddish color during eclipses – lies just above the photosphere. – It’s temperature ranges from 4,000°C to 50,000 °C. • The gases of the chromosphere move away from the photosphere, forming narrow jets of hot gas that shoot outward and then fade away within a few minutes. The Sun’s Outer Parts corona - the outermost layer of the sun’s atmosphere – huge region of gas that has a temperature above 1,000,000ºC. • As the corona expands, electrons and ions stream out into space. • These particles make up solar wind, which flows outward from the sun to the rest of the solar system. sunspot - a dark area of the photosphere of the sun that is cooler than the surrounding areas and that has a strong magnetic field. • The movements of gases within the sun’s convective zone and the movements caused by the sun’s rotation produce magnetic fields. • These magnetic fields cause convection to slow in parts of the convective zone. • Slower convection causes a decrease in the amount of gas that is transferring energy from the core of the sun to these regions of the photosphere. • Because less energy is being transferred, these regions of the photosphere are considerably cooler than surrounding regions, and form areas of the sun that appear darker than their surrounding regions. • Observations of sunspots have shown that the sun rotates. • The numbers and positions of sunspots vary in a cycle that lasts about 11 years. • Sunspots initially appear in groups about midway between the sun’s equator and poles. The number of sunspots increases over the next few until it reaches a peak of 100 of more sunspots. • After the peak, the number of sunspots begins to decrease until it reaches a minimum. Sun spots • Other solar activities are affected by the sunspot cycle, such as the solar-activity cycle. • The solar-activity cycle is caused by the changing solar magnetic field. – characterized by increases and decreases in various types of solar activity, including solar ejections. • Solar ejections are events in which the sun emits atomic particles. Biggest Solar Flare on Record prominence - a loop of relatively cool, incandescent gas that extends above the photosphere. • Solar ejections include: – prominences – solar flares – coronal mass ejections • Prominences are huge arches of glowing gases that follow the curved lines of the magnetic force from a region of one magnetic force to a region of the opposite magnetic polarity. Solar Prominence solar flare - an explosive release of energy that comes from the sun and that is associated with magnetic disturbances on the sun’s surface – the most violent of all solar disturbances – release the energy stored in the strong magnetic fields of sunspots. This release can lead to the formation of coronal loops. coronal mass ejection is a part of coronal gas that is thrown into space from the sun • Some of the particles from a solar flare escape into space, increasing the strength of the solar wind. • Particles also escape as coronal mass ejections. The particles in the ejection can cause disturbances to Earth’s magnetic field. • These disturbances have been known to interfere with radio communications, satellites, and even cause blackouts. Solar Flare http://www.nasa.gov/images/content/15 8528main_solarflare_516.jpg Solar flare http://www.nasa.gov/images/conte nt/162169main_Trace_solar_flare _lg.jpg TRACE Solar Flare aurora - colored light produced by charged particles from the solar wind and from the magnetosphere that react with and excite the oxygen and nitrogen of Earth’s upper atmosphere; usually seen in the sky near Earth’s magnetic poles. – are the result of the interaction between the solar wind and Earth’s magnetosphere. – usually seen close to Earth’s magnetic poles because electrically charged particles are guided toward earth’s magnetic poles by Earth’s magnetosphere.