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Flashcards

Astronomy Test #3

Olivia Gniadek Astronomy Tertiary Inglês 115 flashcards

Flashcards do conjunto (115)

  1. 1Could you distinguish between Earth and Sun-centered solar system models by observing Venus with a telescope?Yes
    Galileo did this
    Saw the phases
  2. 2Why are the planets closest to the Sun more dense than those farther from the Sun?When formed a temperature gradient was present, more heavier solar material could solidify closer, lighter material wouldn't :. material availability
  3. 3What is the solar wind?charged particles from sun
  4. 4Where do asteroids come from?come from the formation of early solar system
  5. 5If Earth was more reflective (had a higher albedo), what would happen to its temperature?Sunlight would be reflected into space, wouldn't be absorbed therefore earth would be cooler
  6. 6What are the main constituents of Earth's atmosphere?Nitrogen and Oxygen
  7. 7Which of the following is not a characteristic of jovian planets?molten core
    crust
  8. 8How did Ptolemy's model differ from Aristotle's model of the universe?Aristotle perfect circles
    Ptolemy was the deference in epicycles
  9. 9Why are smaller terrestrial bodies such as Mercury or the Moon "geologically dead"?the radioactive decay has decreased to such a degree :. no longer molten (internal structure)
  10. 10At any given time, how many high tides are there on Earth?2 high tides
    one on the moon side of the earth and one one the side facing the sun
  11. 11What are Some of the features of Auroras?Due to magnetic field
    occur in polar regions
    due to solar wind coming in contact with the earth's atmosphere
  12. 12Where do comets come from?Come from Kuiper belt (icy and rocky) or the Oort cloud ((pertubated) kicked out by being closer to Jupiter = rockier)
  13. 13What is the main reason that Venus is warmer than Earth?Runaway greenhouse effect
  14. 14Which of the following planets has the most oxygen in its atmosphere?Earth has most oxygen
  15. 15What are some of the features of Primitive meteorites?Early formation of solar system
    Rocky
  16. 16Jupiter does not have a large metal core like Earth. How can it have a magnetic field?Metallic hydrogen, acts like a metal :. causes magnetic field
  17. 17Why do the lunar highlands have many more craters than the lunar maria?Older
    Maria's formed after large bombardment :. lunar highlands are smoothed out
  18. 18Why do we think Mars was once warmer and wetter?Evidence of water, once had rain
    water flowed on surface
  19. 19How does Io get heated by Jupiter?tidal heating causes massaging effect
  20. 20Asteroids have the following features10s of metres to 100s of kms
    Irregular shapes
  21. 21Which of the following planets has the most dense atmosphereterrestrial: Venus
  22. 22What age does radiometric dating give for Moon rocks and meteorites?4.6 billion years
  23. 23What is the structure of Jupiter like?Core - rocky
    Metallic Hydrogen
    Predominant features
    Clouds
  24. 24Which of the following is not one of Kepler's laws of planetary motion?deferents and epicycles
    select the option that is not these
    1. The orbit of a planet around the sun is an ellipse with the sun at one focus
    2. A line joining a planet and the sun sweeps out equal areas in equal times
    3. The square of an orbital period (P) of the planet is proportional to the cube of the semi-major axis (a) of the orbit
  25. 25Why do we think that the solar system formed from a rotating, collapsing gas cloud that ended up as a disk orbiting the Sun?All the planets orbit the Sun in the same direction
    planets have right characteristics to have formed from a disk of mainly hydrogen around a young, hot Sun
    Observations of Sun agree with the theory of a giant ball of mostly hydrogen generating heat by nuclear fusion in the core.
  26. 26What do we think the composition of the solar nebula was?Hydrogen
    Helium
    Other
    Planets and Sun are made out of these
  27. 27Which bodies show evidence of a substantial atmosphere?Mercury - no
    Venus - yes
    Earth - yes
    Mars - not really
  28. 28What is the main source of the original atmospheres of the terrestrial planets?Volcanic outgassing
    Original Atmospheres
  29. 29What are the most common elements in the atmospheres of the jovian planets?Hydrogen
  30. 30Meteorites come from where?Debris of comets and dust
  31. 31Suppose a comet had a very eccentric orbit that brought it quite close to the Sun at closest approach (perihelion) and beyond Mars when furthest from the Sun (aphelion), but with an average distance of 1 AU. How long would it take to complete an orbit and where would it spend most of its time?1 year
    Further out beyond Mars
  32. 32If there was no greenhouse effect, how would Earth be different?Cooler
  33. 33What is the shape of a planets orbitNearly circular
  34. 34What are terraeHighlands on the moon's surface
  35. 35What happens with the earth and the moons tidal wavesSide closest to the moon attracted stronger -> gives a bulge of water on the near side
    Side farthest from the moon is attracted least -> leaves a bulge of water of the far side
    This gives a double sided tidal bulge
  36. 36What are some other ways that solar wind can make its presence knownComet tails are pushed away from sun
    Heliopause maybe ~100AU away
  37. 37What is the ion tail in a cometIonised atoms from coma
    Accelerated by solar wind; pointed away from sun
    Straight but does exhibit filamentary structure which can change daily
    Bluish colour
    Up to 1AU long
  38. 38What is the scale of the outer regions of the solar system?Planetary System = ~40AU radius
    Heliopause = ~100AU radius
  39. 39Where in the Milky Way are we locatedIn the Orion Spiral Arm
  40. 40How many exoplanets have we found thus farOver 3,498 exoplanets
  41. 41What is the composition of the sun74% Hydrogen
    25% Helium
    1% other
  42. 42What is the direction of rotation of the planetsClockwise apart from Venus which spins backwards and Uranus which spins on its side
  43. 43What is the plane that all planets orbit along called and are all orbits the same?Ecliptic plane
    Planets orbit is almost the same
  44. 44What is the approximate tilt of the planets axis~30 degrees
  45. 45What are the similarities between Venus and MarsSimilar topography
    Similar size
    Formed similarly to earth
  46. 46How long is the rotation period of Jupiter?Similar to the sun, the colourful belts of Jupiter rotate different ways I.e. left, right, left etc.
  47. 47What do the colours on Jupiters surface represent?Different chemicals, temperatures and atmospheric height differences that the chemical clouds are forming under
  48. 48How big is Jupiter's red spot?20,000km x 10,000km
  49. 49What determines a shape of an objectIf an object is warm and cools down slowly, it's gets a round spherical shape
    If an object cools quickly it forms an abnormal shape
  50. 50What are the characteristics of Saturn's moon: TitanRain, clouds and sleet are made out of methane and ethane
    It's cool enough that methane could be a liquid or a gas
    Has liquid hydrocarbons
    It has waves like our oceans do
  51. 51How can we determine the chemical composition of a planetUsing the colour spectrum once sun is behind the planet (concept for exoplanets is the same)
  52. 52What is the density of water on earth in comparison to other planets massEarth's water = 1,000kg/m3
    Mercury = 5x the density of water
    Jupiter = less density of water
    Saturn could float on water, that is if you find an ocean big enough
  53. 53How dense is the asteroid beltThinly spread, if all matter in the asteroid belt was clumped together it would form a small moon. Definitely not like Star Wars
  54. 54Where does solar and cosmic radiation come fromSolar from the sun
    Cosmic from other sources in space
  55. 55Where on earth are the auroras located and what are the aurora areas calledIn the North & South poles
    Northern = Borealis
    Southern = Australis
  56. 56What is the key to Ptolemy's model: the epicycle and the deferentA planet moves in a small circle otherwise known as an epicycle
    The centre of the epicycle moves along a larger circle called a deferent which is approx. centred on earth
  57. 57What are inferior planets and elongationOrbits that are smaller than earth's
    The angle between the sun and a planet as viewed from earth
  58. 58What are superior planets and oppositionOrbits that are larger than earth's
    Planet is in opposition part of the sky to the sun (visible at night)
  59. 59What is an ascending node?The point where'd the planet (moving in it's orbital period) crosses the ecliptic from south to north
  60. 60What is a descending node?The point where the planet crosses the ecliptic from north to south
  61. 61What is the sequence of events from the Big Bang?BIG BANG - H, He, Li, Be,- galaxy formation - nucleosynthesis in stars- new elements - generations of stars - big stars create supernovas - interstellar medium enriched with heavier elements I.e. Fe, C, N, O etc
  62. 62What happens at hotter temperaturesMore isolated atoms I.e. H and Fe
    Ionisation of atoms (if hot enough) e.g. H+ or Fe++
    Plasma - ionised gas/atoms
  63. 63What happens at colder temperaturesAtoms form molecules i.e. H2, NH3, CO, N2, H2O
    Materials solidify I.e. ice, dust and rock
    Form metals, metal oxides, silicates erc
  64. 64What does our galaxy containCentrally located nucleus of millions of stars
    Spiral arms - lanes of interstellar gas, dust and young stars
    Interstellar medium ion between stars
  65. 65What does the interstellar medium containMolecular clouds - cool gas and dust
    Inter cloud gas - region between clouds (less dense and warmer)
    Bubbles of hot gas - due to supernovas
  66. 66What are the characteristics of the giant molecular cloudsWeak magnetic fields
    Different sizes and masses
    Cold temperatures 10-50K
    Mainly molecular hydrogen (H2)
    Perhaps 1% microscopic dust and ice
    Contain small dense regions
  67. 67Case study: Bok Nebula "Barnard 86"Core remnant of a molecular cloud
    410 light-years
    12,500AU
    16K
    2x greater in mass than the sun
    Pressure at boundary = 0.0025nPa
    Clouds like this can form isolated low mass stars
  68. 68Where does most of the mass in our solar system lieIn the sun, angular momentum is in the planets
  69. 69What was the sequence of events in the formation of the solar systemEnriched molecular cloud compression - cloud core of new star system - solar nebula - matter attracted to nebula - Protosun develops - gas, dust, ice form disk - planets established - nebula with small residual rotation - core contracts (200,000AU-50AU) - rotation of nebula increases - nebula flattens out
  70. 70Why are there different types of planets1. Solar nebula had radial temperature gradient
    2. Materials condensed into solids at different temperatures
  71. 71What are the rock forming substancesSilicates, metals etc
    Solid at night temperatures
    Solid nearly everywhere in solar nebula
  72. 72What are the molecular compounds like waterWater, methane and ammonia
    Solid at low temperatures ~100-300K
    Not much solid in the inner solar system
    When solid - called ices
    More ice than silicates
    Hydrogen molecules and helium never solidify in the nebula
  73. 73What are the different temperature gradients in the different zones of the solar nebulaInnermost (terrestrial) warm, 300-1200K
    Metal/ silicate materials solid if not too close to protosun
    Any idea vapourised and not readily accreted
    Intermediate (Jovian) cold, ~50-200K
    Metals, silicates, and ices stable solids
    All available for accretion
    Outer (cometary) colder, <30K
    Metal, silicates, ices stable solids
    Material is too sparse - inhibits planet building
    Rocky/icy planetissimals - comet nuclei (Kuiper Belt)
  74. 74What is the planet building systemAccretion of planetissimals to form planets
    A. 100 planetissimals (~1km size) orbiting the sun
    B. After 30 million simulated years have 22 protoplanets
    C. >100 million years - some well established planets
  75. 75What is the consolidation stageInner zone
    Planet sized ball of metal, oxides and silicates
    Intermediate zone
    Growing planet sized ball of metal compounds, silicates and ices
    Grow larger than earth due to ice
    Planet cools and shrinks
    Outer zone:
    Icy planetissimals (~kms in size) dispersed thinly to accrete efficiently
    Millions of objects
  76. 76What is the cleanup stage1. Radiation pressure
    2. Solar wind
    3. Mopping up of debris by planets
    4. Close encounters with other planets
  77. 77What is earth's internal structureCore:
    0-3500kms
    Ni & Fe
    Mantle:
    Liquid iron alloy outer core
    Solid iron alloy core
    Crust:
    Low density rock
    Floats on mantle
    Thinner under oceans ~10km thick
  78. 78What is mercury's internal structureCore:
    75% of planet (diameter)
    Mantle
    600 km thick
    Small magnetic field - some molten core
  79. 79What is oblatenessMeasure of how much a flattened sphere differed from a perfect sphere
  80. 80What does oblateness depend onSize of planet
    Rotation rate
    Matter planet is formed from
    How the matter is distributed inside the planet
  81. 81What is the system of heating of the planets for rocky bodiesObject (like earth) entirely molten
    Differentiation creates a layered structure
    Heavier material sank to the core
    Lighter material floated to outer layers
    Cooling over time
    Outer layers solidify first
    Larger bodies cool slower than smaller bodies
    Need liquid conducting core
  82. 82What is the internal structure of JupiterCore:
    Rocky inclination I.e. Fe, Ni & Si
    High density
    Liquid metallic hydrogen
    Molecular hydrogen
    Colourful band patterns in the top 100kms
    Low density
    H and He abundant
    Strong magnetic field
  83. 83What is the internal structure of Uranus and NeptuneRocky core
    Mantle compressed water with some ammonia
    Layer of liquid molecular hydrogen and liquid helium with a small amount of methane + clouds above
  84. 84What are the moons physical characteristicsDiameter: 3476 km
    Gravity: ~1/6 earth
    Sidereal period: 27.332days
    Average surface temperatures: 403 K (day) 93 K (night)
    Albedo: ~0.1
    Angular size: ~1/2 degrees
    Average density: 3340 kg/m3
  85. 85What are Maria'sLowlands on the moons surface
  86. 86What are the types of rocks found on the surface of the moonIgneous, meaning that the surface of the moon was once molten.
    Basalt: found in the mare, dark, typical of cooled lava
    Anorthosite: found in the highlands, light colour
  87. 87What is the composition of the moonRegolith: fine powder and rock fragments covering the moon's surface;
  88. 88What is the structure of the moonMare on moons crust
    Crust - solid, brittle, less dense material
    Solid upper mantle
    Non-rigid inner mantle
    Core: iron rich
  89. 89What is the moon doing annuallyReceding from earth at ~ 4cm/yr, this slows the earth's orbit by 0.002 seconds per century
  90. 90What does the height of tides depend onHeight of high tides vary due to the effected of sun's gravity
    Spring (larger)
    Neap (weaker) tides
  91. 91What are planetary surface temperatures due toSolar heating (depends on distance from planet to sun and its albedo)
    The surface temperature of the planet also affects the planets atmosphere
  92. 92What is albedoThe fraction of radiation reflected back into space
    E.g.
    Albedo 1 ~ all radiation reflected
    Albedo 0 ~ no radiation reflected
  93. 93What happens if an object absorbs energy at a higher rate that it can radiate awayIt only gets hotter. As the object gets hotter, it radiates more.
  94. 94What happens if sunlight reaches a planet with no atmosphere vs with an atmosphereNo atmosphere: infrared radiation escapes into space
    Atmosphere: some infrared radiation is absorbed in the atmosphere whilst the rest escapes into space. This causes the planets temperature and atmosphere to rise
  95. 95What are the differences between terrestrial and Jovian planetary atmospheresMinimal (compared to terrestrial planets)
    Implies... less processing of the atmosphere
  96. 96What are the levels in the earth's atmosphere?Troposphere - 0-12km, 80% of atmospheric mass, weather zone, clouds & pollution
    Stratosphere - ~12-50km, ozone region, heating of region
    Mesosphere - 50-80km
    Thermosphere - ~80+km, thin, windiest zone
  97. 97What are the levels in venus' atmosphereLower atmosphere - hot, dense, clear
    Cloud layer - 3 separate levels, lower level most opaque, thin haze exists both above and below cloud layer
    Cloud composition - sulphuric acid droplets, no rain on surface, high temperatures, acid and sulphur based components
  98. 98What are the planetary atmospheres of Uranus and NeptuneUranus - 2% methane (greenish blue), featureless (no water or ammonia), 98% rotation axis tilted, global circulation issue?
    Neptune - more dynamic than Uranus, high clouds, faint belts & zones, internal heating driven
  99. 99What is the source of solar wind and what are its characteristicsThe corona
    Not dense
    Plasma (charged particles) that becomes solar wind
  100. 100What are the characteristics of cosmic raysNon-solar source of radiation in the solar system
    Composition: ~87% protons, ~12% alphas
    Particle numbers are less than a solar flux wind
    Energy of the particles are greater than solar winds
  101. 101What are the characteristics of earth's magnetic shieldShock front: Where the solar wind is slowed to subatomic speeds
    Magnetopause:
    Where the pressure of earth's magnetic field balances the solar wind pressure
  102. 102What are the characteristics of Jupiters magnetosphereHuge: envelops the orbits of several moons
    Solar radiation gets trapped and emits synchrotron radiation at radio wavelengths
    Lower energies - radio
    Higher energies - x-rays
  103. 103What happens with auroras in terms of planets without an atmosphere e.g. VenusSolar wind impacts directly on the upper atmosphere ionising the gas
    Shock region develops where the solar wind is slowed and interacts with the atmosphere
  104. 104What happens with auroras on Mercury and MarsMercury - weaker field 1% that of earth's, similar process to earth but smaller scale, too weak to trap radiation
    Mars - no globular magnetic field but does have some magnetised regions in its crust
  105. 105What are cometsFew kms in diameter
    Irregular shapes
    Loose collection of ices, water, methane, ammonia and carbon dioxide, and rocks
    Low albedo
    Covered in black material
    Crust maybe carbon rich
    As it reaches sun, ice vapourises
    Comet surface emit jets of vapourised material in sunlight
  106. 106What is the coma of a cometDense gas & dust cloud surrounding comet
    Hides nucleus
    10,000,00 - 10,000,000km in diameter
    Gases flow - fuzzy ball appearance
  107. 107What is the hydrogen cloudHuge sphere (10^7km diameter)
    Surrounding coma and nucleus
    Hydrogen seen in UV not visible wavelengths and comes from UV dissociated water molecules
  108. 108What is the dust tail in a cometFine dust particles freed from evaporating nucleus
    ~0.1-1 micrometer in diameter
    Curved smooth shape
    Combo of solar photons 'radiation pressure' and gravity - points away from the sun
    Faint yellowish appearance
  109. 109What forms a meteor showerAs a comets nucleus evaporates it leaves behind a trail of dust and rock fragments in the same orbit, it earth passes through this orbit it's called a meteor shower
  110. 110What is a meteor/oid/iteThe brief flash of light visible where a meteoroid enters the surface
    If it survives and reaches the ground it's called a meteorite
  111. 111What are the three categories of meteoritesStony - 95%
    Iron - 4%
    Stony iron 1%
  112. 112What are the characteristics of stony meteoritesLook like ordinary rocks
    Possible fusion crust
    Difficult to find if weathered
  113. 113What are the characteristics of a stony iron meteoriteEqual amounts of iron and silicates
  114. 114What are the characteristics of iron meteoritesContain 10-20% nickel
    Prior to 2000BC main source of refined iron
    Large nickel iron crystals; only possible if the material cooled slowly
  115. 115What are the characteristics of large asteroidsMolten interior with thin crust similar to terrestrial planets

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Tertiary Astronomy FlashCards sobre Astronomy Test #3, criado por Olivia Gniadek em 20-10-2018.
Criado por
Olivia Gniadek
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