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Atmosphere Flash Cards

Sammie Bradley Atmosphere and Ocean Science Undergraduate Degree Englisch 145 Karten

Karten in diesem Stapel (145)

  1. 1When was earth formed?4.6 billion years ago
  2. 2How was earth formedCondensation and Accretion of gases and other material
  3. 3How hot was early earth?100 degrees Celsius
  4. 4What was the first atmosphere composed of?Hydrogen and Helium
  5. 5Which factors affect a planets atmospheric composition?Distance from sun
    Size of planet
    Presence of rocks and water
    Gases present
  6. 6What set the composition of earth's second atmosphereMeteorite/extra terrestrial impact
    Volcanic emissions
    Rock weathering
    Balance with oceans
    Chemical reactions
  7. 7When did life first appear?3.5 billion years ago
  8. 8What were early life forms?Extremophiles (Archea)
  9. 9How did extremophiles generate energy?Lithotrophy - pulled energy from inorganic molecules inside the cell
  10. 10How do cyanobacteria exist today?Stromatolites
  11. 11How was oxygen initially createdCyanobacteria produce O2 and Organics
    O2 reacts with lose oxygen
    O3 is formed
  12. 12When did plants first appear?2.1 billion years ago
  13. 13What did the appearance of plants coincide with?A rapid rise in oxygen in the atmosphere
  14. 14What is the composition of today's atmosphere?Nitrogen 78%
    Oxygen 21%
    Argon 1%
  15. 15What is the mass of the atmosphere?5.15 x 10 ^15
  16. 16What are the layers of the atmosphere? List them from ground level upwards.Troposphere
    Stratosphere
    Mesosphere
    Ionosphere
    Thermosphere
    Exosphere
  17. 17What is the function of each atmospheric layer?Troposphere - Weather
    Stratosphere - UV Protection
    Mesosphere - Meteorite protection
    Ionosphere - Northern lights
    Thermosphere - Absorb and reflect heat
    Exosphere - Satellite orbit and transition to space
  18. 18What is the Chapman mechanism?A series of equations describing ozone reactions in clean air
  19. 19What determines the peak level of ozone productionThe availability of light
    The availability of gas molecules
  20. 20How does aurora borealis form?Electrons colliding with gas molecules
  21. 21What is the environmental lapse rate for: - temperate environment - dry environmentsTemperate -6.5/km
    Dry -10/km
  22. 22What's the definition of air pressure?The mass of the air column above
  23. 23What is air pressure at ground level1
  24. 24How do we measure air pressure?Pascals
    (CHAMELEONS!)
  25. 25What causes atmospheric circulation?Heat imbalance
  26. 26Where is: Heat surplus Heat defIcitHeat surplus - Equator
    Heat deficit - Poles
  27. 27What is the tricellular model?A model of the 3 main convection cells responsible for circulating heat around the globe
  28. 28What are the 3 cell main convection cells and their extent?Hadley cell : 0/Equator - 30
    Ferrel cell : 30-60
    Polar cell : 60 - 90/pole
  29. 29What is the ITCZ?Inter tropical convergence zone
    A thick band of storms that fluctuates around the equator
  30. 30What is the jet stream?Current of fast moving air
    In the northern hemisphere
    Over area of strongest surface temp
  31. 31Describe the 4 main climatesPolar
    Temperate
    Desert
    Tropical
  32. 32What can be a physical barrier to atmospheric movement?Mountain ranges
    Vegetation
    Cities
  33. 33What is the average UK windspeed?5m/s
  34. 34How long can it take pollutants to cross continents?A few days
  35. 35What physical evidence do we have of long distance atmospheric transport?Volcanic ash and Sahara dust
  36. 36Which pollution event was April 1986?Chernobyl disaster
  37. 37Which three factors influenced distribution of radioactive particles from the Chernobyl event?- Wind regimes
    - Rainfall
    -Equator barrier to Southern Hemisphere
  38. 38Which pollution event was May 1980?Mount St Helens volcanic eruption
  39. 39What caused such rapid transport of the Mt St Helens eruption debris?Material was ejected 18km upwards during eruption and straight into stratosphere
  40. 40What is a chemical lifetime?The amount of time a chemical can exist in the atmosphere before being physically or chemically removed
  41. 41What is cross equatorial flow and how long does it take?The amount of time taken to cross the equator
    1 year
  42. 42How long does it take to cross the tropopause?Three years
  43. 43Which 2 processes enable pollutants to cross the tropopause?Convective upshot
    Tropopause folding
  44. 44Name the 5 oceansAtlantic
    Pacific
    Indian
    Southern
    Arctic
  45. 45Which hemisphere do we find the: Arctic? Antarctic?Arctic - Northern
    Antarctic - Southern
  46. 46What is the overall trend in Antarctic sea ice?Rapid ice loss in some areas and rapid ice gain in others but overall stability
  47. 47What is the seasonal area change in Antarctic sea ice?3 to 18 million km2
  48. 48What is the overall trend in Arctic sea ice?Steady decline since 1979
  49. 49What is the seasonal area change in Arctic sea ice?6 to 15 million km2
  50. 50What is an ocean gyre?A closed loop of ocean circulation
  51. 51What are the 5 major ocean gyres?North Atlantic
    South Atlantic
    North Pacific
    South Pacific
    Indian Ocean
  52. 52What are the 2 subpolar gyres?- Alaska
    -Greenland
  53. 53How do we describe eastern boundary currents?Wide
    Shallow
    Slow
  54. 54How do we describe western boundary currents?Narrow
    Deep
    Fast
  55. 55What controls boundary currents?Coriolis
    Wind direction
  56. 56What direction are equatorial ocean currents in the northern and southern hemisphere?East to West in Both hemisphere
  57. 57Why is the antarctic circumpolar current, the only current able to totally circulate the globe?Has no land masses in the way
  58. 58What are the parameters of the antarctic circumpolar current?2000 km wide
    4000 km deep
  59. 59What is unique about the Indian Ocean circulation?It can reverse seasonally
  60. 60Why is the global ocean conveyor belt important?- Transports heat
    - Spreads nutrient
    - Connect surface and deep sea
  61. 61What forms the (NADW) North Atlantic deep water?- Cooling of Atlantic waters
    - Brine rejection due to ice formation
  62. 62Why does brine rejection occur?When salt water freezes, the salt cannot fit into the ice structure and so it is expelled during freezing
  63. 63What is the importance of the (AMOC) Atlantic meridional current?Moderating climate in Europe
  64. 64What natural tracers can oceanographers use to track ocean circulation- Chemical composition
    - Temperature
    - Salinity
    - Dissolved oxygen
  65. 65What’s anthropogenic tracers can be used to track ocean circulation?- CFC Ratios
    - 14C spike (from atomic bombs)
  66. 66What are the three distinct vertical layers of the ocean?- Photic zone
    - Bathyal zone
    - Abyssal zone
  67. 67What is pycnocline?A layer in which density rapidly increases with depth
  68. 68What is a halocline?A layer in which salinity rapidly increases with depth
  69. 69Are pycnoclines permanent or temporary?Both
  70. 70What causes ocean mixing?Heat convection
    Surface winds
    Tides
    Biological disturbances (I.e. Whales diving)
  71. 71What is an ocean mass?A defined parcel of ocean water with its own unique temperature and salinity
  72. 72What are the boundaries between water masses called?Fronts
  73. 73Identify two methods used to monitor oceans- Expendable bathythermography (XBT), measure temperature as sinking
    - ARGO Floats, rise to surface very 10 days and record temperature and salinity on way up
  74. 74What is the density of freshwater?1000 kg m^3
  75. 75What is the density of saltwater?1021 - 1070 kg m^3
  76. 76Why is the density of seawater higher?Salt content increases the density
  77. 77What causes variation in seawater density?- Glacial melt
    - Rivine input
    - Evaporation
  78. 78How does temperature influence water density?It controls how packed the molecules are
  79. 79What temperature does maximum density occur at?4 degrees celsius
  80. 80How does salinity affect density?More saline, more dense
  81. 81Which is more saline, the Atlantic or the Pacific?Atlantic
  82. 82How does pressure influence density?Pressure pushes molecules closer together and so increases density
  83. 83What does water density influence?Vertical movement of water
    Water mixing
    Stratification strength
  84. 84What is the significance of convection and subduction in the oceans?It ventilates the deep and shallow ocean
  85. 85What is static stability?A measurement of the tendency of a water column to overturn
  86. 86What symbol do we nominate to water static stability?E
  87. 87What does it tell us if E < 0 E = 0 E > 0E<0 - Unstable
    E = 0 - Neutral
    E>0 - Stable
  88. 88When do we get mixing?When two water parcels of differing properties meet
  89. 89Why can greater property differences make mixing more challengingA stronger difference has strong restrictive force so there is less time to mix before equilibrium is reached.
  90. 90How can turbulence encourage mixing?Increases the frequency of the movement of water
  91. 91What kind of diffusivity was found to be essential for completing the ocean conveyor belt?Diapycnal eddy diffusivities
  92. 92Where is Diapycnal eddy diffusivity typically associated with?Rough bottom topography
  93. 93When does salt fingering occur?Mixing process that occurs when relatively warm, salty water overlies relatively colder, fresher water. It is driven by the fact that heated water diffuses more readily than salty water
  94. 94What are the major ions in seawater?- Chloride
    - Sodium
    - Sulphate
    - Magnesium
    - Calcium
  95. 95Is the ratio of ions in seawater, variable or constant?Constant
  96. 96Why are the major ions always consistent in seawater?The processes that remove/supply these ions are much slower than the rate of ocean circulation
  97. 97What is the average salinity of sea water?35 psu
  98. 98What are and where are the extremes of ocean salinity?LOW - Baltic - 10 psu
    HIGH - Mediterranean- 38 psu
  99. 99Why is the Atlantic more saline than the Pacific?1. Rockies/Andes block the atmospheric freshwater transport
    2. Trade winds are dry from passing over desert so promote greater evaporation
  100. 100Identify 6 factors that control seawater salinity1. Precipitation (Rain/Snow)
    2. River run off
    3. Melting of ice
    4. Groundwater flow to ocean
    5. Freezing of seawater
    6. Evaporation of seawater
  101. 101What are the main factors controlling addition/removal of freshwater?Evaporation and Condensation
  102. 102When Evaporation > Condensation, do we see higher or lower salinity?Higher salinity
  103. 103When Evaporation < Condensation, do we see higher or lower salinity?Lower salinity
  104. 104How will global warming influence the hydrological cycle?Will be intensified, contrasts will become more extreme
  105. 105What is the principle that backs the intensification of the water cycle with global warmingWith every 1 degree rise, 7% more water vapour can be held
  106. 106Where are low salinities frequently observed?River mouths
  107. 107How does ice formation and melt affect salinity?Formation - increases salinity, as salt is expelled during freezing
    Melting - decreases salinity, as adds fresh water back
  108. 108What is the research on the AMOC currently focused on?Whether the freshening from glacial melt in the sub polar Atlantic is wreaking the AMOC
  109. 109How does the freshening of water impact the AMOC?- Alter surface stratification
    - Reduce deep water convection
    - Reduce amount of heat moving northwards
  110. 110Ultimately, what does a weakening of the AMOC mean for Europe?A climate more similar to that of North America (very cold and very wet!)
  111. 111Has the AMOC experienced weakening before?8,200 years
    Collapse of Laurentide ice sheet melt dam at Hudson Bay.
  112. 112What are the proposed causes of AMOC weakening?1. Meltwater from Greenland glaciers
    2. Intensifying sub polar gyre
    3. Increased freshwater from the arctic
  113. 113Why is ocean temperature and heat content of interest?1. Energy budget
    2. Poleward heat transport
    3. Seasonal climate moderation
    4. Impact on ocean biology, chemistry and physics
  114. 114What’s the range of sea surface temperatures?-1.8 degrees to 30 degrees
  115. 115What is the general sea surface temperature pattern?Decreasing towards poles
  116. 116How does temperature change with depth and why?Temperature decreases with depth.
    1. Source of heat at surface
    2. Cool water sinks
  117. 117What is the difference between temperature and heat content?Temperature is the amount of energy of in PARTICLES in a substance
    Heat content is the amount of energy in a SYSTEM
  118. 118How does heat capacity relate to water?Water has a high heat capacity and can absorb large amounts of heat
  119. 119How does the ocean take in heat?Heat is received by the deans through exchanges with the atmosphere and the sea surface
  120. 120What are the Radiative fluxes that influence ocean heat?- Albedo
    - Atmospheric composition
    - Solar elevation
    - Seawater turbidity
  121. 121What are the Turbulent fluxes that influence ocean heat?- Temperature
    - Humidity
    - Wind speed
  122. 122How long has the earth been in radiative imbalance and what does this mean?Since 1970, earth takes in more energy than it expels
  123. 123How much of the excess energy has the ocean absorbed?93%
  124. 124Which is the ocean so effective for heat absorption?- Large mass
    - Low albedo
    - High heat capacity
  125. 125At what rate has ocean temperature risen?0.11 degrees per decade
  126. 126In which hemisphere is warming most extreme?The Northern Hemisphere
  127. 127When was there an ocean warming hiatus?1998
  128. 128What is it believed the ocean warming hiatus could be caused by?- Redistribution of heat in oceans
    - Cyclical changes in solar activity and La Niña
    - Volcanic eruptions reducing solar activity
  129. 129What causes regional variation in ocean warming?- Surface heat fluxes
    - Altered ocean circulation
  130. 130Give two examples of anomalous events in sea surface temperature1. Pacific warm blob (2013-2014)
    2. Atlantic cold blob (2015-2016)
  131. 131How does albedo differ over - Sea ice - Open oceanSea ice - 80% reflection
    Ocean - 10% reflection
  132. 132What are the major impacts of rising ocean temperatures?1. Ice melt
    2. Sea level change
    3. Alter ocean circulation
    4. Impacts on ocean processes
  133. 133How will ocean warming impact dissolved oxygen?1. Increased stratification, limits oxygen to depth
    2. Reduced gas solubility
    3. Increased oxygen demand at higher temperatures
  134. 134What % decrease will we see in oxygen solubility?3-6% Decrease in oxygen
  135. 135By what % are oxygen minimum zone expecting to increase?%10
  136. 136At what depth does wind affect ocean circulation?Down to 150m
  137. 137What angle does the current move in relation to the water?45 degrees
  138. 138What direction is the deflection in each hemisphere?Northern hemisphere - to the right
    Southern hemisphere - to the left
  139. 139What causes deflection of the oceans?The coriolis force?
  140. 140What can Ocean deflection cause?Convergence and Divergence
  141. 141Why does Coriolis affect the oceans?Water isn’t fixed to the surface so it is moved as the earth spins beneath it
  142. 142Why is the Speed of rotation faster at the equator than the poles?Equatorial region has to cover larger distance in the same time as the poles
  143. 143What is the Ekman spiral?A decaying spiral as you move into the ocean. Less power but further deflection moving in depth.
  144. 144How does convergence affect nutrient supply?Increased in pressure, downwelling, increase in sea height, low productivity and reduction in nutrient supply
  145. 145How does divergence affect nutrient supply?Decrease in pressure, upwelling, decrease in height, high productivity and increase in nutrient supply

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Undergraduate Degree Atmosphere and Ocean Science Karteikarten am Atmosphere Flash Cards, erstellt von Sammie Bradley am 24/07/2020.
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