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5 Written questions

5 Matching questions

  1. negative-feedback mechanisms
  2. can you figure out why O18 increases (relative to O16) in the tests of foraminifera during cold intervals, but decreases (relative to O16) during cold intervals in water samples from ice cores?
  3. what is the greenhouse effect?
  4. what is the composition of foraminifera shells (or tests)?
  5. what was the purpose of the Ocean Drilling Program?
  1. a produce results that are the opposite of the initial change and tend to offset it
    ex: the negative effect that increased cloud cover has on the amount of solar energy available to hear the atmosphere
  2. b the atmosphere warms the planet and makes Earth livable; the important role it plays in heating earth's surface is called the greenhouse effect: this energy heats the air and increases the rate at which it radiates energy, both out to space and back; think of short-wave UV coming in, long-wave radiation going back up from the surface as heat, these waves are absorbed by greenhouse gases, including CO2, methane, and others). We are most concerned about CO2 because we are adding it to the atmosphere in the greatest amounts, and it accumulates (does not dissipate for hundreds of years)owards Earth;
  3. c in ice, O18 increases relative to O16 during warm intervals. IN forarms, O18 decreases relative to O16 during warm intervals. Ice cores go back more than 400,000 years and record oxygen isotopes (T), atmospheric CO2 and methane in trapped air bubbles. The O isotope record form forarms "mirrors" that from glacial ice.
  4. d foraminifera is a skeleton made of CaCO3 (same as calcite) oxygen isotope rations depend upon water temp; these tiny, single celled organisms are sensitive to even small fluctuations in temperature; seafloor sedimetns containing fossils such as this are useful recorders of climate change
  5. e ...

5 Multiple choice questions

  1. includes atmosphere, hydrosphere, geosphere, biosphere and cryosphere; these interact and involve exchanges of energy and moisture among the spheres- resulting in temperature and precipitation patterns (climate) around the globe
  2. ...
  3. ...
  4. by analyzing pollen from accurately dated sediments, it is possible to obtain high-resolution records of vegetational changes in an area because pollen and spores are parts of life cycles of many plants and are easily identifiable
  5. tiny, often microscopic, liquid and solid particles that are suspended in the air. Aerosols act directly by reflecting sunlight back to space and indirectly by making clouds "brighter" reflectors

5 True/False questions

  1. how far back can we trace temperature and atmospheric CO2 concentration using ice core data?30% higher than highest level over at least the last 650,000 years

          

  2. how do we know there has been a sharp rise in atmospheric CO2 since the industrial revolution?changes in carbon dioxide and methane are linked to fluctuating temperatures. the cores also include atmospheric fallous such as wind-blown dust, volcanic ash and modern day pollution

          

  3. how are tree rings used to tell us about past climate change?by analyzing pollen from accurately dated sediments, it is possible to obtain high-resolution records of vegetational changes in an area because pollen and spores are parts of life cycles of many plants and are easily identifiable

          

  4. how do we know what the concentration of atmospheric CO2 was during past glacial and interglacial cycles? where do these samples come from?changes in carbon dioxide and methane are linked to fluctuating temperatures. the cores also include atmospheric fallous such as wind-blown dust, volcanic ash and modern day pollution

          

  5. what are other, natural sources of CO2 and aerosols?(1) seafloor sediments- contain remains of organisms that one lived near sea surface; useful recorders of worldwide climate change
    (2) oxygen isotope analysis- based on precise measurement of the ratio bt 2 isotopes of oxygen; O^16 is most common and the heavier O^18: O^18/O^16 ratio in shells of microorganisms- past temperatures
    (3) climate change recorded in glacial ice
    (4) tree rings- archives of environmental history
    (5)fossil pollen, corals, historical data

          

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