Final Exam - Part II
May 11, 1999
Part I: True/False (5 pts each)
- True
- The variety of climatic zones that one observes on a
mountain are due primarily to differences in temperature and rainfall
amounts.
- False
- Ships logs from the 15th and 16th centuries are used to
reconstruct past climates because of the accuracy of their
meteorological observations.
- True
- Latitude is an important climatic attribute because of
the effect is has on the amount of solar radiation reaching the
Earth's surface.
- True
- The last glacial period occurred during the Cenozoic
Era, the Quaternary Period, and the Pleistocene Epoch.
- True
- Studies reveal that during colder glacial periods,
CO2 levels were lower than during warmer interglacial
periods.
- True
- Climate models predict that if average global
temperatures rise by about 2.5o C, average global
precipitation will increase.
- False
- Dendroclimatology is the study of the accumulation of
rocks and debris carried or deposited by glaciers.
- True
- The holocene epoch began about 10,000 years ago.
- True
- Many scientists believe that the changes in energy
involved in the Milankovitch cycles may not be sufficiently large on
their own to have caused the huge climatic shifts between glacial and
interglacial conditions.
- False
- The Sahara region was much drier than today during the last Ice Age.
- True
- Recent general circulation model studies have suggested
that the warming due to enhanced greenhouse effect is likely to occur
more rapidly over land than the over open seas.
- False
- Seasons are caused by the eccentricity of the Earth's
orbit around the sun and the fact that the Earth is closer to the sun
in summer than the winter.
- False
- The "ITCZ" is near the North Pole.
Part II: Multiple choice questions (5 pts each)
Changes in the Earth's obliquity refer to:
- changes in the shape of the Earth's orbit as it revolves
around the sun
- changes in the tilt of the Earth as it
orbits the sun
- changes in the length of the seasons, especially autumn and
spring
- the precession of the earth on its rotation axis
During the Pleistocene epoch:
- continental glaciers continuously covered large
parts of North America and Europe
- it was much warmer than it is now
- continental glaciers alternately
advanced and retreated over large portions of North
America and Europe
- tropical vegetation was growing over vast regions of the
Central Plains of North America
The Milankovitch Theory proposes that climatic changes are due
to:
- variations in the Earth's orbit as it
travels through space
- volcanic eruptions
- changing levels of CO2 in the Earth's
atmosphere
- particles suspended in the Earth's atmosphere
A rainshadow desert is normally found:
- in the center of a large surface anticyclone
- on the back (western) side of a large thunderstorm
- in polar regions where the air is cold and dry
- in the center of the ITCZ
- on the downwind side of a mountain
range
Oxygen isotope analysis cannot be used to identify
changes in temperature in:
- sea-shells
- ice cores
- ocean floor sediment cores
- rocks and minerals
The end of the last Ice Age promoted the following changes to the
landscape:
- melting of large amounts of ice
- rise of sea level
- prolonged rise of those land areas that had been weighted down
by the masses of ice
- advances of forests to regions with tundra and grassy plains
- all of the above
During the Little Ice Age:
- the climatic optimum occurred
- the Bering land Bridge formed
- alpine glaciers grew in size and
advanced
- continental glaciers covered large portions of North America
- sea level lowered by about 280 ft
A negative feedback mechanism:
- acts to reinforce an initial change
- acts to weaken or oppose and initial
change
- will cause a positive change
- will cause a negative change
Part III: Short Answer (10 pts each)
Name two possible short-term (1-3 years) impacts of explosive volcanic
eruptions on the Earth's climate.
In addition to carbon dioxide, name three other gases that may
contribute to the problem of global warming.
Ice cores from Antarctica and Greenland are a powerful tool for
examining past climates. Name three types of climate information
contained in ice core layers.
Part IV: Longer Answers (20 pts each)
Please answer at least 4 of the following 5 questions. Answers
should be 1 to 3 complete sentences.
Explain the difference between the concepts of weather and
climate.
Explain how the annual growth of trees can be used to
reconstruct past climates.
What climate condition allowed for the migration of human
populations from Asia to North America? Why? (be complete in
your answer).
Between 12,800 and 11,500 years ago a short but
severe cold spell, named the ``Younger Dryas'' event,
occurred. Explain why this event is important to the
understanding of climate variations.
Give two specific examples in which climate fluctuations can
affect human affairs in two of the following four areas:
a) Agriculture, b) species and natural areas, c) water
resources, d) coastal areas.