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EOSC 112: The Fluid Earth |
Week 13 |
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EOSC 112 Homepage Announcements Lecture Summaries Lab Assignments Special Topics Course Syllabus Web Contact: Phil Austin Site created with Cheetah. Last updated: Dec 7 2001 |
Wednesday, November 28
Friday, December 1Final review questions/topics:
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Prof. Pedersen:
Earth and Ocean Science 112
Chapter 5, all
Chapter 7, all
Chapter 11 to p. 221
Plus all web-posted text (and figures)
Example Final Exam Questions
Pedersen Section of the Course
The 2-hour exam will consist mostly of a set of questions requiring
paragraph- (or point-form) type answers. Rather than ask for you to
recite memorized facts, the questions will be designed wherever
possible to ask you to apply what you have learned, or to draw
together various pieces of information or concepts to address a
certain problem (for example, we will have some questions jointly
posed by Austin and Pedersen that might relate ocean and atmosphere
interaction). There will also be a collection of key terms which you
will be asked to define. Such a possible list of terms could include
one or more names of famous contributors to marine geological
knowledge (e.g. Milutin Milankovitch, James Croll...) - you should be
aware of their general contributions, as discussed during the course.
With regard to the balance in the exam between the Austin, Harrison
and Pedersen sections of the course, the final will be weighted
proportional to the lecture component from each professor.
Example questions:
1. Explain why the surface waters off the coast of northwest Africa
are colder than the surface waters at the same latitude immediately
east of Florida.
2. Explain why the deep waters in the equatorial Atlantic are cold (1
to 3 degrees C) while the overlying surface waters are 20 to 25
degrees warmer.
3. Why are siliceous oozes found only in certain well-defined belts in
the oceans, whereas carbonate oozes are more widespread?
4. Describe briefly how oxygen isotope measurements in foraminifera
have been used to provide evidence for an astronomical control for
Quaternary ice ages on Earth.
_____________________________
Prof. Harrison:
Read: Chapt 13 and 14 in Thurman - Introduction to Oceanography
1) What are the main features/characteristics of marine phytoplankotn?
Where do they live in the water column and why? What are the 3 major
phytoplankton groups and what are their characteristics? Why do we need to
know both size and numbers of phytoplankton to understand how important a
particular species is to the total phytoplankton biomass?
2) What are zooplankton, holoplankton and meroplankton (give an example of
each)? What is the most dominant group of zooplankton?. Explain why
zooplankton vertically migrate.
3) Why do phytoplankton need accessory pigments?
4) Plot light and nutrients versus depth and explain your graphs
5) Explain how we could get a small phytoplankton bloom in waters that are
usually nutrient-limited.
6) Compare coastal regions with oceanic gyres in terms of nutrients,
phytoplankton and primary productivity.
7) What is geoengineering and what schemes are being proposed and why?
What are the scientific problems associated with these schemes?
__________________________
Prof. Austin
Review all vocabulary and review questions at the end of
Chapters 3 and 4.
Text material covered:
Chapter 2: be able to define and understand equilibrium, positive and
negative feedback, feedback loops.
Chapter 3 (all)
Chapter 4 (all)
Chapter 12: El Nino (244-250)
Web PDF Notes (all)
Labs 1 (parts a and b).
++++++++++++++++++++
Example material from first half not covered on mid-term:
Monsoon/sea-breeze circulations -- what causes them? What do they
have in common? How are they different?
Cloud forcing (low cloud/high cloud)
Feedbacks: water vapor, ice albedo, temperature gradiant/storm track
(chapter 4 critical thinking problem).
From: mid-term -- luminosity, solar constant, annually averaged
insolation
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