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:____________________________________ 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 |