S269 Title Page

S269 Title Page

 

"For my part I consider the Earth very noble and admirable precisely because of the diverse alterations, changes, generations etc. that occur in it incessantly.  If, not being subject to any changes, it were a vast desert of sand..., or if at the time of the flood the waters which covered it had frozen, and it had remained an enormous globe of ice where nothing was ever born or ever altered or changed, I should deem it a useless lump in the universe..."  [Galileo Galilei, quoted in Dava Sobel, Galileo's Daughter]

Observation and Explanation in Science
Origins of Earth and Life
The Dynamic Earth
Atmosphere Earth and Life
Evolving Life and the Earth
The Holocene
TMAs, Advice and Exercises
Other interesting topics
Teasers
Frequently Asked Questions
Notice Board
Feedback
 

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Frequently Asked Questions

These are questions that students have asked, and my replies.  This section will grow as I receive more questions!

Questions Replies
OEL

With reference to the calculation of d13C (OEL p. 57, Equation 3.1), how is the standard ratio of 13C/12C in the inorganic carbon pool determined?

The standard ratio of 13C/12C is set using the ratio in the calcium carbonate in the bullet-shaped tests of belemnites, squid-like cephalopods whose fossils are common in Jurassic rocks (approx. 150 Ma).  [Stephen Drury, Stepping Stones, the making of our home world (Oxford University Press 1999), p. 199]
TDE

With reference to p. 51, how do cyclonic winds create the conditions for upwelling, and anticyclonic winds create the conditions for downwelling.

The reason is partially explained in S269, but is fully explained in S330, Ocean Circulation, p. 59 (Figure 3.23).  The Coriolis force deflects objects, including water, moving over the surface of the Earth.  Deflection is to the right in the Northern Hemisphere.  So in the Northern Hemisphere a low pressure (cyclonic) weather system sets up a stress field on the ocean surface in which water is deflected to the right, i.e. outward from the direction of wind motion.  Outward movement of surface waters creates upwelling.  High pressure (anticyclonic) winds deflect surface water inward (but still to the right), creating the conditions for downwelling.

In the Southern Hemisphere the Coriolis force deflects to the left.  But although the sense of movement is opposite to that in the Northern Hemisphere, low pressure still creates upwelling, and high pressure downwelling.

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S269 Teasers

If you enjoy making your brain hurt (and who would take an OU degree who doesn't?), try to answer the following questions:

In one sentence, can you define what is meant by the "Earth System"?  (Suggestion:  Try this at the beginning of the course, and again at the end.)

 

Is there a "Moon System"?

 

S269 explores the many ways in which geological processes have influenced the evolution of life.  Has the presence of life influenced the way the Earth works?

 

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Notice Board

Tutorial venues and dates 03 March, Bulmershe School, Reading

07 April, Bulmershe School, Reading

12 May, Bulmershe School, Reading

09 June, Bulmershe School, Reading

01  September, Reading College of Arts and Technology

22 September, Bulmershe School, Reading

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Feedback

I welcome your feedback on any aspect of my presentation of S269, including:

Tutorial content
Classroom exercises and style
Marking of assignments
My availability
This website
Anything else you want to say!

Or you can send me feedback about the course itself, and I will forward your comments to the Course Team.

To email your feedback to me, please use the hotlink to my email address below.  Alternatively, you can write to me, or telephone me, or speak to me after tutorials.

Telephone  0118-986-7530
Email address david_scarboro@hotmail.com

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