Skip to main content Accessibility help
×
Hostname: page-component-78c5997874-v9fdk Total loading time: 0 Render date: 2024-11-05T04:07:22.644Z Has data issue: false hasContentIssue false

4 - Wind, Water, and Waves: Energy from the Fluid Earth

Published online by Cambridge University Press:  05 March 2015

Alan R. Carroll
Affiliation:
University of Wisconsin, Madison
Get access

Summary

The wind goeth toward the south, and turneth about unto the north; it whirleth about continually, and the wind returneth again according to his circuits. All the rivers run into the sea; yet the sea is not full; unto the place from whence the rivers come, thither they return again.

Book of Ecclesiastes, King James version

If you don't like the weather around here, just wait 5 minutes and it will change.

Universally expressed local opinion about all weather, everywhere

Sunlight is abundant, free, and, from the human perspective, eternal. However, as noted in the previous chapter, sunlight is not particularly strong in its natural state, and requires artificial concentration if it is to do any really ambitious work. Fortunately when it comes to concentrating sunlight, nature has already taken the lead. This is true because sunlight causes dramatically unequal heating of the Earth's surface at different latitudes, between land and sea, and between night and day. Uneven heating sets air and water into motion, leading to a complex and sometimes violent sequence of events that act to spread warmth more evenly across the globe. These events never reach an end, however, because the Sun continues to shine and the Earth never stands still. We therefore experience perpetually dynamic weather.

Wind can thus be thought of as solar energy converted into motion. The interaction between wind currents and surface topography help to focus this flow, resulting in localized areas where surface wind speeds exceed the regional average. An opportunity therefore exists for the wind to do real work, if we are somewhat selective about where and when that work is to be done. This is of course no great revelation; wind has propelled sailing ships and turned windmills since the dawn of recorded history. However, wind has also developed a well-deserved reputation for inconstancy. Some days it arrives with a destructive vengeance that precludes any peaceable use; other days it fails to show up at all.

Type
Chapter
Information
Geofuels
Energy and the Earth
, pp. 57 - 79
Publisher: Cambridge University Press
Print publication year: 2015

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Ahrens, C. D., 2007, Meteorology Today: An Introduction to Weather, Climate, and the Environment, 8th ed.: Belmont, CA, Thompon Higher Education, 537 p.Google Scholar
Archer, C. L., and Jacobson, M. Z., 2005, Evaluation of global wind power: Journal of Geophysical Research, v. 110, D12110, DOI:10.1029/2004JD005462.CrossRefGoogle Scholar
Boyle, G. ed., 2004, Renewable Energy: Power for a Sustainable Future: Oxford, Oxford University Press in association with the Open University, 452 p.
Ferrari, R. L., 2001, Lake Meade Sedimentation Survey: U.S. Department of the Interior, Bureau of Reclamation Report, 212 p.
Fonstad, M., Pugatch, W., and Vogt, B., 2003, Kansas is flatter than a pancake: Annals of Improbable Research, May/June, p. 16–18.Google Scholar
Isaacs, J. D., and Schmitt, W. R., 1980, Ocean energy: Forms and prospects: Science, v. 207, p. 265–273.CrossRefGoogle ScholarPubMed
Manwell, J. R., McGowan, J. G., and Rogers, A. L., 2002, Wind Energy Explained: Theory, Design, and Application: Chichester, UK, John Wiley and Sons, 577 p.CrossRefGoogle Scholar
McCully, P., 2001, Silenced Rivers: The Ecology and Politics of Large Dams: London, Zed Books, 359 p.Google Scholar
Syvitski, J. P. M., Vörösmarty, C. J., Kettner, A. J., and Green, P., 2005, Impact of humans on the flux of terrestrial sediment to the global coastal ocean: Science, v. 308, p. 376–380, DOI: 10.1126/science.1109454CrossRefGoogle ScholarPubMed
Vörösmarty, C. J., Meybeck, M., Fekete, B., Sharma, K., Green, P., and Syvitski, J. P. M., 2003, Anthropogenic sediment retention: Major global impact from registered river impoundments: Global and Planetary Change, v. 39, p. 169–190.CrossRefGoogle Scholar

Save book to Kindle

To save this book to your Kindle, first ensure [email protected] is added to your Approved Personal Document E-mail List under your Personal Document Settings on the Manage Your Content and Devices page of your Amazon account. Then enter the ‘name’ part of your Kindle email address below. Find out more about saving to your Kindle.

Note you can select to save to either the @free.kindle.com or @kindle.com variations. ‘@free.kindle.com’ emails are free but can only be saved to your device when it is connected to wi-fi. ‘@kindle.com’ emails can be delivered even when you are not connected to wi-fi, but note that service fees apply.

Find out more about the Kindle Personal Document Service.

Available formats
×

Save book to Dropbox

To save content items to your account, please confirm that you agree to abide by our usage policies. If this is the first time you use this feature, you will be asked to authorise Cambridge Core to connect with your account. Find out more about saving content to Dropbox.

Available formats
×

Save book to Google Drive

To save content items to your account, please confirm that you agree to abide by our usage policies. If this is the first time you use this feature, you will be asked to authorise Cambridge Core to connect with your account. Find out more about saving content to Google Drive.

Available formats
×