By James F. Manwell, Jon G. McGowan, Anthony L. Rogers
Wind energy’s bestselling textbook- totally revised.This must-have moment version contains up to date facts, diagrams, illustrations and thorough new fabric on:the basics of wind turbine aerodynamics; wind turbine trying out and modelling; wind turbine layout criteria; offshore wind power; unique goal purposes, corresponding to strength garage and gasoline creation. Fifty extra homework difficulties and a brand new appendix on information processing make this entire variation excellent for engineering students.This ebook deals a whole exam of 1 of the main promising assets of renewable strength and is a brilliant creation to this cross-disciplinary box for training engineers.“provides a wealth of data and is a superb reference publication for individuals drawn to the topic of wind energy.” (IEEE strength & strength journal, November/December 2003)“deserves a spot within the library of each collage and faculty the place renewable power is taught.” (The foreign magazine of electric Engineering schooling, Vol.41, No.2 April 2004)“a very complete and well-organized therapy of the present prestige of wind power.” (Choice, Vol. forty, No. four, December 2002)
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Additional info for Wind Energy Explained: Theory, Design and Application
2001). In addition, this text will refer to wind resource material included in several books devoted to this subject. These include the work of Justus (1978), Hiester and Pennell (1981), and the text of Rohatgi and Nelson (1994). 2 General Characteristics of the Wind Resource In discussing the general characteristics of the wind resource it is important to consider such topics as the global origins of the wind resource, the general characteristics of the wind, and estimates of the wind resource potential.
1 Lapse Rate The lapse rate of the atmosphere is generally defined as the rate of change of temperature with height. As will be shown in the following analysis, it is easier to determine the lapse rate by calculating the change in pressure with height and using conventional thermodynamic relationships. If the atmosphere is approximated as a dry (no water vapor in the mixture) ideal gas, the relationship between a change in pressure and a change in elevation for a fluid element in a gravitational field is given by: dp ¼ Àrg dz ð2:13Þ where p ¼ atmospheric pressure, r ¼ atmospheric density, z ¼ elevation above ground, and g ¼ local gravitational acceleration (assumed constant here).
L. (1994) Power from Wind. Cambridge University Press, Cambridge, UK. Inglis, D. R. (1978) Windpower and Other Energy Options. University of Michigan Press, Ann Arbor. Jacobs, M. L. (1961) Experience with Jacobs wind-driven electric generating plant, 1931–1957. Proc. of the United Nations Conference on New Sources of Energy, 7, 337–339. Johnson, G. L. (1985) Wind Energy Systems. Prentice Hall, Englewood Cliffs, NJ. Le Gourieres, D. (1982) Wind Power Plants. Pergamon Press, Oxford. Marchant, J. (2006) In Search of Lost Time.
Wind Energy Explained: Theory, Design and Application by James F. Manwell, Jon G. McGowan, Anthony L. Rogers