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- <math>x>r</math>, and <math>-l<x<r</math> so that the body surface is entirely in the an arbitrary continuous function<math>.</math> Our aim is to find the outward normal7 KB (1,145 words) - 03:15, 12 February 2010
- * [[Green Function Methods for Floating Elastic Plates]] ...y [[Squire and Dixon 2000]] and [[Williams and Squire 2002]] using a Green function method applicable to infinitely deep water and they obtained simple express7 KB (1,042 words) - 07:15, 4 April 2009
- Equation (1) is subject to the free edge boundary as a function of arclength <math>s</math> along <math>\partial \Delta</math>;9 KB (1,498 words) - 05:48, 30 October 2012
- <math>x>r</math>, and <math>-l<x<r</math> so that the body surface is entirely in the an arbitrary continuous function<math>.</math> Our aim is to find the outward normal8 KB (1,400 words) - 21:32, 10 February 2010
- This is an generalisation of the [[Dispersion Relation for a Free Surface]], to the case where the surface condition is given by a [[:Category:Floating Elastic Plate|Floating Elastic6 KB (1,064 words) - 09:36, 20 October 2009
- We consider the entire free surface to be occupied by a [[Floating Elastic Plate]] with a single discontinuity = Solution using the [[Free-Surface Green Function for a Floating Elastic Plate]] =22 KB (4,078 words) - 05:36, 10 May 2010
- require the representation of the [[Infinite Depth]], [[Free-Surface Green Function]] immersed surface of body <math>\Delta_j</math>. The source strength distribution8 KB (1,256 words) - 08:20, 19 October 2009
- Denoting the potential at the surface by we introduce the operator <math>\mathbf{G}</math> which maps the surface14 KB (2,229 words) - 00:26, 25 February 2010
- normal derivative of the potential and the potential under the surface of We consider a thin plate, floating on the water surface above a sea bed of41 KB (6,389 words) - 09:22, 20 October 2009
- This results is used to calculate the [[Free-Surface Green Function for a Floating Elastic Plate]]. to show that the function20 KB (3,424 words) - 12:02, 11 December 2009
- one is [[Infinite Array Green Function]] the other is based on appropriate branch of the <math>\arccos</math> function is given by14 KB (2,538 words) - 08:21, 19 October 2009
- Here the ice is treated as a floating material of uniform surface density with no elastic properties nor viscosity. ...de of propagation beneath the raft as compared to that under an open water surface ([[Squire et. al. 1995]]).30 KB (4,556 words) - 10:52, 10 September 2009
- ...roviding a solid barrier between the ocean and atmosphere that hinders the free exchange of heat and moisture between the two. It is also involved in helpi ...reads out across the ocean floor (i.e. away from the poles), rising to the surface because of mixing due to roughness in the sea bed and wind, and returning t36 KB (5,801 words) - 09:39, 10 September 2009