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<!DOCTYPE HTML PUBLIC "-//W3C//DTD HTML 3.2//EN">
<HTML>
<!-- Mirrored from homepages.cae.wisc.edu/~chinwu/Coastal_Java/groin.html by HTTrack Website Copier/3.x [XR&CO'2014], Wed, 14 Oct 2020 15:22:16 GMT -->
<HEAD>
<TITLE> CACR Evolution at a Groin</TITLE>
</HEAD>
<BODY bgcolor="#C0C0C0">
<img src="cacr.mini.gif" ALIGN="LEFT">
<P><FONT COLOR="#0000FF"><center><FONT SIZE=+4>
Shoreline Evolution at a Groin </center></FONT></P>
<clear "LEFT">
<P>
<HR WIDTH="100%"></P></CENTER>
<CENTER><P><APPLET code= Groin-2.html archive="groin.jar" width=700 height=220> This application requires a Java-enhanced browser to use. Sorry.</APPLET></P></CENTER>
<font color="#000000"><p>
The deposition of sand on the updrift side of a groin and the subsequent (and antisymmetric) erosion of sand on the downdrift side of a groin can be determined analytically from a one-line contour model.
<p>
The magenta region is the shoreline viewed from above. The vertical black line denotes the groin and the horizontal black line in the center is the original shoreline position. <p>
The variable <I> width</I> denotes the width of the figure, and <I>time</I> indicates the elapsed time in days. The <I>Q</I> shows the area accreted (or eroded) with time. To determine the impounded sand volume, multiply this amount by (B+h*), where B is the berm height of the beach and h* is the depth of closure. Finally, <I>xm</I> is the distance from the groin to a location where the shoreline displacement (at bypassing) is one hundredth the length of the groin. This is a measure of the alongshore influence of the groin.
<p>
The animation stops when the groin begins to bypass sand.
<P><FONT COLOR="#FF0000">Comments: <a href="mailto: [email protected]"> Robert Dalrymple</a></FONT>
<br>Center for Applied Coastal Research<br>
University of Delaware, Newark DE 19716<br>USA
</BODY>
<!-- Mirrored from homepages.cae.wisc.edu/~chinwu/Coastal_Java/groin.html by HTTrack Website Copier/3.x [XR&CO'2014], Wed, 14 Oct 2020 15:22:17 GMT -->
</HTML>