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2008 Annual Monitoring Report (pdf 10.9MB) - Bolsa Chica ...

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<strong>Bolsa</strong> <strong>Chica</strong> Lowlands Restoration <strong>Monitoring</strong><br />

<strong>2008</strong> <strong>Annual</strong> <strong>Report</strong><br />

Figure 2-16. Long-Term shorezone volume changes, May 1963 to October <strong>2008</strong><br />

<strong>Bolsa</strong> <strong>Chica</strong> <strong>Monitoring</strong> Period Shorezone Volume Changes (2005 to <strong>2008</strong>): It is not possible to<br />

quantify the shorezone volume changes for the <strong>Bolsa</strong> <strong>Chica</strong> <strong>Monitoring</strong> Period because the October<br />

2005 profile does not extend below the waterline. However, investigation of the time series plots in<br />

Appendix 2-D indicates that a trend of shorezone volume loss has prevailed at each transect between<br />

January 2007 and October <strong>2008</strong>. This may be attributable dispersal of the ebb bar and natural<br />

shoreline erosion between Surfside-Sunset nourishment intervals.<br />

Beach Width Measurement<br />

Time series plots for the beach width measurements obtained at the seven <strong>Bolsa</strong> <strong>Chica</strong> area transects<br />

by Moffatt and Nichol and at three nearby locations by the U.S. Army Corps of Engineers are<br />

presented in Appendices 2-E and 2-F, respectively.<br />

The results of the beach width measurements obtained at the seven <strong>Bolsa</strong> <strong>Chica</strong> area transects are<br />

summarized in Table 2-5. During the two-year period between the January 2007 and December <strong>2008</strong><br />

observations, the MSL beach width decreased at three of the seven sites, increased at three locations,<br />

and was essentially unchanged (3 m or less) at the remaining site. In general, the shoreline tended to<br />

advance north of the entrance channel and retreat to the south. The greatest shoreline advance was<br />

14 m, and occurred north of the entrance channel at Transects 311+22 and 318+30. The greatest<br />

shoreline retreat, 22 m, occurred immediately south of the entrance channel at Transect 333+30, and at<br />

the north end of the study area at Transect 249+30. Shoreline change rates during the two-year period<br />

ranged from -10.9 m/yr at Transect 249+30 to 8.0 m/yr at Transect 318+30.<br />

Merkel & Associates, Inc. 129

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