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2007 Annual Monitoring Report (pdf 16MB) - Bolsa Chica Lowlands ...

2007 Annual Monitoring Report (pdf 16MB) - Bolsa Chica Lowlands ...

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<strong>Bolsa</strong> <strong>Chica</strong> <strong>Lowlands</strong> Restoration <strong>Monitoring</strong><strong>2007</strong> <strong>Annual</strong> <strong>Report</strong><strong>Bolsa</strong> <strong>Chica</strong> State BeachCityof Huntington Beach80249+30311+22318+30333+30350+71378+29423+8970Beach Width Change (m)6050403020100-10-200 1 2 3 4 5 6Alongshore Distance (km)Figure 2-13. <strong>Bolsa</strong> <strong>Chica</strong> <strong>Monitoring</strong> Period Shoreline Changes, October 2005 to October <strong>2007</strong>.Sediment Volume ChangesLong-Term Subaerial Volume Changes (1963 to <strong>2007</strong>): The long-term subaerial volume trends(Appendix 2-D) were similar to the long-term shoreline changes. Volume gains occurred at six ofthe seven <strong>Bolsa</strong> <strong>Chica</strong> area transects during the 44-year period between 1963 and <strong>2007</strong>. Theexception was Transect 378+29, where subaerial volumes were relatively stable during this periodwith no apparent trend. Figure 2-14, which shows the net long-term subaerial volume changesbetween May 1963 and May <strong>2007</strong>, bears a striking resemblance to Figure 2-11 (showing shorelinechanges for the same period).<strong>Bolsa</strong> <strong>Chica</strong> <strong>Monitoring</strong> Period Subaerial Volume Changes (2005 to <strong>2007</strong>): Subaerial volumechanges during the two-year <strong>Bolsa</strong> <strong>Chica</strong> <strong>Monitoring</strong> Period are shown in Figure 2-15. Thevolume changes north of the channel were very similar to the beach width changes. In contrast tothe predominance of shoreline retreat south of the entrance channel, subaerial volume loss occurredat only one transect in this region. This apparent discrepancy at Transect 333+30 (immediatelysouth of the entrance channel) can be explained by the erosion of the beach between the waterlineand the berm (resulting in shoreline retreat) accompanied by stability from the berm to the backbeach (preserving the volume of sand nourishment placed in this area). The volume gains atMerkel & Associates, Inc. 84

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