16.05.2015 Views

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

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

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

SHOW MORE
SHOW LESS

Create successful ePaper yourself

Turn your PDF publications into a flip-book with our unique Google optimized e-Paper software.

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

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

surveys, the method provides a cost-effective means to supplement the more accurate MSL beach<br />

widths derived from the semi-annual beach profile survey data.<br />

Results<br />

The beach profile plots are provided in Appendix 2-B. MSL beach widths and sediment volume data<br />

are presented in Appendices 2-C and 2-D, respectively. Appendix 2-E contains the beach width<br />

measurements obtained for the <strong>Bolsa</strong> <strong>Chica</strong> monitoring program, while Appendix 2-F contains those<br />

collected by the U.S. Army Corps of Engineers.<br />

Beach Profile Plots<br />

The <strong>2008</strong> beach profile data were used in conjunction with data from the historical surveys to create<br />

profile plots and compute changes in beach width and sediment volume. The beach profile plots<br />

developed from the survey data are provided in Appendix 2-B. The range on each profile plot<br />

represents the distance in meters seaward of the survey origin measured along the transect alignment.<br />

The elevation is given in meters relative to NAVD88.<br />

Two sets of beach profile plots were generated for each transect. The first set of plots shows all of the<br />

beach profile data available for each transect, while the second set of plots shows only those profiles<br />

obtained in during the three-year period encompassing the end of construction of the <strong>Bolsa</strong> <strong>Chica</strong><br />

Lowlands Restoration Project and the first two years post-construction (October 2005 to October<br />

<strong>2008</strong>). The plots focusing on the recent three-year period also show the envelope of all available<br />

profile data that preceded the opening of the <strong>Bolsa</strong> <strong>Chica</strong> entrance channel in August 2006 (May 1963<br />

to March 2006). These plots also include two panels for each transect - one isolating the nearshore<br />

region of the profile and another displaying the entire profile length.<br />

Mean Sea Level Beach Widths<br />

Mean Sea Level (MSL) beach widths are provided in Appendix 2-C. The beach width was computed<br />

as the horizontal distance, in meters, between the landward edge of the beach sand and the point at<br />

which the beach profile intersected the plane of MSL Datum. In the <strong>Bolsa</strong> <strong>Chica</strong> area, MSL lies 0.79<br />

m above NAVD88. Notwithstanding the use of NAVD88 as the elevation reference for the profile<br />

data, MSL was adopted as the shoreline reference in the belief that it provides a more accurate<br />

indicator of changes in beach configuration.<br />

Sediment Volumes<br />

Sediment volume changes are provided in Appendix 2-D. The volume changes were computed along<br />

each transect for the entire width of the shorezone, and for that portion of the profile located above<br />

MSL (subaerial volume).<br />

The offshore boundary of the control volume for the beach above MSL was placed at the intersection<br />

of the profile and a horizontal line corresponding to the elevation of MSL. The offshore boundary for<br />

the shorezone was placed at the “statistical range of closure”. This parameter represents the distance<br />

seaward of the transect origin, beyond which profile variations are smaller than the accuracy of the<br />

survey technique. As implied by its definition, the statistical range of closure was adopted as the<br />

offshore boundary to separate the signal of true profile change from the noise of survey inaccuracy.<br />

The sea bottom elevation at the range of closure corresponds to the “depth of closure” or the depth at<br />

which sediment transport is not substantially affected by littoral processes.<br />

The statistical range of closure was determined for the five historical transects as part of the CCSTWS-<br />

OC. However, these boundaries were no longer appropriate due to the profile changes that resulted at<br />

Merkel & Associates, Inc. 121

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!