August 24, C OASTAL D ATA I NFORMATION P ROGRAM C OASTAL D ATA I NFORMATION P ROGRAM present
CDIP was developed with seed money from the California Sea Grant program and the California Department of Boating and Waterways. Mission was to acquire a nearshore wave climatology for the US that would allow coastal practitioners to make more rational design decisions.
CDIP Mission Based at SIO 32 Wave Stations 14 People $2.5M+ / year budget Funded by: CDBW USACE (SCCOOS BEACON ONR…) Develop US nearshore wave climatology for more rational design decisions COASTAL DATA INFORMATION PROGRAM
27 Operational CDIP Stations 23 Directional Wave Buoys 2 Pressure sensor stations 2 Anemometers California, Georgia, Guam, Hawaii, Oregon, Washington Historical Stations (1975-present) 63 Wave Buoys 30 Directional Arrays 36 Surge – Inner Harbor 21 Single Point Pressure California, Georgia, Hawaii, Minnesota, North Carolina, Oregon, Virginia, Washington, Guam Approx 300 GB Data Storage
Net/Phone/ Wireless Modem Data Transmission Datawell Directional Wave Buoy Data Acquisition System Located at Coast Guard, Harbor Master, Marine Exchange offices Scripps Central Computer Facility - 29 Km max distance from shore HF/FM Transmission Data 30 minutes
Central Computer Automated Real-Time Processing Time Domain Quality Control Time Series Frequency Domain STORAGE raw spectral parameters WEB UPDATE Real-Time/Historical Pub/Non-Public NWS Transmission Station Specific Requests Error/Diagnostic Statistics Post Processing Inter-comparison of last 24 hours
CDIP In-House Diagnostics Data Collection Coverage Percentages Pt. Reyes – 91.88% La Jolla – 99.66% Torrey Pines I – 99.09% Torrey Pines O – 99.23% Oceanside – 99.29% Harvest – 94.70% San Pedro – 94.95% Dana Point – 99.47% San Pedro – 94.95% Pt Dume – 95.88% Harvest – 94.70% Pt. Reyes – 91.88% Grays Harbor – 87.56%
MEASUREMENTS 30 min) NOWCASTS FORECASTS MODELS
Modeling Waves Across the Basin Headland shadowing Islandshadowing Diffractioneffects Amplification over shoals Refractive effects Directional wave buoy to initiate model
Northwest Swell West Swell
South Swell San Pedro Harbor
San Diego Harbor Entrance
San Pedro & Long Beach Harbor Entrance 6 Feb 2004 – 1728 PST 31 Jan 2000 – 1257 PST 9 May 2003 – 0645 PST
San Francisco Swell Model
San Diego Harbor Entrance 8 Mar 2002 – 0916 PST
FORECASTS - Local Sea & Swell Prediction Two buoys are used to initialize the model
FORECAST MODELS
Regional Prediction of Wave-Driven Sand Transport Los Angeles County Coastline
Santa Monica Bay Directional Buoy Nearshore Directional wave prediction along the 10m depth contour
END USERS - WAVES COMMERCIAL MARINERS RECREATIONAL MILITARY & GOV
In-Situ ATV & JetSki Surveys: San Onofre and Torrey Pines LIDAR CDIP Wave Buoys SOUTHERN CALIFORNIA BEACH PROCESSES STUDY (SCBPS)
SOUTHERN CALIFORNIA BEACH PROCESSES STUDY SCRIPPS INSTITUTION OF OCEANOGRAPHY UNIVERSITY OF CALIFORNIA, SAN DIEGO Objectives Monitor beach sand levels, cliff erosion, and waves Monitor beach sand levels, cliff erosion, and waves Relate spatial patterns of erosion and wave activity Relate spatial patterns of erosion and wave activity Test and improve erosion models used for management Test and improve erosion models used for management decisions decisions
SOUTHERN CALIFORNIA BEACH PROCESSES STUDY Selected Region Dana Point Dana Point to to Point La Jolla Point La Jolla Length 55 miles Length 55 miles Why this region? Man-made Harbors Lagoons Cliffs
Expanded airborne coastline surveys FY2002 Nourishment site study FY Southern California Beach Processes Study ( ) ( ) Local wave buoys to estimate near-beach wave conditions San Diego Oceanside San Clemente
Southern California Beach Processes Study Seasonal (four per year) Laser “LIDAR” Surveys: Precise surveys of cliffs and beach above the water line
LEUCADIA, CA – FEB 2002
DANA POINT HARBOR LIDAR IMAGE – Sep 2002
END USERS – SAND/EROSION LOCAL GOVERNMENTS COASTAL ENGINEERS Torrey Pines State Beach, 11/23/02
Conversion of measurements to produce useful products.
WEB ACCESS STATS 80,000 VISITORS/DAY 159 WEB SITES LINK DIRECTLY TO CDIP