2010 Bathymetric Survey and DEM of Corte Madera Bay, California

Metadata also available as

Frequently anticipated questions:


What does this data set describe?

Title: 2010 Bathymetric Survey and DEM of Corte Madera Bay, California
Abstract:
Interpolated 10-m resolution bathymetry collected in Corte Madera Bay in the spring of 2010. Reference Frame = WGS84(G1150) Vertical Datum = WGS84(G1150) all units in meters.
A 1-m resolution BASE surface was created in CARIS using a swath angle weighting scheme where higher weight is given to soundings from the inner part of a swath than to outer beams from adjacent track lines. The 1-m resolution BASE surface was exported from CARIS to an ASCII text file, datum conversions were applied and the data then imported into Fledermaus for interpolation using a cell size of 10 m and weighted moving average gridding algorithm with a weight diameter of 80 m.
  1. How should this data set be cited?

    U.S. Geological Survey (USGS), Pacific Coastal and Marine Science Center (PCMSC), Santa Cruz, CA., 2011, 2010 Bathymetric Survey and DEM of Corte Madera Bay, California: U.S. Geological Survey Open-File Report OF2011-1217.

    Online Links:

  2. What geographic area does the data set cover?

    West_Bounding_Coordinate: -122.504712
    East_Bounding_Coordinate: -122.458596
    North_Bounding_Coordinate: 37.943068
    South_Bounding_Coordinate: 37.905329

  3. What does it look like?

    <http://walrus.wr.usgs.gov/infobank/s/s310sf/html/s-3-10-sf.index.png> (PNG)
    Image showing S-3-10-SF survey tracklines.
    <http://walrus.wr.usgs.gov/infobank/s/s910sf/html/s-9-10-sf.index.png> (PNG)
    Image showing S-9-10-SF survey tracklines.

  4. Does the data set describe conditions during a particular time period?

    Beginning_Date: 26-Jan-2010
    Ending_Date: 30-Mar-2010
    Currentness_Reference: ground condition

  5. What is the general form of this data set?

    Geospatial_Data_Presentation_Form: raster digital data

  6. How does the data set represent geographic features?

    1. How are geographic features stored in the data set?

      This is a raster data set. It contains the following raster data types:

      • Dimensions 417 x 404, type grid cell

    2. What coordinate system is used to represent geographic features?

      Grid_Coordinate_System_Name: Universal Transverse Mercator
      Universal_Transverse_Mercator:
      UTM_Zone_Number: 10
      Transverse_Mercator:
      Scale_Factor_at_Central_Meridian: 0.9996
      Longitude_of_Central_Meridian: -123
      Latitude_of_Projection_Origin: 0.0
      False_Easting: 500000
      False_Northing: 0.0

      Planar coordinates are encoded using row and column
      Abscissae (x-coordinates) are specified to the nearest 10.0
      Ordinates (y-coordinates) are specified to the nearest 10.0
      Planar coordinates are specified in meters

      The horizontal datum used is World Geodetic System 1984 (G1150).
      The ellipsoid used is WGS 84.
      The semi-major axis of the ellipsoid used is 6378137.
      The flattening of the ellipsoid used is 1/298.257.

      Vertical_Coordinate_System_Definition:
      Altitude_System_Definition:
      Altitude_Datum_Name: World Geodetic System 1984 (G1150)
      Altitude_Resolution: 0.01
      Altitude_Distance_Units: meters
      Altitude_Encoding_Method: Attribute values

  7. How does the data set describe geographic features?

    Altitude
    Altitude (elevation) above the WGS84 (G1150) ellipsoid in meters. Values are positive up. (Source: NA)


Who produced the data set?

  1. Who are the originators of the data set? (may include formal authors, digital compilers, and editors)

  2. Who also contributed to the data set?

  3. To whom should users address questions about the data?

    USGS Pacific Coastal and Marine Science Center
    Attn: David P Finlayson
    Operational Geologist
    400 Natural Bridges Drive
    Santa Cruz, CA 95060
    USA

    (831) 427-4757 (voice)
    (831) 427-4748 (FAX)
    dfinlayson@usgs.gov


Why was the data set created?

Bathymetry of Corte Madera Bay collected for use in wave-attenuation studies and sea level rise analyses.


How was the data set created?

  1. From what previous works were the data drawn?

    S-3-10-SF (source 1 of 2)
    U.S. Geological Survey, Coastal and Marine Geology Program, USGS CMG Field Activity S-3-10-SF.

    Online Links:

    Type_of_Source_Media: online
    Source_Contribution:
    This 2010 field activity collected bathymetric data in San Francisco Bay.

    S-9-10-SF (source 2 of 2)
    U.S. Geological Survey, Coastal and Marine Geology Program, USGS CMG Field Activity S-9-10-SF.

    Online Links:

    Type_of_Source_Media: online
    Source_Contribution:
    This 2010 field activity collected bathymetric data in San Francisco Bay.

  2. How were the data generated, processed, and modified?

    Date: 2010 (process 1 of 6)
    Sonar Data Collection
    The bathymetric surveys were conducted using a 234.5 kHz SEA (Systems Engineering & Assessment Ltd) SWATHplus-M phase-differencing sidescan sonar. The sonar was pole-mounted on the 34-foot USGS mapping vessel R/V Parke Snavely, and affixed to a hull brace. Real-time kinematic (RTK) GPS position data were passed through a CodaOctopus F180 intertial measurement unit (IMU) to the sonar hardware and data collection software. Sonar heads, GPS antennae, and the IMU were surveyed in place to a common reference frame with a Geodimeter 640 Total Station. The R/V Snavely was outfitted with three networked workstations and a navigation computer for use by the captain and survey crew for data collection and initial processing.

    Date: 2010 (process 2 of 6)
    Geodetic Control
    Geodetic control for the survey was established using a shore based Global Positioning System (GPS) base station broadcasting Real Time Kinematic (RTK) corrections to the survey vessel via UHF radio link. The base station was located in the hills along Taylor Drive. The base station was programmed using the WGS84 (G1150) reference frame with an Epoch of 2010.1532.
    The base station was programmed using the following coordinates: (see also CM01-base-setup.JPG) Reference Frame: WGS84 (G1150) Epoch: 2010.0630 Latitude: N 37° 54 51.37721 Longitude: W 122° 29 13.21809 Ellipsoid Height: 88.829m
    The average value for the derived OPUS solutions for CM01 are: Reference Frame: ITRF00 [same as WGS84 (G1150)] Epoch: 2010.1532 Latitude: N 37° 54 51.37819 Longitude: W 122° 29 13.21786 Ellipsoid Height: 88.780m
    The differences to be added to the RTK broadcast locations are: Latitude: +0.00098 Longitude: -0.00023 Ellipsoid Height: -0.049m
    Using UTM coordinates as a comparison: The base station was programmed using the following coordinates: Reference Frame: NAD83, UTM zone 10 Epoch: 2002.0000 Northing: 4196426.796m Easting: 545093.600m Ellipsoid Height: 89.359m Orthometric Height: 121.700m (based Geoid09)
    The average value for the derived OPUS solutions for CM01 are: Reference Frame: NAD83, UTM zone 10 Epoch: 2002.0000 Northing: 4196426.825m Easting: 545093.607m Ellipsoid Height: 89.310m Orthometric Height: 121.651m (based Geoid09)
    The differences to be added to the RTK broadcast locations are: Northing: +0.029m Easting: +0.007m Ellipsoid Height: -0.049m Orthometric Height: -0.049m

    Date: 2010 (process 3 of 6)
    Vessel Position and Attitude
    The R/V Snavely was equipped with a CodaOctopus F180 attitude and positioning system for the duration of the survey. The F180 is running F190 firmware, and receives real-time kinematic (RTK) corrections directly. The RTK GPS data (2 cm error ellipse) are combined with the inertial motion measurements directly within the F190 hardware so that high-precision position and attitude corrections are fed in real-time to the sonar acquisition equipment. The WGS84 (G1150) Epoch 2010.1532 3-dimensional reference frame was used for all data acquisition.

    Date: 2010 (process 4 of 6)
    Sound Velocity Measurements
    Sound velocity measurements were collected continuously with an Applied Micro Systems Micro SV deployed on the transducer frame for real-time sound velocity adjustments at the transducer-water interface. The Micro SV is accurate to +/- 0.03 m/s. In addition, sound velocity profiles (SVP) were collected with an Applied Micro Systems, SvPlus 3472. This instrument provides time-of-flight sound-velocity measurements by using invar rods with a sound-velocity accuracy of ±0.06 m/s, pressure measured by a semiconductor bridge strain gauge to an accuracy of 0.15 percent (Full Scale) and temperature measured by thermistor to an accuracy of 0.05 degrees Celsius (Applied Microsystems Ltd., 2005).

    Date: 2010 (process 5 of 6)
    Sonar Sounding Processing
    GPS data and measurements of vessel motion are combined in the F180 hardware to produce a high-precision vessel attitude packet. This packet is transmitted to the Swath Processor acquisition software in real-time and combined with instantaneous sound velocity measurements at the transducer head before each ping. Up to 20 pings per second are transmitted with each ping consisting of 2048 samples per side (port and starboard). The returned samples are projected to the seafloor using a ray-tracing algorithm working with the previously measured sound velocity profiles in SEA Swath Processor (version 3.05.18.04). A series of statistical filters are applied to the raw samples that isolate the seafloor returns from other uninteresting targets in the water column. Finally, the processed data is stored line-by-line in both raw (.sxr) and processed (.sxp) trackline files. Processed (.sxp) files were further processed with sxpegn (build 151) by Amy Foxgrover (USGS) to remove erroneous data from the files and make valid gain-normalized amplitude data for processing backscatter data.

    Date: 20-Mar-2011 (process 6 of 6)
    Digital Elevation Model Production The 1-m resolution BASE surface was created in CARIS using a swath angle weighting scheme where higher weight is given to soundings from the inner part of a swath than to outer beams from adjacent track lines.
    The data was imported into Fledermaus for interpolation to 10-m resolution using a weighted moving average gridding algorithm with a weight diameter of 80 m

  3. What similar or related data should the user be aware of?


How reliable are the data; what problems remain in the data set?

  1. How well have the observations been checked?

    This bathymetric data has not been independently verified for accuracy.

  2. How accurate are the geographic locations?

    Uncertainty in the horizontal position of each sounding is a function of the total uncertainty propagated through each of the following component instruments: 1) base station GPS, 2) vessel GPS, 3) intertial motion unit (IMU), 4) water sound velocity model, and 5) beam spreading in the water column. Assuming no systematic errors in the measurement instruments themselves, beam spreading is the dominate source of positional uncertainty. The 1-degree sonar beam of the SWATHplus-M results in horizontal uncertainty ranging from 0.10 m at 10 m slant range, to about 0.45 m at 50 m slant range.

  3. How accurate are the heights or depths?

    After filtering the data to remove obvious outliers, the standard deviation of the remaining sounding elevations was calculated for each 1 m x 1 m cell (each containing over 400 soundings on average) in CARIS. The mean of the standard deviation for all cells in the Corte Madera survey is 0.06 m and 98% of the cells in the data set have a standard deviation of less than 0.15 m.

  4. Where are the gaps in the data? What is missing?

    Two separate bathymetric surveys of Corte Madera Bay were conducted: the first (USGS Field Activity ID: S-3-10-SF) from January 26 - 29, 2010 and the second (USGS Field Activity ID: S-9-10-SF) on March 29 and 30, 2010. The combined bathymetric surveys consist of 215 survey lines covering an area of approximately 6.5 square km extending north to the dredged ferry channel leading to Corte Madera Creek and to the south, just beyond Paradise Cay Yacht Harbor.

  5. How consistent are the relationships among the observations, including topology?

    All bathymetric values are derived from the same instruments and processing workflow.


How can someone get a copy of the data set?

Are there legal restrictions on access or use of the data?

Access_Constraints:
If physical samples or materials are available, constraints on their on-site access are described in "WR CMG Sample Distribution Policy" at URL: <http://walrus.wr.usgs.gov/infobank/programs/html/main/sample-dist-policy.html>
Use_Constraints:
Not suitable for navigation.
Read and fully comprehend the metadata prior to data use.
Acknowledge the U.S. Geological Survey (USGS), the Originator, when using the data set as a source. Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government.
Share data products developed using the source data set with the Originator.
Data should not be used beyond the limits of the source scale.
This information is not intended for navigational purposes.
The data set is NOT a survey document and should not be utilized as such. Some USGS information accessed through this means may be preliminary in nature and presented without the approval of the Director of the USGS.
This information is provided with the understanding that it is not guaranteed to be correct or complete and conclusions drawn from such information are the responsibility of the user.

  1. Who distributes the data set? (Distributor 1 of 1)

    U.S. Geological Survey, Pacific Coastal and Marine Science Center (PCMSC)
    Attn: David P Finlayson
    400 Natural Bridges Drive
    Santa Cruz, CA 95060-5792
    US

    831-427-4757 (voice)
    831-427-4748 (FAX)
    dfinlayson@usgs.gov

  2. What's the catalog number I need to order this data set?

    Downloadable Data

  3. What legal disclaimers am I supposed to read?

    This information is not intended for navigational purposes.
    Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government.
    Please recognize the U.S. Geological Survey (USGS) as the source of this information. Physical materials are under controlled on-site access. Some USGS information accessed through this means may be preliminary in nature and presented without the approval of the Director of the USGS. This information is provided with the understanding that it is not guaranteed to be correct or complete and conclusions drawn from such information are the responsibility of the user.

  4. How can I download or order the data?


Who wrote the metadata?

Dates:
Last modified: 29-Apr-2011
Metadata author:
Amy Foxgrover
400 Natural Bridges Drive
Santa Cruz, California 95060
USA

831-427-4785 (voice)
afoxgrover@usgs.gov

Hours_of_Service: 9 am to 5 pm Pacific Time (GMT -7)
Metadata standard:
Content Standard for Digital Geospatial Metadata (FGDC-STD-001-1998)


Generated by mp version 2.9.12 on Thu Oct 13 21:20:33 2011