287
Study Name:
Survey Type:
CLDS-1999
Bathymetry
Survey Name:
CLDS-1999 PERIODIC MONITORING Bathymetry
Disposal Site:

CLDS (1995-pres)

Start Date: 9/11/1999 End Date: 9/11/1999 Collector:
SAIC
Process Description The bathymetric data were analyzed using SAIC's Hydrographic Data Analysis System (HDAS),

version 1.03. Raw bathymetric data were imported into HDAS, corrected for sound velocity, and

standardized to mean lower low water using the NOAA observed tides. The bathymetric data were

then used to construct depth models of the surveyed area.
Logical Consistency The precise navigation required for all field operations was provided by the SAIC Integrated

Navigation and Data Acquisition System (IDAS). This system uses a Hewlett-Packard 9920 Series

computer to collect position, depth, and time data for subsequent analysis as well as provide real-
Attribute Accuracy Bathymetric data were collected with the use of SAIC's Portable Integrated Navigation and Survey

System (PINSS). This system utilizes a Toshiba 3200 series computer to provide real-time navigation,

as well as collect position, depth, and time data for later analysis. A Del Norte Trisponder® System

provided positioning data to an accuracy of ±3 m in the horizontal control NAD 27. Shore stations

were established along the Connecticut coast at the known benchmarks of Stratford Point and

Lighthouse Point. An ODOM DF3200 Echotrac® Survey Fathometer with a narrow beam, 208 kHz

transducer measured individual depths to a resolution of 3.0 cm (0.1 ft.). Depth values transmitted to

INDAS were adjusted for transducer depth. The acoustic returns of the fathometer can reliably

detect changes in depth of 20 cm or greater due to the accumulation of errors introduced by the

positioning system, vertical motion of the survey vessel, changes in sound velocity through the
Horizontal Accuracy Differential Global Positioning System (DGPS) data were used in conjunction with PINSS to position

the survey vessel. A Trimble 4000DSi GPS receiver and a Trimble NavBeacon XL differential beacon

receiver provided DGPS positioning data to PINSS in the horizontal control of North American Datum

of 1983 (NAD 83) to an accuracy of ±5 m. The Coast Guard differential beacon broadcasting from

Montauk Point, Long Island, New York, (293 kHz) was utilized for satellite corrections due to its
Vertical Accuracy An ODOM DF3200 Echotrac® Survey Fathometer with a narrow beam, 208 kHz transducer

measured individual depths to a resolution of 3.0 cm (0.1 ft.). Depth values transmitted to INDAS

were adjusted for transducer depth. The acoustic returns of the fathometer can reliably detect

changes in depth of 20 cm or greater due to the accumulation of errors introduced by the positioning

system, vertical motion of the survey vessel, changes in sound velocity through the water column,
Depth Datum Name Mean Lower Low Water (MLLW)
Depth Distance Units centimeters
Use Constraints This data was collected and processed for a specific U.S. Army Corps of Engineers activity and

indicates the general existing conditions at the time of collection. As such, the data are only valid for

their intended use, content, time, and accuracy specifications. The user is responsible for the

results of any application of the data for other than the intended purpose.
Contact Person Tom Fredette, Ph.D. Program Manager, US Army Corps of Engineers, New England District

696 Virgina Road, Concord, MA, 01742-2751, Phone:(978) 318-8291 Fax:(978) 318-8303

thomas.j.fredette@usace.army.mil