Select the standard so the engine can confirm if your survey configuration meets specification
Enter the project name so the report can identify which project this assessment is associated with.
Enter your name so the report can identify who undertook the assessment.
The project duration is used to compute the tide gauge error arising from the drift rate of the sensor.
Select the Multibeam System
Select the Positioning System
Select the Attitude System
Select the full opening angular sector for the sonar, eg 180 degrees for horizon to horizon, set to 120.5 for 3.5*WD coverage
Select the pings per second rate. Set to -1 for automatic as fast as possible
Select the Swath Coverage, 100% for FULL Bathymetric Coverage, 200% for Full Seafloor Coverage. For Order 1a set to 110%
Select the Minimum Depth for the survey. This is used to bracket the computations.
Select the Maximum Depth for the survey. This is used to bracket the computations.
Vessel speed has a direct impact on data density and feature detection capability.
The Mean SV for water column is used to compute the THU and TVU on outer beams. This only needs to be approximate for the area of operation.
Acceptable SVP error arises from observing SVP in one location and them moving to a different water body, tide cycle.
The maximum operational PITCH impacts most notebly on outer beams for both TVU and THU.
The maximum operational ROLL impacts most notebly on outer beams for both TVU and THU.
The maximum operational HEAVE impacts the entire ping for TVU.
Uncertainy associated with an imperfect patch test affects both THU and TVU.
Uncertainy associated with an imperfect patch test affects both THU and TVU.
How well you have measured the GNSS antenna is important as it creates an error via lever arm computations contributing to both THU and TVU. This uncertainty is applied for Dx, Dy and Dz
The Antenna to MBES offset impacts both TVU and THU. sign does not matter
The Antenna to MBES offset impacts both TVU and THU. sign does not matter
The Antenna to MBES offset impacts both TVU and THU via offset errors. Its always good to minimise these. sign does not matter
The IMU to MBES offset creates lever arm sources of error. Its always good to minimise these.
The IMU to MBES offset creates lever arm sources of error. Its always good to minimise these.
The IMU to MBES offset creates lever arm sources of error. Its always good to minimise these.
Select the Tide reduction source
The tide gauge may settle into the seafloor. You can select the stability of the tide gauge here.
The tide model source of error is based on the estimation of uncertainty from tide zoning.
If harmonic constituents Sa/Ssa, P1, K2,ν2, 2N2 are not included in the harmonic analysis.
Select the Draft Sensor.
The Squat Vs Speed Uncertainty is based how well you have modelled the vessel squat at your calibration phase.
Mean sea level anomaly deals with the effect long term climate events on water levels . They occur at interannual / decadal timescales and even longer term and are more random in nature.
Select the processed GNSS height accuracy. this is a function of receiver, processing and smoothing techniques.
Select the GNSS Antenna to Waterline offset accuracy.
The ellipsoid model source of error is based on the estimation of uncertainty from geoid modelling.
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