WO2020148531A1 - Echo sounder callibration - Google Patents

Echo sounder callibration Download PDF

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Publication number
WO2020148531A1
WO2020148531A1 PCT/GB2020/050075 GB2020050075W WO2020148531A1 WO 2020148531 A1 WO2020148531 A1 WO 2020148531A1 GB 2020050075 W GB2020050075 W GB 2020050075W WO 2020148531 A1 WO2020148531 A1 WO 2020148531A1
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Prior art keywords
depth
echo sounder
location
data
obtaining
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Ceased
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PCT/GB2020/050075
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French (fr)
Inventor
Matthew Neil JOSEPH
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BAE Systems PLC
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BAE Systems PLC
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Classifications

    • GPHYSICS
    • G01MEASURING; TESTING
    • G01SRADIO DIRECTION-FINDING; RADIO NAVIGATION; DETERMINING DISTANCE OR VELOCITY BY USE OF RADIO WAVES; LOCATING OR PRESENCE-DETECTING BY USE OF THE REFLECTION OR RERADIATION OF RADIO WAVES; ANALOGOUS ARRANGEMENTS USING OTHER WAVES
    • G01S15/00Systems using the reflection or reradiation of acoustic waves, e.g. sonar systems
    • G01S15/88Sonar systems specially adapted for specific applications
    • G01S15/93Sonar systems specially adapted for specific applications for anti-collision purposes
    • GPHYSICS
    • G01MEASURING; TESTING
    • G01SRADIO DIRECTION-FINDING; RADIO NAVIGATION; DETERMINING DISTANCE OR VELOCITY BY USE OF RADIO WAVES; LOCATING OR PRESENCE-DETECTING BY USE OF THE REFLECTION OR RERADIATION OF RADIO WAVES; ANALOGOUS ARRANGEMENTS USING OTHER WAVES
    • G01S7/00Details of systems according to groups G01S13/00, G01S15/00, G01S17/00
    • G01S7/52Details of systems according to groups G01S13/00, G01S15/00, G01S17/00 of systems according to group G01S15/00
    • G01S7/52004Means for monitoring or calibrating
    • GPHYSICS
    • G01MEASURING; TESTING
    • G01CMEASURING DISTANCES, LEVELS OR BEARINGS; SURVEYING; NAVIGATION; GYROSCOPIC INSTRUMENTS; PHOTOGRAMMETRY OR VIDEOGRAMMETRY
    • G01C13/00Surveying specially adapted to open water, e.g. sea, lake, river or canal
    • G01C13/008Surveying specially adapted to open water, e.g. sea, lake, river or canal measuring depth of open water
    • GPHYSICS
    • G01MEASURING; TESTING
    • G01SRADIO DIRECTION-FINDING; RADIO NAVIGATION; DETERMINING DISTANCE OR VELOCITY BY USE OF RADIO WAVES; LOCATING OR PRESENCE-DETECTING BY USE OF THE REFLECTION OR RERADIATION OF RADIO WAVES; ANALOGOUS ARRANGEMENTS USING OTHER WAVES
    • G01S15/00Systems using the reflection or reradiation of acoustic waves, e.g. sonar systems
    • G01S15/02Systems using the reflection or reradiation of acoustic waves, e.g. sonar systems using reflection of acoustic waves
    • G01S15/06Systems determining the position data of a target
    • G01S15/08Systems for measuring distance only
    • GPHYSICS
    • G01MEASURING; TESTING
    • G01SRADIO DIRECTION-FINDING; RADIO NAVIGATION; DETERMINING DISTANCE OR VELOCITY BY USE OF RADIO WAVES; LOCATING OR PRESENCE-DETECTING BY USE OF THE REFLECTION OR RERADIATION OF RADIO WAVES; ANALOGOUS ARRANGEMENTS USING OTHER WAVES
    • G01S15/00Systems using the reflection or reradiation of acoustic waves, e.g. sonar systems
    • G01S15/86Combinations of sonar systems with lidar systems; Combinations of sonar systems with systems not using wave reflection
    • GPHYSICS
    • G01MEASURING; TESTING
    • G01SRADIO DIRECTION-FINDING; RADIO NAVIGATION; DETERMINING DISTANCE OR VELOCITY BY USE OF RADIO WAVES; LOCATING OR PRESENCE-DETECTING BY USE OF THE REFLECTION OR RERADIATION OF RADIO WAVES; ANALOGOUS ARRANGEMENTS USING OTHER WAVES
    • G01S15/00Systems using the reflection or reradiation of acoustic waves, e.g. sonar systems
    • G01S15/88Sonar systems specially adapted for specific applications
    • G01S15/89Sonar systems specially adapted for specific applications for mapping or imaging
    • GPHYSICS
    • G01MEASURING; TESTING
    • G01SRADIO DIRECTION-FINDING; RADIO NAVIGATION; DETERMINING DISTANCE OR VELOCITY BY USE OF RADIO WAVES; LOCATING OR PRESENCE-DETECTING BY USE OF THE REFLECTION OR RERADIATION OF RADIO WAVES; ANALOGOUS ARRANGEMENTS USING OTHER WAVES
    • G01S15/00Systems using the reflection or reradiation of acoustic waves, e.g. sonar systems
    • G01S15/87Combinations of sonar systems
    • GPHYSICS
    • G01MEASURING; TESTING
    • G01SRADIO DIRECTION-FINDING; RADIO NAVIGATION; DETERMINING DISTANCE OR VELOCITY BY USE OF RADIO WAVES; LOCATING OR PRESENCE-DETECTING BY USE OF THE REFLECTION OR RERADIATION OF RADIO WAVES; ANALOGOUS ARRANGEMENTS USING OTHER WAVES
    • G01S2205/00Position-fixing by co-ordinating two or more direction or position line determinations; Position-fixing by co-ordinating two or more distance determinations
    • G01S2205/01Position-fixing by co-ordinating two or more direction or position line determinations; Position-fixing by co-ordinating two or more distance determinations specially adapted for specific applications
    • G01S2205/04Nautical

Definitions

  • the present invention relates to a method for calibrating an echo sounder on a marine vessel.
  • Water depth information is critical for marine navigation, and echo sounding is a well-known method of determining the depth of a body of water.
  • Sonar pulses i.e. sound waves
  • the time interval between emission and return of a sonar pulse is measured.
  • the local depth can be calculated.
  • Modern marine vessels, of increasing size, are often equipped with their own echo sounders and need to be able to trust the depth information provided.
  • the present invention provides a method of calibrating an echo sounder device on a marine vessel in order to ensure increased confidence in echo sounding measurements.
  • a method of calibrating an echo sounder on a marine vessel comprises measuring a first water depth using the echo sounder on the marine vessel, obtaining location data for the echo sounder, obtaining a second water depth from another source for a location nearby to the echo sounder, comparing the first depth to the second depth, and carrying out a pre-determ ined action if the measured depth differs from the second depth by more than a pre-determ ined threshold. Calibration and checking of the echo sounder can therefore be carried out whilst the marine vessel is operating at sea, rather than requiring the vessel to be in a port in order to carry out static or physical calibration/checking.
  • the second water depth is obtained from surveyed data for a location closest to the echo sounder. In another example, the second water depth is from a second echo sounder on the same marine vessel. ln one example, obtaining the location data for the echo sounder comprises obtaining location data for the vessel, obtaining orientation data for the vessel, obtaining positional data for the echo sounder on the vessel, and calculating the location data for the echo sounder. This allows for more accurate calibration of the echo sounder.
  • tidal data is taken into account for the location of the echo sounder. This may provide increased accuracy of any calculations between the measured depth and any previously calculated depths.
  • the pre-determ ined threshold is dependent upon the distance between the echo sounder location and the second measured depth location.
  • the pre-determ ined threshold is dynamically updated as more depth data is measured.
  • the draft of the marine vessel is factored into the echo sounder depth measurements.
  • a computing device adapted to carry out a method comprising measuring a first water depth using an echo sounder on a marine vessel, obtaining location data for the echo sounder, obtaining a second water depth from another source for a location nearby to the echo sounder, comparing the first depth to the second depth, and carrying out a pre-determ ined action if the measured depth differs from the second depth by more than a pre-determ ined threshold.
  • Figure 1 is an example of a nautical chart
  • Figure 2 is a side-on schematic view of an example marine vessel
  • Figure 3 is a top-down schematic view of an example marine vessel
  • Figure 4 is an example of results obtained by the present invention.
  • FIG. 5 is a flow chart of an example method according to the invention. DESCRIPTION
  • Figure 1 shows a simplified example of a nautical chart 10 providing a graphical representation of a body of water 30, typically a sea, and adjacent coastal regions 20.
  • the nautical chart 10 shown also includes points 35 indicating previously measured depth data for the water 30.
  • Other sources of marine depth data are also available, such as digital charts, and depth information may be shown in number of ways, e.g. point data or gridded depth information.
  • the present invention provides a method of calibrating (or at least checking) on-board echo sounders to ensure they are working properly.
  • FIG 2 shows an example of a marine vessel 50 on a body of water 40.
  • the marine vessel 50 is equipped with an on-board echo sounder 60.
  • the echo sound 60 emits a sonar pulse into the water 40 from the surface toward the seabed 70 (or floor of the local body of water, e.g. lake).
  • the sound pulse is reflected from the seabed 70 (at point 82), and returns to the surface and is detected by the echo sounder 60.
  • the depth d of the water 40 (i.e. the local distance to the seabed 70) is measured by multiplying the speed of sound in water v SOm , d by half the time t taken for the signal to return to the echo sounder 60 after being emitted: Whilst the approximate speed of sound v so «nd is known to be 1.5 x 10 3 m/s, the speed of sound is affected by, amongst other things pressure (and therefore depth), temperature and salinity. Therefore, for precise depth measurement the exact local speed of sound must also be measured, for example by deploying a sound velocity probe info the water.
  • the location of the echo sounder 60 In order to calibrate the echo sounder 60, and ensure it is working correctly, the location of the echo sounder must be obtained, so that the measured depths can be compared to previously recorded depths for the same, or nearby, location.
  • Modern marine vessels are often equipped with electrical navigation equipment, such as Global Positioning System (GPS) receivers. These provide accurate geolocation data to the marine vessel, allowing the operators to identify their exact location.
  • GPS Global Positioning System
  • the location of the echo sounder 60 is considered to be the same as the location of the marine vessel 50 upon which it is carried.
  • a second water depth measurement for that location is obtained.
  • This second depth measurement may come from any source, including nautical chart information (digital or traditional), a second echo sounder (not shown) located on the same vessel, or echo sounder measurements from a nearby other vessel.
  • the method may also involve comparing the echo sounder depth measurement to multiple other local measurements.
  • the second depth measurement is obtained by locating the nearest previously charted depth to the location of the echo sounder 60, shown at depth point 84.
  • the second depth measurement (at point 84) is compared to the first water depth (at point 82) measured by the echo sounder 60 on the marine vessel 50 and the difference 86 is calculated. If the value of the difference 86 is greater than a predetermined threshold, a pre determined action is carried out.
  • the action may take any form, such as logging/flagging the measured depth as outlying from the predetermined tolerance, alerting a user directly, or perhaps automatically adjusting the echo sounder.
  • the distance between the first 82 and second 84 points of depth measurement is also recorded.
  • the benefits of carrying out“on-the-go” echo sounder calibration mean that any results can be checked whilst the marine vessel is operating at sea, rather than requiring the vessel to be in a port in order to carry out static or physical calibration. This means the reliability and confidence in the echo sounder results can be maintained and/or improved during use, and any errors or problems can be identified (and possibly addressed) immediately, instead of remaining undetected until the vessel is next in port for inspection.
  • Figure 3 shows a top-down view of the marine vessel 50 as seen in Figure 2.
  • the location of the marine vessel 50 is calculated by a GPS receiver (or other location device) at point A.
  • the echo sounder 60 is located at point B on the vessel 50, a known distance A-B (and direction) from point A.
  • the accurate location B of the echo sounder 60 can be calculated.
  • the more-accurate location data for the echo sounder 60 is used to determine the nearest previously measured depth point C which may not be the same as the closest depth point to the (nominal) location A of the vessel 50.
  • the distance B-C between the echo sounder 60 (at point B) and previously measured depth (at point C) is also recorded.
  • the location of the marine vessel 50 (or the echo sounder 60) is used to obtain local tidal information.
  • the echo sounder 60 can be more accurately calibrated since the difference between the two measured depths can be adjusted to take the difference in tide heights into account.
  • the second water depth is obtained from a previously surveyed data point closest to the echo sounder location.
  • the second depth measurement may be obtained from a second echo sounder located on the same vessel. The positions of both echo sounders (and the distance between them) is known and therefore a pre- determined threshold for any difference in their readings can be determined.
  • the second depth measurement is provided from an echo sounder located on a second marine vessel whose position is known at the time of the second depth measurement.
  • multiple vessels taking echo sounder measurements in a relatively close proximity to each other may share the depth measurements to cross-calibrate the multiple echo sounders.
  • the pre-determ ined threshold is dependent upon the distance between the first (echo sounder) location and the second measured depth location.
  • Figure 4 shows a graph comprising example results from echo sounder measurements; plotting the difference between the first (i.e. echo sounder) and second measurements against the distance between the two measurement locations.
  • a tolerance or threshold line is shown for both positive and negative difference values, and the tolerance increases as the distance B-C between the between the first (echo sounder) location and the second measured depth location increases.
  • Figure 5 shows a flow chart of a method according to the present invention.
  • a first water depth is measured using an echo sounder on a marine vessel.
  • location data for the echo sounder is obtained.
  • a second (previously measured) water depth for a location nearby to the echo sounder is obtained.
  • the first and second water depth measurement values are compared.
  • a pre-determ ined action is carried out (e.g. alerting a user, or flagging the reading as an outlier) if the first measured depth differs from the second depth by more than a pre-determ ined amount.
  • Steps S1 , S2 and S3 may be carried out in any order, or indeed at the same time.
  • the pre-determ ined threshold is dynamically updated as more depth data is measured. Therefore, as the echo sounder 60 records more depth measurements, and compares them to previously measured depths, a more accurate (i.e. tighter) error profile can be calculated.
  • the draft of the marine vessel 50 i.e. how low the marine vessel sits in the water
  • the marine vessel 50 may sit lower in the water, and any depth measurement should take this into account.
  • a computer device is adapted to carry out the method steps described by the present invention.

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  • Engineering & Computer Science (AREA)
  • Radar, Positioning & Navigation (AREA)
  • Remote Sensing (AREA)
  • Physics & Mathematics (AREA)
  • General Physics & Mathematics (AREA)
  • Computer Networks & Wireless Communication (AREA)
  • Acoustics & Sound (AREA)
  • Life Sciences & Earth Sciences (AREA)
  • Hydrology & Water Resources (AREA)
  • Measurement Of Velocity Or Position Using Acoustic Or Ultrasonic Waves (AREA)

Abstract

The present invention relates to a method of calibrating an echo sounder on a marine vessel. The method comprises measuring a first water depth using an echo sounder on a marine vessel, obtaining location data for the echo sounder, obtaining a second, previously measured, water depth from another source for a location nearby to the echo sounder, comparing the first depth to the second depth, and carrying out a pre-determined action if the measured depth differs from the second depth by more than a pre-determined threshold.

Description

ECHO SOUNDER CALIBRATION
The present invention relates to a method for calibrating an echo sounder on a marine vessel. BACKGROUND
Water depth information is critical for marine navigation, and echo sounding is a well-known method of determining the depth of a body of water. Sonar pulses (i.e. sound waves) are transmitted downwards into the water from the surface, and the time interval between emission and return of a sonar pulse is measured. By knowing the speed of sound through the water, and the time taken for the sonar pulse to return to the surface, the local depth can be calculated. Modern marine vessels, of increasing size, are often equipped with their own echo sounders and need to be able to trust the depth information provided. The present invention provides a method of calibrating an echo sounder device on a marine vessel in order to ensure increased confidence in echo sounding measurements.
SUMMARY OF INVENTION
According to a first example, there is provided a method of calibrating an echo sounder on a marine vessel. The method comprises measuring a first water depth using the echo sounder on the marine vessel, obtaining location data for the echo sounder, obtaining a second water depth from another source for a location nearby to the echo sounder, comparing the first depth to the second depth, and carrying out a pre-determ ined action if the measured depth differs from the second depth by more than a pre-determ ined threshold. Calibration and checking of the echo sounder can therefore be carried out whilst the marine vessel is operating at sea, rather than requiring the vessel to be in a port in order to carry out static or physical calibration/checking.
In one example, the second water depth is obtained from surveyed data for a location closest to the echo sounder. In another example, the second water depth is from a second echo sounder on the same marine vessel. ln one example, obtaining the location data for the echo sounder comprises obtaining location data for the vessel, obtaining orientation data for the vessel, obtaining positional data for the echo sounder on the vessel, and calculating the location data for the echo sounder. This allows for more accurate calibration of the echo sounder.
In another example, tidal data is taken into account for the location of the echo sounder. This may provide increased accuracy of any calculations between the measured depth and any previously calculated depths.
In another example, the pre-determ ined threshold is dependent upon the distance between the echo sounder location and the second measured depth location.
In another example, the pre-determ ined threshold is dynamically updated as more depth data is measured.
In another example, the draft of the marine vessel is factored into the echo sounder depth measurements.
In another example of the invention, there is provided a computing device adapted to carry out a method comprising measuring a first water depth using an echo sounder on a marine vessel, obtaining location data for the echo sounder, obtaining a second water depth from another source for a location nearby to the echo sounder, comparing the first depth to the second depth, and carrying out a pre-determ ined action if the measured depth differs from the second depth by more than a pre-determ ined threshold.
FIGURES
The present invention will now be described, by way of example only, with reference to the accompanying drawings, in which:
Figure 1 is an example of a nautical chart;
Figure 2 is a side-on schematic view of an example marine vessel;
Figure 3 is a top-down schematic view of an example marine vessel;
Figure 4 is an example of results obtained by the present invention; and
Figure 5 is a flow chart of an example method according to the invention. DESCRIPTION
Careful navigation by marine vessels through shallow waters is required in order to avoid running aground; stranding the vessel and possibly causing damage. Nautical charts have been historically fundamental tools for marine navigation, and many countries require marine vessels, especially commercial ships, to carry them on-board when traversing territorial waters in their region.
Figure 1 shows a simplified example of a nautical chart 10 providing a graphical representation of a body of water 30, typically a sea, and adjacent coastal regions 20. The nautical chart 10 shown also includes points 35 indicating previously measured depth data for the water 30. Other sources of marine depth data are also available, such as digital charts, and depth information may be shown in number of ways, e.g. point data or gridded depth information.
However, the nature of a waterway (e.g. the coastline or depth values) depicted by a chart 10 (or other source of marine depth information) may change over time, and old or uncorrected charts increase the risk of a marine vessel running aground whilst traversing the waters. Therefore, most modern large vessels, for example commercial or naval ships, are also equipped with their own echo sounders to provide“live” or up-to-date depth information for their immediate locality.
The present invention provides a method of calibrating (or at least checking) on-board echo sounders to ensure they are working properly.
Figure 2 shows an example of a marine vessel 50 on a body of water 40. The marine vessel 50 is equipped with an on-board echo sounder 60. The echo sound 60 emits a sonar pulse into the water 40 from the surface toward the seabed 70 (or floor of the local body of water, e.g. lake). The sound pulse is reflected from the seabed 70 (at point 82), and returns to the surface and is detected by the echo sounder 60.
The depth d of the water 40 (i.e. the local distance to the seabed 70) is measured by multiplying the speed of sound in water vSOm,d by half the time t taken for the signal to return to the echo sounder 60 after being emitted:
Figure imgf000005_0001
Whilst the approximate speed of sound vso«nd is known to be 1.5 x 103 m/s, the speed of sound is affected by, amongst other things pressure (and therefore depth), temperature and salinity. Therefore, for precise depth measurement the exact local speed of sound must also be measured, for example by deploying a sound velocity probe info the water.
In order to calibrate the echo sounder 60, and ensure it is working correctly, the location of the echo sounder must be obtained, so that the measured depths can be compared to previously recorded depths for the same, or nearby, location. Modern marine vessels are often equipped with electrical navigation equipment, such as Global Positioning System (GPS) receivers. These provide accurate geolocation data to the marine vessel, allowing the operators to identify their exact location. In a first example, the location of the echo sounder 60 is considered to be the same as the location of the marine vessel 50 upon which it is carried.
Once the location of the echo sounder 60 (or at least the location of the marine vessel 50 upon which it is carried) is known, a second water depth measurement for that location (or nearby location) is obtained. This second depth measurement may come from any source, including nautical chart information (digital or traditional), a second echo sounder (not shown) located on the same vessel, or echo sounder measurements from a nearby other vessel. The method may also involve comparing the echo sounder depth measurement to multiple other local measurements.
In the example shown in Figure 2, the second depth measurement is obtained by locating the nearest previously charted depth to the location of the echo sounder 60, shown at depth point 84. The second depth measurement (at point 84) is compared to the first water depth (at point 82) measured by the echo sounder 60 on the marine vessel 50 and the difference 86 is calculated. If the value of the difference 86 is greater than a predetermined threshold, a pre determined action is carried out. The action may take any form, such as logging/flagging the measured depth as outlying from the predetermined tolerance, alerting a user directly, or perhaps automatically adjusting the echo sounder. The distance between the first 82 and second 84 points of depth measurement is also recorded. The benefits of carrying out“on-the-go” echo sounder calibration mean that any results can be checked whilst the marine vessel is operating at sea, rather than requiring the vessel to be in a port in order to carry out static or physical calibration. This means the reliability and confidence in the echo sounder results can be maintained and/or improved during use, and any errors or problems can be identified (and possibly addressed) immediately, instead of remaining undetected until the vessel is next in port for inspection.
!n a second example, in order to provide a more accurate calibration, and for echo sounders on larger marine vessels, the position of the echo sounder in relation to the nominal (or calculated) position of the marine vessel may be calculated. Figure 3 shows a top-down view of the marine vessel 50 as seen in Figure 2. The location of the marine vessel 50 is calculated by a GPS receiver (or other location device) at point A. The echo sounder 60 is located at point B on the vessel 50, a known distance A-B (and direction) from point A. By measuring the orientation (angle a) of the marine vessel 50, and knowing the distance A-B between the known location A of the vessel and the relative position B of the echo sounder 60, the accurate location B of the echo sounder 60 can be calculated. The more-accurate location data for the echo sounder 60 is used to determine the nearest previously measured depth point C which may not be the same as the closest depth point to the (nominal) location A of the vessel 50. The distance B-C between the echo sounder 60 (at point B) and previously measured depth (at point C) is also recorded.
In another example, in order to carry out more accurate depth measurements, the location of the marine vessel 50 (or the echo sounder 60) is used to obtain local tidal information. By taking the tide into account, the echo sounder 60 can be more accurately calibrated since the difference between the two measured depths can be adjusted to take the difference in tide heights into account.
In one example, and as discussed above, the second water depth is obtained from a previously surveyed data point closest to the echo sounder location. In another example, the second depth measurement may be obtained from a second echo sounder located on the same vessel. The positions of both echo sounders (and the distance between them) is known and therefore a pre- determined threshold for any difference in their readings can be determined. In another example, the second depth measurement is provided from an echo sounder located on a second marine vessel whose position is known at the time of the second depth measurement. In another example, multiple vessels taking echo sounder measurements in a relatively close proximity to each other (although not necessarily at the same time) may share the depth measurements to cross-calibrate the multiple echo sounders.
It is expected that the greater the distance between the location of the first measurement from the second measurement, the greater the variance in depth between the two. For example, it is to be assumed that two separate points on the seabed 1 m apart are more likely to have a smaller depth difference than two separate points on the seabed 100m apart. Therefore, in one example, the pre-determ ined threshold is dependent upon the distance between the first (echo sounder) location and the second measured depth location.
Figure 4 shows a graph comprising example results from echo sounder measurements; plotting the difference between the first (i.e. echo sounder) and second measurements against the distance between the two measurement locations. A tolerance or threshold line is shown for both positive and negative difference values, and the tolerance increases as the distance B-C between the between the first (echo sounder) location and the second measured depth location increases.
Figure 5 shows a flow chart of a method according to the present invention. At stage S1 , a first water depth is measured using an echo sounder on a marine vessel. At stage S2, location data for the echo sounder is obtained. At stage S3, a second (previously measured) water depth for a location nearby to the echo sounder is obtained. At stage S4, the first and second water depth measurement values are compared. At stage S5, a pre-determ ined action is carried out (e.g. alerting a user, or flagging the reading as an outlier) if the first measured depth differs from the second depth by more than a pre-determ ined amount. Steps S1 , S2 and S3 may be carried out in any order, or indeed at the same time. ln one example, the pre-determ ined threshold is dynamically updated as more depth data is measured. Therefore, as the echo sounder 60 records more depth measurements, and compares them to previously measured depths, a more accurate (i.e. tighter) error profile can be calculated.
In order to obtain even more accuracy in calibrating the echo sounder 60, the draft of the marine vessel 50 (i.e. how low the marine vessel sits in the water) may be taken into account during calibrating calculations. If the marine vessel 50 is heavily loaded, it may sit lower in the water, and any depth measurement should take this into account.
In one example, a computer device is adapted to carry out the method steps described by the present invention.

Claims

1. A method of calibrating an echo sounder on a marine vessel, the method comprising:
(S1 ) measuring a first water depth using an echo sounder on a marine vessel;
(52) obtaining location data for the echo sounder;
(53) obtaining a second water depth from another source for a location nearby to the echo sounder;
(S4) comparing the first depth to the second depth; and
(S5) carrying out a pre-determ ined action if the measured depth differs from the second depth by more than a pre-determ ined threshold.
2. The method according to claim 1 , wherein the second water depth is surveyed data for a location closest to the echo sounder.
3. The method according to claim 1 , wherein the second water depth is from a second echo sounder on the same marine vessel. 4. The method according to any preceding claim, wherein the step of obtaining the location data for the echo sounder comprises:
obtaining location data A for the vessel;
obtaining orientation data a for the vessel; obtaining positional data A-B for the echo sounder on the vessel; and
calculating the location data B for the echo sounder.
5. The method according to any preceding claim, comprising obtaining tidal data for the location of the echo sounder;
6. The method according to any preceding claim, wherein the pre determined threshold is dependent upon the distance B-C between the echo sounder location B and the second measured depth location C.
7. The method according to any preceding claim, wherein the pre determined threshold is dynamically updated as more depth data is measured.
8. The method according to any preceding claim, wherein the draft of the marine vessel is factored into the echo sounder depth measurements.
9. A computing device adapted to carry out the method according to any preceding claim.
PCT/GB2020/050075 2019-01-17 2020-01-15 Echo sounder callibration Ceased WO2020148531A1 (en)

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Cited By (4)

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