- Research Article
- Open Access

# Silent Localization of Underwater Sensors Using Magnetometers

- Jonas Callmer
^{1}Email author, - Martin Skoglund
^{1}and - Fredrik Gustafsson (EURASIPMember)
^{1}

**2010**:709318

https://doi.org/10.1155/2010/709318

© Jonas Callmer et al. 2010

**Received:**1 July 2009**Accepted:**15 October 2009**Published:**11 January 2010

## Abstract

Sensor localization is a central problem for sensor networks. If the sensor positions are uncertain, the target tracking ability of the sensor network is reduced. Sensor localization in underwater environments is traditionally addressed using acoustic range measurements involving known anchor or surface nodes. We explore the usage of triaxial magnetometers and a friendly vessel with known magnetic dipole to silently localize the sensors. The ferromagnetic field created by the dipole is measured by the magnetometers and is used to localize the sensors. The trajectory of the vessel and the sensor positions are estimated simultaneously using an Extended Kalman Filter (EKF). Simulations show that the sensors can be accurately positioned using magnetometers.

## Keywords

- Global Navigation Satellite System
- Global Navigation Satellite System
- Magnetic Dipole
- Extend Kalman Filter
- Sensor Position

## 1. Introduction

Today, surveillance of ports and other maritime environments is getting increasingly important for naval and customs services. Surface vessels are rather easy to detect and track, unlike submarines and other underwater vessels which pose new threats such as terrorism and smuggling. To detect these vessels, an advanced underwater sensor network is necessary. Such sensors can measure fluctuations in for example, magnetic and electric fields, pressure changes, and acoustics.

Deploying an underwater sensor in its predetermined position can be difficult due to currents, surge, and the lack of a Global Navigation Satellite System (GNSS) functioning underwater. Sometimes the sensors must be deployed fast, resulting in very uncertain sensor positions. These positions must then be estimated in order to enable the network to accurately track an alien vessel.

Lately, many solutions to the underwater sensor localization problem have been suggested. They can be broadly divided into two major categories: range-based and range-free. In general, range-based schemes provide more accurate positioning than range-free schemes.

Range-based schemes use information about the range or angle between sensors. The problem is thereafter formulated as a multilateral problem. Common methods to measure range or angle include Time of Arrival (ToA), Time Difference of Arrival (TDoA), Angle of Arrival (AoA), or Received Signal Strength Indicator (RSSI). These methods usually require active pinging but silent methods based on TDoA have been suggested [1]. The 3D positioning problem can be transformed into a 2D problem by the use of depth sensors [2]. The range positioning scheme is often aided by surface nodes, anchor nodes, mobile beacons, or autonomous underwater vehicles [3–5]. Joint sensor localization and time synchronization were performed in [6].

Range-free schemes generally provide a coarse estimate of a node's location and their main advantages lie in their simplicity. Examples of range-free schemes are Density-aware Hop-count Localization (DHL) [7] and Area Localization Scheme (ALS) [8]. A more thorough description of underwater sensor localization solutions, can be found in the surveys [9, 10].

In this paper we propose a method to silently localize underwater sensors equipped with triaxial magnetometers using a friendly vessel with known static magnetization characteristics. (For methods to estimate the magnetic characteristics, see [11].) Each sensor is further equipped with a pressure sensor and an accelerometer used for depth estimation and sensor orientation estimation, respectively. To enable global positioning of the sensors, the vessel or one sensor must be positioned globally. To the best of the authors knowledge this is the first time magnetic dipole tracking is used for sensor localization.

For target tracking in shallow waters, magnetometers are often a more useful sensor than acoustics, since sound scatters significantly in these environments [12]. Birsan has explored the use of magnetometers and the magnetic dipole of a vessel for target tracking [13, 14]. Two sensors with known positions were used to track a vessel while simultaneously estimating the unknown magnetic dipole of the vessel. Tracking and estimation were performed using an unscented Kalman filter [13] and an unscented particle filter [14]. Dalberg et al. [15] fused electromagnetic and acoustic data to track surface vessels using underwater sensors.

Several studies of the electromagnetic characteristics of the maritime environment have stated that the permeability of the seabed differs considerably from the permeability of air or water. The environment should therefore be modeled as a horizontally stratified model with site specific permeability and layer thickness for each segment [12, 15, 16]. This has not been included in our simulation study but should be considered in field experiments.

In the past 10–15 years quite a lot of effort has been put into reducing the static magnetic signature of naval vessels by active signature cancelling. This has increased the importance of other sources of magnetic fields such as Corrosion Related Magnetism (CRM) [16, 17]. CRM is generated by currents in the hull, normally induced by corrosion or the propeller. It is therefore very difficult to estimate and subsequently difficult to cancel. This makes CRM important in naval target tracking but not so much in sensor localization. In our study, a friendly vessel used for sensor localization can turn off its active signature cancelling, resulting in a magnetic field from the dipole which is considerably stronger than the field induced by CRM. We have therefore neglected CRM.

An underwater sensor network used for real-time surveillance must be silent. Neither sensor localization, surveillance or data transfer can be allowed to expose the sensor network. Silent communication rules out the use of acoustic modems which are the common mean of wireless underwater data transfer [9]. We therefore assume that the sensors are connected by wire. As a consequence, common problems in underwater sensor networks such as time synchronization, limited bandwidth, and limited energy resources will be neglected.

The sensor localization problem is basically reversed Simultaneous Localization and Mapping (SLAM). In common SLAM [18, 19], landmarks in the environment are tracked with on-board sensors. The positions of these landmarks and the vehicle trajectory are estimated simultaneously in a filter. In sensor localization, the sensors are observing the vessel from the "landmarks" position. The problem has the same form as SLAM but with a known number of landmarks and known data association.

The paper outline is as follows: Section 2 describes the system, measurement models, and state estimation. Simulations of the performance of the positioning scheme, its sensitivity to different errors, and the importance of the appearance of the trajectory are studied in Section 3. The paper ends with conclusions.

## 2. Methodology

This section describes the nonlinear state estimation problem solved here with EKF-SLAM, how the vessel dynamics, and sensors are modeled and how different performance measures are computed. All vectors are expressed in a world fixed coordinate system unless otherwise stated.

### 2.1. System Description

The sensor positioning system is assumed to have the following process and measurement model:

where is a nonlinear state transition function, is a nonlinear measurement function, the state vector, the inputs, the process noise, input noise, and measurement noise. In SLAM the state vector consists of both the vessel position and landmark (sensor) states stacked, that is, .

#### 2.1.1. Process Model

The process model describes the vehicle and the sensors dynamics. There are complex vessel models available which include 3D orientation, angular rates, engine speed, rudder angle, waves, hull, and so forth; see for example [20]. Since we do not consider any particular vessel or weather condition, a very simple vessel model is used. It is assumed that no substantial movement in the -coordinate, pitch, and roll angles of the vessel is made, hence a nonlinear 5 states coordinated turn model is sufficient. The parametrization used is a linearized discretisation according to [21].

where is the sampling interval and denote position, speed, heading, and angular rate, respectively. Furthermore, it is assumed that the sensors are static and do not move after sometime of deployment, hence a process model for the sensors is

where is the number of sensors, and are sensor 's and position, respectively.

#### 2.1.2. Measurement Model

Each sensor contains a pressure sensor which is used as an input, , of the -component. The sensor also contains accelerometers which are used to determine the direction of the earth gravitational field. The magnetometers in the sensor can be used to compute the direction of the earth magnetic inclination if the environment is free from magnetic disturbances such as ships. In most cases the magnetic inclination vector will not be parallel to the gravitational vector (except for the magnetic north and south pole) and the sensor orientation may be readily measured. The sensor orientation is modeled as a static input .

In this paper we only consider the ferromagnetic signature due to the iron in vessel construction. The ferromagnetic signature stems from the large pieces of metal used to construct a vessel. Each piece has its own magnetic dipole and the sum of these dipoles can roughly be simplified into a single dipole. The magnetic flux density for a dipole diminishes cubically with the distance to the dipole. With vector magnetometers dipole orientation can be estimated. Triaxial measurements of the magnetic flux density from a dipole can be modeled as

where is the magnetic dipole of the vessel, and is the permeability of the medium. is the vector from each sensor to the vessel where is the static orientation of sensor in the global coordinate frame, and is the measured depth of the sensor. Note that and should be seen as inputs, , since these are measured variables but not part of the state vector. The dipole model without coordinate transformations can be found in for example [22]. In the proximity of the vessel, a possibly better model would be a multiple dipole model [23] where the measurement is the sum of several dipoles, but this is out of the scope of this paper. A single dipole is a reasonable approximation if the measurements are made at a large distance compared to vessel size [11].

### 2.2. State Estimation

Our approach to the state estimation problem is to use an Extended Kalman Filter (EKF) in the formulation of EKF-SLAM; for details see for example [18]. There are some characteristics in this system which do not usually exist in the common slam problem.

- (i)
The landmarks (sensor) are naturally associated to the measurements, that is, data association is solved.

- (ii)
The sensors global orientations are known which in turn makes it possible to estimate the orientation of the trajectory.

- (iii)
The planar motion assumption and the pressure sensor make it possible to transform sensor positioning into 2D.

A well-known problem with SLAM is the ever expanding state space that comes with addition of new landmarks which will eventually make it intractable to compute a solution. In a sensor network the number of sensors (landmarks) will normally be known.

Due to the duality of the estimation problem implied in slam, that is,*estimate a map and simultaneously localize the vehicle in the map*, the question of state observability needs to be answered. Previous observability analyses on the slam problem [24–29] have focused on vehicle fixed range and/or bearing sensors, such as laser and camera. Reference [26, 29] conclude that only one known landmark needs to be observed in 2D slam for the global map to be locally weakly observable. In our proposed system the sensors are in the actual landmarks position and their measurements are informative in both range and bearing to the dipole, hence the global map is observable if one sensor position is known. Theoretically this means that the sensor positions and the trajectory can be estimated in a global coordinate frame with a global map position error depending only on the error of the known sensor. If no global position of either sensor or vessel is available, the sensors can be positioned locally.

Even if the system is observable there are no guarantees that an EKF will converge since it depends on the linearization error and the initial linearization point. More recent approaches to the slam problem [30, 31] consider smoothing instead of filtering. These methods can handle linearization errors better since the whole trajectory and map can be relinearized. Yet, a good initial linearization point is necessary.

### 2.3. Cramér-Rao Lower Bound

Given the trajectory of a vessel, it is interesting to study a lower bound on the covariance of the estimated sensor positions. We have chosen to study the Cramér-Rao Lower Bound (CRLB) due to its simplistic advantages. CRLB is the inverse of the Fisher Information Matrix (FIM), , which in case of Gaussian measurement errors can be calculated as

where is Gaussian measurement noise and denote the gradient of w.r.t. . The CRLB of a sensor position is given by

where is true sensor position and is the corresponding estimate. Since information is additive, the FIM of a sensor location for a certain trajectory can be calculated as the sum of the FIMs from all vessel positions along the trajectory. The lower bound of the covariance of the sensor position estimate is then the inverse of the sum of the FIMs. A more extensive study of the fundamentals of CRLB can be found in [32].

## 3. Simulation Results

### 3.1. Magnetometers Only

If there is no reliable global position measurement of the vessel, the trajectory of the vessel must be estimated using the same magnetic fluctuations as are being used to localize the sensors. Simulations show that the sensor network needs to be more dense when no GNSS is available. If there is little or no overlap in which two or more sensors observe the vessel simultaneously, the trajectory estimate and in the end the sensor position estimates depend more on the vessel model than observations. Yet, the sensor positions are still coupled through the covariance matrix.

200 Monte Carlo simulations using different trajectories and sensor locations show that this configuration results in a positioning error of 26.3% in average. A sensor failing to retain the true sensor position within two standard deviations was considered incorrectly positioned. In Figure 2, sensor 7 is incorrectly positioned.

### 3.2. Magnetometers and GNSS

200 Monte Carlo simulations using different trajectories and sensor locations show that using magnetometers and GNSS results in a sensor positioning error of 12.9% in average.

### 3.3. Trajectory Evaluation Using CRLB

### 3.4. Sensitivity Analysis, Magnetic Dipole

The magnetic dipole of the vessel will probably not be accurately measured in a real world experiment. How will the positioning perform if the estimated magnitude of the dipole is for example 102% or 110% of the true magnitude?

Sensitivity analysis of error in dipole estimate.

Dipole | 80% | 90% | 95% | 98% | 99% | 100% |
---|---|---|---|---|---|---|

SLAM | 44.6% | 25.7% | 23.4% | 23.4% | 18.9% | 14.3% |

GNSS | 38.3% | 9.7% | 3.4% | 2.9% | 0.0% | 0.0% |

Dipole | 101% | 102% | 105% | 110% | 120% | |

SLAM | 14.3% | 14.3% | 16.6% | 34.3% | 53.1% | |

GNSS | 4.0% | 4.6% | 8.6% | 12.0% | 38.3% |

### 3.5. Sensitivity Analysis, Sensor Orientation

Sensitivity analysis of error in estimated sensor orientation.

Ori Cov | 0.0 rad | 0.01 rad | 0.04 rad | 0.16 rad | 0.36 rad |
---|---|---|---|---|---|

SLAM | 26.3% | 29.8% | 36.9% | 54.8% | 52.4% |

GNSS | 12.9% | 12.5% | 11.9% | 18.5% | 26.8% |

Note that the sensor positioning error of a system using GNSS and magnetometers was merely unaffected by the introduction of an orientation covariance of up to 0.04 rad. If the sensor observes the vessel from many different directions, the positioning still succeeds. When only magnetometers are used, the trajectory measurements cannot compensate for the errors in orientation, rendering larger positioning errors.

## 4. Conclusions

We have presented a silent underwater sensor localization scheme using triaxial magnetometers and a friendly vessel with known magnetic characteristics. More accurate sensor positions will enhance the detection, tracking, and classification abilities of the underwater sensor network. Monte Carlo simulations indicate that a sensor positioning accuracy of 26.1% is achievable when only magnetometers are used, and of 12.9% when GNSS and magnetometers are used. Knowing the magnetic dipole of the vessel is important and a dipole magnitude error of 10% results in a positioning error increase of about 10%. Simulations also show that our positioning scheme is quite unsensitive to minor errors in sensor orientation, when GNSS is used throughout the trajectory.

## Declarations

### Acknowledgments

This work was supported by the Strategic Research Center MOVIII, funded by the Swedish Foundation for Strategic Research, SSF, CADICS, a Linnaeus center funded by the Swedish Research Council, and LINK-SIC, an Industry Excellence Center founded by Vinnova.

## Authors’ Affiliations

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