To predict the performance of coastal and shipborne radars, it is essential to assess the propagation characteristics of electromagnetic waves in the maritime boundary layer. To be independent upon environmental measurements, which are generally not as precise and reliable as they have to be for a proper input to simulation programs, usually based upon parabolic equation models, a method to retrieve the refractive index gradients in the low troposphere is the Refractivity from Clutter (RFC) algorithm. The propagation factor is computed from the received clutter power and is iteratively processed in order to retrieve the refractive index profiles. Under a respective French-German technical agreement a measurement program concerning radar propagation in the maritime boundary layer has been initiated, with contributions from ONERA-CERT, DGA MI / TN, Fraunhofer-FHR and the German Technical Center for Ships and Naval Weapons (WTD 71). The paper gives an overview on the RFC method with examples from the previous campaigns. It describes the experimental set-up and its methodology.
Air-sea interaction processes play a dominant role with respect to detection ranges of shipborne radar and infrared sensor
systems. Especially in the littoral most often temperature and humidity gradients affect propagation paths and are the
reason for abnormal phenomena such as ducting or mirage. Besides refractivity, spray and aerosols ejected from the sea
surface can further degrade the quality of shipborne surveillance systems. Thus environmental effects might seriously
hamper ship self defense.
During the Ligurian Air-Sea Interaction Experiment (LASIE '07 - 16.06.-26.06.2007) the Federal Armed Forces
Underwater Acoustics and Marine Geophysics Research Institute (FWG) carried out simultaneous in-situ measurements
of meteorological and oceanographic parameters to study air-sea interaction processes with respect to littoral boundary
layer variability.
The characterization of the environment included both, in-situ measurements of atmospheric and sea surface parameters.
Investigations were carried out on board RV PLANET, RV URANIA and at the ODAS-Italy1 buoy of the Italian
National Council of Research (CNR). On board RV PLANET the sea surface and meteorological conditions were
analyzed by two multi-sensor buoys, ship sensors and radiosondes. Emphasis was given to the vertical structure of the
Marine Boundary Layer (MBL) and its variability. It was analyzed by a one lense lidar ceilometer CL31, a tethersonde
system TT12 and radiosondes RS92 (Vaisala). The latter were launched every three hours. The TT12 consisted of three
radiosondes, which could be adapted to separate altitudes of special interest. The experiment was characterized by
changing meteorological conditions resulting in offshore and onshore blowing winds. In the first case the air temperature
TAir was higher than the sea surface temperature TWater leading to a very stable surface layer. This situation was
associated with a strong temperature inversion and a very clear atmosphere with a visibility of about 70 km. The second
case (TAir<TWater) was dominated by convection processes and a pronounced aerosol production. Good correlation was
found for the Mixing Layer Height (MLH) by the lidar ceilometer and the radio soundings.
The detection and tracking of naval targets, including low Radar Cross Section (RCS) objects like inflatable boats or sea skimming missiles requires a thorough knowledge of the propagation properties of the maritime boundary layer. Models are in existence, which allow a prediction of the propagation factor using the parabolic equation algorithm. As a necessary input, the refractive index has to be known. This index, however, is strongly influenced by the actual atmospheric conditions, characterized mainly by temperature, humidity and air pressure. An approach is initiated to retrieve the vertical profile of the refractive index from the propagation factor measured on an onboard target. The method is based on the LS-SVM (Least-Squares Support Vector Machines) theory. The inversion method is here used to determine refractive index from data measured during the VAMPIRA campaign (Validation Measurement for Propagation in the Infrared and RAdar) conducted as a multinational approach over a transmission path across the Baltic Sea. As a propagation factor has been measured on two reference reflectors mounted onboard a naval vessel at different heights, the inversion method can be tested on both heights. The paper describes the experimental campaign and validates the LS-SVM inversion method for refractivity from propagation factor on simple measured data.
The detection and tracking of naval targets, including low RCS objects like inflatable boats requires a thorough
knowledge of the propagation properties of the maritime boundary layer. Models are in existence, which allow a
prediction of the propagation factor using the parabolic equation algorithm. As a necessary input the refractive index of
the atmosphere has to be known. This parameter, however, is strongly influenced by the actual atmospheric conditions,
characterized mainly by air-sea temperature difference, humidity and air pressure. An approach was initiated to retrieve
the vertical profile of the refractive index from sea clutter data. The method is based on the LS-SVM (Least-Squares
Support Vector Machines) theory and has already been validated on simulated data. Here an inversion method to
determine propagation factors is presented based upon data measured during the Vampira campaign conducted as a
multinational approach over a transmission path across the Baltic Sea. As the propagation factor has been measured on
two reference reflectors mounted onboard a naval vessel at different heights, the results can be combined in order to
increase the accuracy of the inversion system. The paper discusses results achieved with the inversion method.
In the framework of a cooperative program between Singapore and Germany, radar propagation measurements over sea
were carried out in the tropical area of Singapore Strait. The data have been analyzed and propagation models have been
tested using the relevant environmental information. It turned out that the tropical atmospheric conditions were
considerably different to those of moderate climate areas, such as the Baltic Sea or the North Sea.
The paper describes the experimental approach and discusses results of tropical conditions compared to those of
European coastal environments.
In the marine boundary layer, air-sea interaction processes have an impact on radar and infrared propagation. Range performance near the sea surface depends on the meteorological conditions and sea surface roughness. Strong gradients of humidity and temperature close to the air-water interface are most often the reason for abnormal propagation effects such as ducting or mirage. For ship borne radars the evaporation duct is the dominant propagation mechanism affecting the maximum detection range of horizon-search radars. Ducting can also increase sea clutter return within and beyond the geometric horizon. Surface-based ducts can enhance land clutter return from extended ranges.
During a sea trial in the Baltic Sea in 2005, FWG characterized the environmental boundary layer. In-situ measurements included recordings of atmospheric and sea surface parameters. Simultaneous investigations were carried out at the land based test site and on board two ships. Based on FWG-buoy measurements and radiosoundings the sea surface and meteorological conditions were analyzed to study refractive variability within the maritime boundary layer. We compared measurement results with predictions of the mesoscale meteorological Local Model (LM), developed by German Weather Service.
Radar propagation was measured in addition to atmospheric conditions. A research vessel was illuminated by radar operating at X-band on outbound and inbound runs. The radar system was located at the pier of the land based test site. Radar propagation characteristics were measured on board the ship with two omni directional antennas mounted in 5.5 m and 16.8 m height above mean sea level.
Results of refractive variability are presented in conjunction with radar propagation data and model outputs.
The performance of radar sensors operating within the marine boundary layer is severely influenced by the actual atmospheric conditions, the sea surface and the geometry between radar and reflection point. Propagation models are in existence, which cope with the varying environment and allow a performance prediction for sensors in different radar bands. To assess the propagation within different layers simultaneously at X-, Ka- and W-band an experiment was performed using the experimental three frequency radar MEMPHIS operating against point targets at different heights above sea, carried on a naval vessel, which moved on outbound and inbound courses to ranges well beyond horizon. In-situ measurements included recordings of atmospheric properties and sea surface parameters. Based upon the environmental measurements, refractivity profiles were calculated. With the help of the vertical refractivity gradient and the air sea temperature difference, conditions for the radar propagation were determined.
The experimental results were used to validate respective simulations with the parabolic equation model TERPEM. In conclusion, the experimental results and calculations underline the importance of the environmental characterization of the marine boundary layer with high temporal and spatial resolution.
This paper describes the experimental approach and gives representative results for measurement and simulation.
Radar propagation near the sea surface depends on meteorological conditions and sea surface roughness. Often strong gradients of humidity and temperature can be observed close to the air-water interface leading to abnormal propagation effects such as ducting. For shipborne radars operating at frequencies above L-band, the evaporation duct is the dominant propagation mechanism affecting the maximum detection range of horizon-search radars. Ducting can also increase sea clutter return within and beyond the normal horizon, and surface-based ducts can enhance land clutter return from extended ranges.
During sea trials in the Skagerrak and the Baltic Sea in 2003 and 2004, FWG was responsible for environmental characterization of the boundary layer. In-situ measurements included recordings of atmospheric and sea surface parameters. Investigations with multi-sensor buoys and with radiosondes were performed on board the German research vessel PLANET respectively on FGS HELMSAND. The drift buoys developed by FWG provided unperturbed, time resolved information on air-sea interaction processes. In addition to meteorological parameters sea state, sea surface roughness, and sea surface temperature were measured. Refractivity profiles were determined based on data sets gathered by measurements of pressure, humidity and temperature from the sea surface up to 1 km altitude.
Simultaneously to atmospheric measurements radar propagation investigations were performed by FGAN-FHR (Research Institute for High Frequency Physics and Radar Techniques). PLANET, FGS STOLLERGRUND were illuminated by a radar operating at X-, Ka- and W-band. The radar system was located at the land-based test site Hirtshals, Denmark during the trials in 2003 and at the land-based test site Surendorf, Germany during the experiment in 2004. Radar propagation characteristics at X-band were measured on board the ships with two omnidirectional antennas mounted in two different altitudes above sea surface. Results of refractivity variability in the marine boundary layer are presented in conjunction with radar propagation data and model outputs.
Radar and infrared propagation drastically depend on the meteorological and oceanographic conditions. Concerning a joint sea trial of German research institutes at the Baltic Sea 2001, FWG was responsible for the environmental characterization of the marine boundary layer. In-situ measurements included recordings of atmospheric properties and sea surface parameters. They were studied by two multi-sensor buoys, on board a vessel and with radiosondes. Pressure, air temperature and humidity were measured from the sea surface to 1 km altitude. The free drifting buoys which have been constructed at FWG offer the opportunity to gain unperturbed, time resolved information about environmental parameters up to 5 m above sea level. Based on the in-situ measurements refractivity profiles can be calculated. With the help of the vertical refractivity gradient and the air sea temperature difference, conditions for radar and infrared propagation are determined. Further experimental results include wind speed and direction, wave height, rain rate and other important parameters. Taking advantage of the parabolic equation model radar propagation is calculated numerically. In conclusion, the experimental results and calculations underline the importance of the environmental characterization of the marine boundary layer with high temporal and spatial resolution.
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