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Tytuł artykułu

Radar characteristics of precipitation affecting the tracking of ship’s radar objects

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Treść / Zawartość
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Języki publikacji
EN
Abstrakty
EN
In this paper, we consider the possibility of using the radar characteristics of precipitation in order to reduce the negative impact of the echo signal generated by them on the radar tracking of objects performed by the ship’s radar. In the formation of an echo signal by precipitation, both the precipitation particles themselves: their size, state (solid or liquid phase), shape, and the factors that determine their combined action (concentration, relative position, preferred orientation), are important. The size of rain particles when compared to the wavelength emitted by the ship's radar antenna contributes to the creation of a larger or smaller noise echo on the display of the ship's radar, the power of which in the Rayleigh scattering region toward the radar is characterized by the effective scattering area. Falling raindrops are a collection of randomly located reflectors and their scattering properties depend on the spatial distribution and regularity of movement. At the same time, the radar characteristics of clouds with precipitation generated by them can be used in ship radars to determine the intensity of the atmospheric process along the ship’s route, and the uncertainty in determining the attenuation of the power of an electromagnetic wave emitted by a ship’s radar antenna and passing through the precipitation zone can be reduced by simultaneous use of two wavelengths on which ship’s radars operate.
Twórcy
autor
  • National University «Odessa Maritime Academy», Odessa, Ukraine
Bibliografia
  • 1. Stepanenko V. D.: Radiolocation in meteorology. L.:Gidrometeoizdat. 352 (1973).
  • 2. Krasyuk N.P., Koblov V.L., Krasyuk V.N.: Influence of the troposphere and underlying surface on radar operation. M.: Radio and communication. 213 (1988).
  • 3. Abramov V.V.: Electrodynamic model of interference from hydrometeors. Questions of radio electronics. 15, 92-97 (1981).
  • 4. Barton D.K.: Models of interfering reflections from the earth's surface for the analysis and design of radars. M.: TIIER. 73, 2, 27-35 (1985).
  • 5. Alibegova Zh. D.: The structure of fields of liquid precipitation for short intervals of time. L.: Gidrometeoizdat. 134 (1975).
  • 6. Battan L.D.: Radar meteorology / ed. E.M. Salman and K.Ya. Kondratiev. L.: Gidrometeoizdat. 196 (1962).
  • 7. Brylev G.B., Pleshcheev Yu.G., Stepanenko V.D., et al.: Influence of radio wave attenuation on the size of the area of radio echo zones of precipitation, In: Radar meteorology. L.: Gidrometeoizdat. 59-63 (1981).
  • 8. Brylev G.B., Gashina S.B., Nizdoiminoga G.L.: Radar characteristics of clouds and precipitation. L.: Gidrometeoizdat. 231 (1986).
Uwagi
Opracowanie rekordu ze środków MEiN, umowa nr SONP/SP/546092/2022 w ramach programu "Społeczna odpowiedzialność nauki" - moduł: Popularyzacja nauki i promocja sportu (2022-2023).
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-7a6a4ae8-54a0-4b5e-b332-e1c0031279f7
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