Scattering Properties of the Ocean Surface: The Miller-Brown-Vegh Model Revisited
We review the model of Miller-Brown-Vegh (MBV) that is commonly used to describe scattering from the ocean surface. The model has been built on two essential elements: the Kirchhoff approximation and an assumption regarding the probability distribution of the ocean surface elevations. A comparison w...
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Veröffentlicht in: | IEEE transactions on antennas and propagation 2008-04, Vol.56 (4), p.1103-1109 |
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creator | Hristov, T.S. Anderson, K.D. Friehe, C.A. |
description | We review the model of Miller-Brown-Vegh (MBV) that is commonly used to describe scattering from the ocean surface. The model has been built on two essential elements: the Kirchhoff approximation and an assumption regarding the probability distribution of the ocean surface elevations. A comparison with theoretical results preceeding the MBV model as well as with experimental data suggest that the MBV model is inconsistent with the predicted and observed probability distribution of sea waves. Here, a scattering model based on more rigorous statistics of the ocean surface is considered instead. The analysis we present offers an explanation as well as a remedy for the reported tendency of models describing propagation in evaporation ducts to overestimate the signal's intensity at the receiver. |
doi_str_mv | 10.1109/TAP.2008.919177 |
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The model has been built on two essential elements: the Kirchhoff approximation and an assumption regarding the probability distribution of the ocean surface elevations. A comparison with theoretical results preceeding the MBV model as well as with experimental data suggest that the MBV model is inconsistent with the predicted and observed probability distribution of sea waves. Here, a scattering model based on more rigorous statistics of the ocean surface is considered instead. The analysis we present offers an explanation as well as a remedy for the reported tendency of models describing propagation in evaporation ducts to overestimate the signal's intensity at the receiver.</description><identifier>ISSN: 0018-926X</identifier><identifier>EISSN: 1558-2221</identifier><identifier>DOI: 10.1109/TAP.2008.919177</identifier><identifier>CODEN: IETPAK</identifier><language>eng</language><publisher>New York, NY: IEEE</publisher><subject>Applied classical electromagnetism ; Applied sciences ; Diffraction, scattering, reflection ; Ducts ; Electromagnetic scattering ; Electromagnetic wave propagation, radiowave propagation ; Electromagnetism; electron and ion optics ; evaporation duct ; Exact sciences and technology ; Fundamental areas of phenomenology (including applications) ; Kirchhoff's Law ; Miller-Brown-Vegh (MBV) model ; Oceans ; Physics ; Predictive models ; Probability distribution ; Radiocommunications ; Radiowave propagation ; Rough surfaces ; Sea surface ; Sea surface scattering ; Statistical distributions ; Surface waves ; Telecommunications ; Telecommunications and information theory</subject><ispartof>IEEE transactions on antennas and propagation, 2008-04, Vol.56 (4), p.1103-1109</ispartof><rights>2008 INIST-CNRS</rights><rights>Copyright The Institute of Electrical and Electronics Engineers, Inc. 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The model has been built on two essential elements: the Kirchhoff approximation and an assumption regarding the probability distribution of the ocean surface elevations. A comparison with theoretical results preceeding the MBV model as well as with experimental data suggest that the MBV model is inconsistent with the predicted and observed probability distribution of sea waves. Here, a scattering model based on more rigorous statistics of the ocean surface is considered instead. The analysis we present offers an explanation as well as a remedy for the reported tendency of models describing propagation in evaporation ducts to overestimate the signal's intensity at the receiver.</description><subject>Applied classical electromagnetism</subject><subject>Applied sciences</subject><subject>Diffraction, scattering, reflection</subject><subject>Ducts</subject><subject>Electromagnetic scattering</subject><subject>Electromagnetic wave propagation, radiowave propagation</subject><subject>Electromagnetism; electron and ion optics</subject><subject>evaporation duct</subject><subject>Exact sciences and technology</subject><subject>Fundamental areas of phenomenology (including applications)</subject><subject>Kirchhoff's Law</subject><subject>Miller-Brown-Vegh (MBV) model</subject><subject>Oceans</subject><subject>Physics</subject><subject>Predictive models</subject><subject>Probability distribution</subject><subject>Radiocommunications</subject><subject>Radiowave propagation</subject><subject>Rough surfaces</subject><subject>Sea surface</subject><subject>Sea surface scattering</subject><subject>Statistical distributions</subject><subject>Surface waves</subject><subject>Telecommunications</subject><subject>Telecommunications and information theory</subject><issn>0018-926X</issn><issn>1558-2221</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2008</creationdate><recordtype>article</recordtype><sourceid>RIE</sourceid><recordid>eNqFkb1PwzAQxS0EEqUwM7BESMCU4q_EMVup-JKKWmhBbJbrXFpXISl2CuK_x1WrDgwwne7e75509xA6JrhDCJaX4-6wQzHOOpJIIsQOapEkyWJKKdlFLYxJFkuavu2jA-_noeUZ5y30NDK6acDZahoNXb0A11jwUV1EzQyigQFdRaOlK7SBq2gcRo-2LMHF167-quJXmM6ixzqHMnqGT-ttA_kh2it06eFoU9vo5fZm3LuP-4O7h163HxtOaBMbliQmnWCaSZ4QrA3GNAcoTE4TDTmROqWGcIKZ4TKHMKRpboSeTJigrDCsjS7WvgtXfyzBN-rdegNlqSuol15JzFImGeeBPP-TDIzgIkv-BSlOWXg1C-DpL3BeL10VzlWSUIZTwVbQ5RoyrvbeQaEWzr5r960IVqvIVIhMrSJT68jCxtnGVnujy8Lpyli_XaOYCsGzlfPJmrMAsJV5kBLJ2Q_Me51C</recordid><startdate>20080401</startdate><enddate>20080401</enddate><creator>Hristov, T.S.</creator><creator>Anderson, K.D.</creator><creator>Friehe, C.A.</creator><general>IEEE</general><general>Institute of Electrical and Electronics Engineers</general><general>The Institute of Electrical and Electronics Engineers, Inc. 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The model has been built on two essential elements: the Kirchhoff approximation and an assumption regarding the probability distribution of the ocean surface elevations. A comparison with theoretical results preceeding the MBV model as well as with experimental data suggest that the MBV model is inconsistent with the predicted and observed probability distribution of sea waves. Here, a scattering model based on more rigorous statistics of the ocean surface is considered instead. The analysis we present offers an explanation as well as a remedy for the reported tendency of models describing propagation in evaporation ducts to overestimate the signal's intensity at the receiver.</abstract><cop>New York, NY</cop><pub>IEEE</pub><doi>10.1109/TAP.2008.919177</doi><tpages>7</tpages></addata></record> |
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subjects | Applied classical electromagnetism Applied sciences Diffraction, scattering, reflection Ducts Electromagnetic scattering Electromagnetic wave propagation, radiowave propagation Electromagnetism electron and ion optics evaporation duct Exact sciences and technology Fundamental areas of phenomenology (including applications) Kirchhoff's Law Miller-Brown-Vegh (MBV) model Oceans Physics Predictive models Probability distribution Radiocommunications Radiowave propagation Rough surfaces Sea surface Sea surface scattering Statistical distributions Surface waves Telecommunications Telecommunications and information theory |
title | Scattering Properties of the Ocean Surface: The Miller-Brown-Vegh Model Revisited |
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