Radar Scattering from Modulated Wind Waves: Proceedings of the Workshop on Modulation of Short Wind Waves in the Gravity-Capillary Range by Non-Uniform Currents, held in Bergen aan Zee, The Netherlands, 24?26 May 1988
Ten years ago, de Loor and co-workers at TNO, The Netherlands, were the first to report bottom topography patterns in real aperture radar (RAR) images of the southern North Sea. At that time, this was a real puzzle. The skin depth of microwaves for sea water is only of the order of centimeters while...
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Format: | Elektronisch E-Book |
Sprache: | English |
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Dordrecht
Springer Netherlands
1989
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Online-Zugang: | BTU01 Volltext |
Zusammenfassung: | Ten years ago, de Loor and co-workers at TNO, The Netherlands, were the first to report bottom topography patterns in real aperture radar (RAR) images of the southern North Sea. At that time, this was a real puzzle. The skin depth of microwaves for sea water is only of the order of centimeters while the sea bottom is about 20 meters below the surface. Electromagnetic radiation therefore cannot probe the bottom directly. Similar phenomena were found in radar imagery from SEASAT and SIR-AlB synthetic aperture radars (SAR's) of Nantucket Shoals, the English Channel and many other coastal areas. Since then theory and ocean field experiments (Le., Phelps Bank, Georgia Straits, SARSEX, TOWARD, FASINEX, etc.) have advanced our understanding considerably. We now know that these surface signatures are the results of surface currents, perturbed by the bottom topography, which refract the propagation and modulate the energy of (short) surface waves so as to cause microwave backscatter power variations. Hence, any large scale ocean features containing nonuniform surface currents (i.e. internal waves, eddies, fronts, etc.) will cause similar manifestations in the radar imagery by means of current-wave-microwave interactions. Observations confirm this |
Beschreibung: | 1 Online-Ressource (X, 275 p) |
ISBN: | 9789400923096 |
DOI: | 10.1007/978-94-009-2309-6 |
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520 | |a Ten years ago, de Loor and co-workers at TNO, The Netherlands, were the first to report bottom topography patterns in real aperture radar (RAR) images of the southern North Sea. At that time, this was a real puzzle. The skin depth of microwaves for sea water is only of the order of centimeters while the sea bottom is about 20 meters below the surface. Electromagnetic radiation therefore cannot probe the bottom directly. Similar phenomena were found in radar imagery from SEASAT and SIR-AlB synthetic aperture radars (SAR's) of Nantucket Shoals, the English Channel and many other coastal areas. Since then theory and ocean field experiments (Le., Phelps Bank, Georgia Straits, SARSEX, TOWARD, FASINEX, etc.) have advanced our understanding considerably. We now know that these surface signatures are the results of surface currents, perturbed by the bottom topography, which refract the propagation and modulate the energy of (short) surface waves so as to cause microwave backscatter power variations. Hence, any large scale ocean features containing nonuniform surface currents (i.e. internal waves, eddies, fronts, etc.) will cause similar manifestations in the radar imagery by means of current-wave-microwave interactions. Observations confirm this | ||
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dewey-ones | 551 - Geology, hydrology, meteorology |
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dewey-sort | 3551.46 |
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discipline | Geologie / Paläontologie |
doi_str_mv | 10.1007/978-94-009-2309-6 |
format | Electronic eBook |
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id | DE-604.BV045176834 |
illustrated | Not Illustrated |
indexdate | 2024-07-10T08:10:45Z |
institution | BVB |
isbn | 9789400923096 |
language | English |
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spelling | Radar Scattering from Modulated Wind Waves Proceedings of the Workshop on Modulation of Short Wind Waves in the Gravity-Capillary Range by Non-Uniform Currents, held in Bergen aan Zee, The Netherlands, 24?26 May 1988 edited by G. J. Komen, W. A. Oost Proceedings of the Workshop on Modulation of Short Wind Waves in the Gravity-Capillary Range by Non-Uniform Currents, held in Bergen aan Zee, The Netherlands, May 24-26, 1988 Dordrecht Springer Netherlands 1989 1 Online-Ressource (X, 275 p) txt rdacontent c rdamedia cr rdacarrier Ten years ago, de Loor and co-workers at TNO, The Netherlands, were the first to report bottom topography patterns in real aperture radar (RAR) images of the southern North Sea. At that time, this was a real puzzle. The skin depth of microwaves for sea water is only of the order of centimeters while the sea bottom is about 20 meters below the surface. Electromagnetic radiation therefore cannot probe the bottom directly. Similar phenomena were found in radar imagery from SEASAT and SIR-AlB synthetic aperture radars (SAR's) of Nantucket Shoals, the English Channel and many other coastal areas. Since then theory and ocean field experiments (Le., Phelps Bank, Georgia Straits, SARSEX, TOWARD, FASINEX, etc.) have advanced our understanding considerably. We now know that these surface signatures are the results of surface currents, perturbed by the bottom topography, which refract the propagation and modulate the energy of (short) surface waves so as to cause microwave backscatter power variations. Hence, any large scale ocean features containing nonuniform surface currents (i.e. internal waves, eddies, fronts, etc.) will cause similar manifestations in the radar imagery by means of current-wave-microwave interactions. Observations confirm this Earth Sciences Oceanography Remote Sensing/Photogrammetry Atmospheric Sciences Earth sciences Atmospheric sciences Remote sensing Komen, G. J. edt Oost, W. A. edt Erscheint auch als Druck-Ausgabe 9789401075374 https://doi.org/10.1007/978-94-009-2309-6 Verlag URL des Erstveröffentlichers Volltext |
spellingShingle | Radar Scattering from Modulated Wind Waves Proceedings of the Workshop on Modulation of Short Wind Waves in the Gravity-Capillary Range by Non-Uniform Currents, held in Bergen aan Zee, The Netherlands, 24?26 May 1988 Earth Sciences Oceanography Remote Sensing/Photogrammetry Atmospheric Sciences Earth sciences Atmospheric sciences Remote sensing |
title | Radar Scattering from Modulated Wind Waves Proceedings of the Workshop on Modulation of Short Wind Waves in the Gravity-Capillary Range by Non-Uniform Currents, held in Bergen aan Zee, The Netherlands, 24?26 May 1988 |
title_alt | Proceedings of the Workshop on Modulation of Short Wind Waves in the Gravity-Capillary Range by Non-Uniform Currents, held in Bergen aan Zee, The Netherlands, May 24-26, 1988 |
title_auth | Radar Scattering from Modulated Wind Waves Proceedings of the Workshop on Modulation of Short Wind Waves in the Gravity-Capillary Range by Non-Uniform Currents, held in Bergen aan Zee, The Netherlands, 24?26 May 1988 |
title_exact_search | Radar Scattering from Modulated Wind Waves Proceedings of the Workshop on Modulation of Short Wind Waves in the Gravity-Capillary Range by Non-Uniform Currents, held in Bergen aan Zee, The Netherlands, 24?26 May 1988 |
title_full | Radar Scattering from Modulated Wind Waves Proceedings of the Workshop on Modulation of Short Wind Waves in the Gravity-Capillary Range by Non-Uniform Currents, held in Bergen aan Zee, The Netherlands, 24?26 May 1988 edited by G. J. Komen, W. A. Oost |
title_fullStr | Radar Scattering from Modulated Wind Waves Proceedings of the Workshop on Modulation of Short Wind Waves in the Gravity-Capillary Range by Non-Uniform Currents, held in Bergen aan Zee, The Netherlands, 24?26 May 1988 edited by G. J. Komen, W. A. Oost |
title_full_unstemmed | Radar Scattering from Modulated Wind Waves Proceedings of the Workshop on Modulation of Short Wind Waves in the Gravity-Capillary Range by Non-Uniform Currents, held in Bergen aan Zee, The Netherlands, 24?26 May 1988 edited by G. J. Komen, W. A. Oost |
title_short | Radar Scattering from Modulated Wind Waves |
title_sort | radar scattering from modulated wind waves proceedings of the workshop on modulation of short wind waves in the gravity capillary range by non uniform currents held in bergen aan zee the netherlands 24 26 may 1988 |
title_sub | Proceedings of the Workshop on Modulation of Short Wind Waves in the Gravity-Capillary Range by Non-Uniform Currents, held in Bergen aan Zee, The Netherlands, 24?26 May 1988 |
topic | Earth Sciences Oceanography Remote Sensing/Photogrammetry Atmospheric Sciences Earth sciences Atmospheric sciences Remote sensing |
topic_facet | Earth Sciences Oceanography Remote Sensing/Photogrammetry Atmospheric Sciences Earth sciences Atmospheric sciences Remote sensing |
url | https://doi.org/10.1007/978-94-009-2309-6 |
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