Radar Scattering Modulated Wind (17 results)

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  • Condition: Used - Very good

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    hardcover. Condition: Very Good. Missing. First Edition. In stock. signed by both authors on first page. Signed by Author.

  • Language: English

    Published by Springer, 1989

    0792301463 / 9780792301462

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    Seller: Phatpocket Limited, Waltham Abbey, HERTS, United KingdomPhatpocket Limited

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    Condition: Good. Your purchase helps support Sri Lankan Children's Charity 'The Rainbow Centre'. Ex-library, so some stamps and wear, but in good overall condition. Our donations to The Rainbow Centre have helped provide an education and a safe haven to hundreds of children who live in appalling conditions.

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  • Language: English

    Published by Springer, 2012

    9401075379 / 9789401075374

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    Seller: Ria Christie Collections, Uxbridge, United KingdomRia Christie Collections

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    £ 106.66

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    Condition: New. In English.

  • Language: English

    Published by Springer, 1989

    0792301463 / 9780792301462

    • Hardcover

    Seller: Ria Christie Collections, Uxbridge, United KingdomRia Christie Collections

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    £ 106.71

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    Condition: New. In English.

  • Language: English

    Published by Springer, 1989

    0792301463 / 9780792301462

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    Seller: Books Puddle, Woodside, NY, U.S.A.Books Puddle

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    Condition: New

    £ 124.91

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    Condition: New. pp. 288 Index.

  • Language: English

    Published by Kluwer Academic Publishers, 1989

    0792301463 / 9780792301462

    • Hardcover

    Seller: Kennys Bookshop and Art Galleries Ltd., Galway, GY, IrelandKennys Bookshop and Art Galleries Ltd.

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    Condition: New

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    Condition: New. 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 Editor(s): Komen, G. J.; Oost, W. A. Num Pages: 275 pages, biography. BIC Classification: RBKC. Category: (P) Professional & Vocational; (UP) Postgraduate, Research & Scholarly. Dimension: 234 x 156 x 17. Weight in Grams: 581. . 1989. Hardback. . . . .

  • Condition: New

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    Paperback. Condition: Brand New. 288 pages. 9.25x6.10x0.65 inches. In Stock.

  • Language: English

    Published by Kluwer Academic Publishers, 1989

    0792301463 / 9780792301462

    • Hardcover

    Seller: Kennys Bookstore, Olney, MD, U.S.A.Kennys Bookstore

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    Condition: New. 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 Editor(s): Komen, G. J.; Oost, W. A. Num Pages: 275 pages, biography. BIC Classification: RBKC. Category: (P) Professional & Vocational; (UP) Postgraduate, Research & Scholarly. Dimension: 234 x 156 x 17. Weight in Grams: 581. . 1989. Hardback. . . . . Books ship from the US and Ireland.

  • Language: English

    Published by Springer Netherlands, 2012

    9401075379 / 9789401075374

    • Softcover

    Seller: moluna, Greven, Germanymoluna

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    Condition: New. 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 Ten years ago, de Loor and co-workers at TNO, The Netherlands, were the firs.

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    Taschenbuch. Condition: Neu. Neuware - 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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    Buch. Condition: Neu. Druck auf Anfrage Neuware - Printed after ordering - 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.

  • Language: English

    Published by Springer Netherlands Mrz 1989, 1989

    0792301463 / 9780792301462

    • Hardcover
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    Seller: BuchWeltWeit Ludwig Meier e.K., Bergisch Gladbach, GermanyBuchWeltWeit Ludwig Meier e.K.

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    Buch. Condition: Neu. This item is printed on demand - it takes 3-4 days longer - Neuware -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. 288 pp. Englisch.

  • Language: English

    Published by Springer Netherlands, 1989

    0792301463 / 9780792301462

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    Seller: moluna, Greven, Germanymoluna

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    Gebunden. Condition: New. Dieser Artikel ist ein Print on Demand Artikel und wird nach Ihrer Bestellung fuer Sie gedruckt. 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 Ten years ago, de Loor and co-workers at TNO, The Netherlands, were the firs.

  • Language: English

    Published by Springer, 1989

    0792301463 / 9780792301462

    • Hardcover
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    Seller: Majestic Books, Hounslow, United KingdomMajestic Books

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    Condition: New

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    Condition: New. Print on Demand pp. 288 52:B&W 6.14 x 9.21in or 234 x 156mm (Royal 8vo) Case Laminate on White w/Gloss Lam.

  • Language: English

    Published by Springer, 1989

    0792301463 / 9780792301462

    • Hardcover
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    Seller: Biblios, frankfurt am main, HESSE, GermanyBiblios

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    Condition: New. PRINT ON DEMAND pp. 288.

  • Language: English

    Published by Springer Netherlands, Springer Netherlands Mär 1989, 1989

    0792301463 / 9780792301462

    • Hardcover
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    Seller: buchversandmimpf2000, Emtmannsberg, BAYE, Germanybuchversandmimpf2000

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    Buch. Condition: Neu. This item is printed on demand - Print on Demand Titel. Neuware -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.Springer Verlag GmbH, Tiergartenstr. 17, 69121 Heidelberg 288 pp. Englisch.