Isbn: 9786202060325 - effectiveness of digital elevation models in the barotse floodplain, zambia:: effectiveness of digital elevation models (9 resultados)

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  • Idioma: Inglés

    Editorial: LAP LAMBERT Academic Publishing, 2018

    6202060328 / 9786202060325

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    Librería: Books Puddle, Woodside, NY, Estados Unidos de AmericaBooks Puddle

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    Cantidad disponible: 4 disponibles

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  • Idioma: Inglés

    Editorial: LAP LAMBERT Academic Publishing, 2018

    6202060328 / 9786202060325

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    Librería: Revaluation Books, Exeter, Reino UnidoRevaluation Books

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    Paperback. Condición: Brand New. 68 pages. 8.66x5.91x0.16 inches. In Stock.

  • Idioma: Inglés

    Editorial: LAP LAMBERT Academic Publishing, 2018

    6202060328 / 9786202060325

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    Librería: preigu, Osnabrück, Alemaniapreigu

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    Taschenbuch. Condición: Neu. Effectiveness of Digital Elevation Models in the Barotse Floodplain, Zambia: | Effectiveness of digital elevation models | Elias Awol Mohammed | Taschenbuch | 68 S. | Englisch | 2018 | LAP LAMBERT Academic Publishing | EAN 9786202060325 | Verantwortliche Person für die EU: preigu GmbH & Co. KG, Lengericher Landstr. 19, 49078 Osnabrück, mail[at]preigu[dot]de | Anbieter: preigu.…

  • Idioma: Inglés

    Editorial: LAP LAMBERT Academic Publishing Apr 2018, 2018

    6202060328 / 9786202060325

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    Librería: BuchWeltWeit Ludwig Meier e.K., Bergisch Gladbach, AlemaniaBuchWeltWeit Ludwig Meier e.K.

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    Taschenbuch. Condición: Neu. This item is printed on demand - it takes 3-4 days longer - Neuware -The extensive Barotse floodplain in western Zambia is among the most flood prone area. This study focused on hydrodynamic flood modeling to simulate flood inundation characteristics that will benefit provision of recession farming, canal management, and land use planning in the Barotse floodplain. For this study the one-dimensional hydrodynamic model (HEC-RAS 4.1.), HEC-GeoRAS10 (GIS extension), ARC-GIS 10, and Google Earth are used. The SRTM 30-m, SRTM 90-m, and ASTER 30-m DEMs are first compared to select a better DEM for model simulation. This was done by a visual comparison and through objective functions using SRTM 30-m as reference. The mean elevation deviation of SRTM 90-m ranges from 0 to 1m and STER 30-m ranges from -9 to 3m. SRTM 30-m better captured the channel geometry and the heterogeneity of the floodplain to a certain details. ASTER 30-m as resulted in a somewhat exaggerated elevation of river channel banks. The floodplain terrain slope shows the largest variation in ASTER 30-m and the least variation for the course DEM SRTM 90-m. This study was a first attempt to model the flood dynamics of the complex Brotse floodplain. 68 pp. Englisch.…

  • Idioma: Inglés

    Editorial: LAP LAMBERT Academic Publishing, 2018

    6202060328 / 9786202060325

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    Librería: Majestic Books, Hounslow, Reino UnidoMajestic Books

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    EUR 62,08

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    Cantidad disponible: 4 disponibles

    Condición: New. Print on Demand.

  • Idioma: Inglés

    Editorial: LAP LAMBERT Academic Publishing, 2018

    6202060328 / 9786202060325

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    Librería: AHA-BUCH GmbH, Einbeck, AlemaniaAHA-BUCH GmbH

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    Taschenbuch. Condición: Neu. nach der Bestellung gedruckt Neuware - Printed after ordering - The extensive Barotse floodplain in western Zambia is among the most flood prone area. This study focused on hydrodynamic flood modeling to simulate flood inundation characteristics that will benefit provision of recession farming, canal management, and land use planning in the Barotse floodplain. For this study the one-dimensional hydrodynamic model (HEC-RAS 4.1.), HEC-GeoRAS10 (GIS extension), ARC-GIS 10, and Google Earth are used. The SRTM 30-m, SRTM 90-m, and ASTER 30-m DEMs are first compared to select a better DEM for model simulation. This was done by a visual comparison and through objective functions using SRTM 30-m as reference. The mean elevation deviation of SRTM 90-m ranges from 0 to 1m and STER 30-m ranges from -9 to 3m. SRTM 30-m better captured the channel geometry and the heterogeneity of the floodplain to a certain details. ASTER 30-m as resulted in a somewhat exaggerated elevation of river channel banks. The floodplain terrain slope shows the largest variation in ASTER 30-m and the least variation for the course DEM SRTM 90-m. This study was a first attempt to model the flood dynamics of the complex Brotse floodplain.…

  • Idioma: Inglés

    Editorial: LAP LAMBERT Academic Publishing, 2018

    6202060328 / 9786202060325

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    Librería: Biblios, frankfurt am main, HESSE, AlemaniaBiblios

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    EUR 62,54

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    Condición: New. PRINT ON DEMAND.

  • Idioma: Inglés

    Editorial: LAP LAMBERT Academic Publishing, 2018

    6202060328 / 9786202060325

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    Librería: moluna, Greven, Alemaniamoluna

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    Condición: New. Dieser Artikel ist ein Print on Demand Artikel und wird nach Ihrer Bestellung fuer Sie gedruckt. Autor/Autorin: Mohammed Elias Awol*Name: Mr. Elias Awol Mohammed *Profession: Soil and Water, Irrigation Engineering *Work experience: Soil and water conservation, Water harvesting, Irrigation, Climate, Land administration, Soil fertility and Techn. …

  • Idioma: Inglés

    Editorial: LAP LAMBERT Academic Publishing Apr 2018, 2018

    6202060328 / 9786202060325

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    Librería: buchversandmimpf2000, Emtmannsberg, BAYE, Alemaniabuchversandmimpf2000

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    EUR 35,90

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    Taschenbuch. Condición: Neu. This item is printed on demand - Print on Demand Titel. Neuware -The extensive Barotse floodplain in western Zambia is among the most flood prone area. This study focused on hydrodynamic flood modeling to simulate flood inundation characteristics that will benefit provision of recession farming, canal management, and land use planning in the Barotse floodplain. For this study the one-dimensional hydrodynamic model (HEC-RAS 4.1.), HEC-GeoRAS10 (GIS extension), ARC-GIS 10, and Google Earth are used. The SRTM 30-m, SRTM 90-m, and ASTER 30-m DEMs are first compared to select a better DEM for model simulation. This was done by a visual comparison and through objective functions using SRTM 30-m as reference. The mean elevation deviation of SRTM 90-m ranges from 0 to 1m and STER 30-m ranges from -9 to 3m. SRTM 30-m better captured the channel geometry and the heterogeneity of the floodplain to a certain details. ASTER 30-m as resulted in a somewhat exaggerated elevation of river channel banks. The floodplain terrain slope shows the largest variation in ASTER 30-m and the least variation for the course DEM SRTM 90-m. This study was a first attempt to model the flood dynamics of the complex Brotse floodplain.VDM Verlag, Dudweiler Landstraße 99, 66123 Saarbrücken 68 pp. Englisch.…