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Coastal flooding normally occurs when dry and low-lying land is submerged by seawater. The range of a coastal flooding is a result of the elevation of floodwater that penetrates the inland which is controlled by the topography of the coastal land exposed to flooding. Flood damage modelling was limited to local, regional or national scales. However, with the presence of climate change and an increase in the population rates, flood events have intensified and called for a global interest in finding out different methods with both spatial and temporal dynamics.

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rdfs:label
  • Coastal flooding (en)
  • Banjir rob (in)
  • Submersion marine (fr)
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  • Coastal flooding normally occurs when dry and low-lying land is submerged by seawater. The range of a coastal flooding is a result of the elevation of floodwater that penetrates the inland which is controlled by the topography of the coastal land exposed to flooding. Flood damage modelling was limited to local, regional or national scales. However, with the presence of climate change and an increase in the population rates, flood events have intensified and called for a global interest in finding out different methods with both spatial and temporal dynamics. (en)
  • Banjir rob adalah banjir di tepi pantai karena permukaan air laut yang lebih tinggi daripada bibir pantai atau daratan di pesisir pantai. Banjir rob secara khusus diartikan sebagai banjir yang diakibatkan oleh air laut yang menggenangi daratan yang lebih rendah, tetapi sebenarnya tidak terbatas pada banjir yang berakibat oleh air laut melainkan juga curah hujan tinggi di daratan yang menyebabkan air melambat mengalir ke laut yang hasilnya akan mengakibatkan air tertahan dalam waktu yang relatif lama di daratan pesisir pantai. Fenomena ini juga diperparah oleh kondisi pasang naik air laut di waktu-waktu tertentu. Permasalahan banjir rob merupakan permasalahan serius yang dihadapi beberapa wilayah pesisir di Indonesia seperti pesisir utara Pulau Jawa, pesisir timur Sumatera Utara, pesisir pa (in)
  • Une submersion marine est une inondation temporaire et éventuellement épisodique de zone côtière, générée par la mer voisine, avec de l'eau salée ou saumâtre, lors d’évènements météorologiques (tempête, cyclone tropical, forte dépression et vent de mer) ou océanographiques (houle, marée, tsunami) d’ampleur très inhabituelle. Elle commence lorsque les plus hauts jets d'eau de mer de la bordure maritime dépassent la crête des accumulations littorales provoquant un transfert d'eau et parfois de sédiments sur le versant terre du cordon littoral. (fr)
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  • http://commons.wikimedia.org/wiki/Special:FilePath/KatrinaNewOrleansFlooded_edit2.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Mangroves.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Lili2002coastalflooding.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Hurricane_Carol_Storm_Surge_in_color_1954.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/US_Navy_050102-N-9593M-040_A_village_near_the_coast_of_Sumatra_lays_in_ruin_after_the_Tsunami_that_struck_South_East_Asia.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/53sitges.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Major_cities_threatened_by_sea_level_rise.png
  • http://commons.wikimedia.org/wiki/Special:FilePath/NASA-Satellite-sea-level-rise-observations.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Thames.barrier.5.london.arp.jpg
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