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Statements

Subject Item
dbr:Coastal_flooding
rdfs:label
Submersion marine Coastal flooding Banjir rob
rdfs:comment
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. 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 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.
foaf:depiction
n5:53sitges.jpg n5:Lili2002coastalflooding.jpg n5:Mangroves.jpg n5:Major_cities_threatened_by_sea_level_rise.png n5:NASA-Satellite-sea-level-rise-observations.jpg n5: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 n5:Hurricane_Carol_Storm_Surge_in_color_1954.jpg n5:Thames.barrier.5.london.arp.jpg n5:KatrinaNewOrleansFlooded_edit2.jpg
dcterms:subject
dbc:Flood dbc:Coasts dbc:Coastal_geography
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n12:4iGcD dbpedia-fa:سیل_ساحلی wikidata:Q5138350 dbpedia-fr:Submersion_marine dbpedia-id:Banjir_rob dbpedia-simple:Coastal_flooding dbpedia-tr:Kıyı_taşkını
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dbo:thumbnail
n5:Lili2002coastalflooding.jpg?width=300
dbp:align
right
dbp:caption
Satellite observations of sea level rise since 1993 Major cities threatened by sea level rise. The cities indicated are under threat of even a small sea level rise compared to the level in 2010. Even moderate projections indicate that such a rise will have occurred by 2060.
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horizontal
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Major cities threatened by sea level rise.png NASA-Satellite-sea-level-rise-observations.jpg
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dbo:abstract
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 pantai Kalimantan Barat dan Selatan. Faktor utama yang mengakibatkan terjadinya banjir rob adalah kenaikan permukaan air laut, penurunan muka tanah dan abrasi pantai dalam hal ini di daratan pesisir. Penurunan muka tanah merupakan faktor yang meningkatkan intensitas banjir rob di beberapa wilayah pesisir pantai utara Pulau Jawa terutama di DKI Jakarta, Bekasi, Karawang, Pekalongan, Semarang, Demak dan Gresik. 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. La capacité de ce risque naturel à engendrer des modifications du trait de cote dépend beaucoup de l'énergie des vagues déversantes. Les brèches pouvant être ainsi créées dans les dunes ou les digues littorales sont souvent déterminantes dans l'ampleur du phénomène. La submersion marine se distingue de la transgression marine surtout par son aspect éphémère (quelques heures / jours). À l'échelle des temps géologiques, une succession de submersions marines de plus en plus envahissantes indique une transgression marine. Ce risque est aggravé par la montée de la mer due au changement climatique. 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. The seawater can flood the land via several different paths: direct flooding, overtopping of a barrier, breaching of a barrier. Coastal flooding is largely a natural event, however human influence on the coastal environment can exacerbate coastal flooding. Extraction of water from groundwater reservoirs in the coastal zone can instigate subsidence of the land, thus increasing the risk of flooding. Engineered protection structures along the coast such as sea walls alter the natural processes of the beach, often leading to erosion on adjacent stretches of the coast which also increases the risk of flooding. Moreover, sea level rise and extreme weather caused by climate change will increase the intensity and amount of coastal flooding affecting hundreds of millions of people.
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