{"refrec":{"BRefID":205479,"RR":"<b>Baeteman, C.</b> (2010). Geological considerations on the effect of sea-level rise on coastal lowlands, in particular in developing countries = Geologische bedenkingen betreffende de invloed van de zeespiegelstijging in lage kustgebieden, in het bijzonder in ontwikkelingslanden. <i>Meded. Zitt. K. Acad. Overzeese Wet. = Bull. séances Acad. r. sci. O.-m. 56(2)</i>: 195-207","BEntID":197609,"PublicFlag":1,"CheckedFlag":0,"wosflag":0,"vabbflag":null,"RefStringPartII":". <i>Meded. Zitt. K. Acad. Overzeese Wet. = Bull. Séances Acad. r. sci. O.-m. 56(2)</i>: 195-207","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Baeteman, C.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Baeteman, C.","Englishabstract":"The coastal lowlands of developing countries in particular are among the most densely populated and economically productive. Therefore, it is essential to get a realistic appraisal of the likely response of these areas to the predicted sea-level rise due to global warming. A short review of the different factors causing sea-level rise is presented and shows that the conception of global sea level must be abandoned. The method - ol ogies used to assess the impact of a sea-level rise are critically evaluated whereby it is noticed that the coastal processes and the controlling factors are not sufficiently considered. The geological history of the last 10,000 years of deltas and estuaries provides an analogue of the way coastal lowlands may respond to the predicted sea-level rise, and indic ates that these areas will be able to keep pace with the predicted rate of sea-level rise providing that sufficient sediment is continuously available and dikes are absent. The high rate of human-induced subsidence in big cities is a far more devastating problem than the effects of sea-level rise.  ","AbstractOtherLang":"De lage kustgebieden in de ontwikkelingslanden behoren tot de dichts bevolkte gebieden met grote economische productiviteit. Daarom is het essentieel om een realistisch beeld te hebben van de mogelijke reactie van deze gebieden op de voorspelde zeespiegelstijging ten gevolge de opwarming van de aarde. Een kort overzicht van de verschillende factoren die een zeespiegelstijging veroorzaken doet besluiten dat het begrip globale zeespiegel moet verlaten worden. De methoden die gebruikt worden om de invloed van een zeespiegelstijging in te schatten worden kritisch geëvalueerd waarbij tot uiting is gekomen dat er onvoldoende rekening gehouden wordt met kustprocessen en de factoren die kustveranderingen bepalen. De geologische geschiedenis van de laatste 10 000 jaar van de deltas en estuaria die kan gebruikt worden als analogie om te achterhalen hoe de lage kustgebieden kunnen veranderen ten gevolge de zeespiegelstijging, toont aan dat deze gebieden gelijke tred kunnen houden met de snelheid van de voorspelde zeespiegelstijging op voorwaarde dat voldoende sediment beschikbaar is en dat dijken geen obstructie vormen. De door de mens veroorzaakte sterke subsidentie in de grote steden vormt een veel groter probleem dan de invloed van een zeespiegelstijging.  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