2011
DOI: 10.1080/01431160903464112
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Quality analysis of SRTM and HYDRO1K: a case study of flood inundation in Mozambique

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Cited by 23 publications
(19 citation statements)
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“…Therefore they are useful sources of topographic data, especially for low-lying coastal areas with gentle slopes (Gorokhovich and Voustianiouk, 2006;Schumann et al, 2008), and consequently applicable for inundation modelling (Karlsson and Arnberg, 2011). Figure 4 shows results of flood modelling undertaken for the lower Niger River (Nigeria) using SRTM 30 and 90 m. The Niger River overflowed its banks in 2007 and flooded a large part of the floodplain.…”
Section: Altimetrymentioning
confidence: 99%
“…Therefore they are useful sources of topographic data, especially for low-lying coastal areas with gentle slopes (Gorokhovich and Voustianiouk, 2006;Schumann et al, 2008), and consequently applicable for inundation modelling (Karlsson and Arnberg, 2011). Figure 4 shows results of flood modelling undertaken for the lower Niger River (Nigeria) using SRTM 30 and 90 m. The Niger River overflowed its banks in 2007 and flooded a large part of the floodplain.…”
Section: Altimetrymentioning
confidence: 99%
“…Assim, a rede de drenagem pode ser modelada incorretamente em áreas com abundância dessas feições. Karlsson & Arnberg (2011) afirmam que um dos maiores erros nos dados do SRTM é a presença de vegetação.…”
Section: Figura 5 Dados Resultantes Da Classificação Semissupervisiounclassified
“…Hydro 1k data sets are currently being developed individually for each continent. The absolute vertical accuracy for HYDRO1k data, a hydrologically modified version of the elevation model GTOPO30, is not specified officially, but GTOPO30 has a vertical accuracy of 39 m in terms of linear error at the 90% confidence level, corresponding to a root mean square error of 18 m over the area of interest [41]. The Lambert Azimuthal Equal Area projection was selected for this data.…”
Section: Dem and In Situ Datamentioning
confidence: 99%