Monitoring of the Spatio-Temporal Dynamics of the Floods in the Guayas Watershed (Ecuadorian Pacific Coast) Using Global Monitoring ENVISAT ASAR Images and Rainfall Data

被引:13
|
作者
Frappart, Frederic [1 ,2 ]
Bourrel, Luc [1 ]
Brodu, Nicolas [3 ]
Riofrio Salazar, Ximena [1 ,4 ]
Baup, Frederic [5 ]
Darrozes, Jose [1 ]
Pombosa, Rodrigo [6 ]
机构
[1] OMP, CNRS IRD UPS, UMR 5563, GET, 14 Ave Edouard Belin, F-31400 Toulouse, France
[2] OMP, CNRS IRD UPS, UMR 5566, LEGOS, 14 Ave Edouard Belin, F-31400 Toulouse, France
[3] Inria Bordeaux Sud Ouest, Geostat, 200 Ave Vieille Tour, F-33405 Talence, France
[4] Secretaria Educ Super Ciencia & Tecnol SENESCYT, Whymper E7-37 & Alpallana, Quito 170516, Ecuador
[5] OMP, UPS CNRS IRD CNES, UMR5126, Ctr Etud Spatiales BIOsphere CESBIO, 14 Ave Edouard Belin, F-31400 Toulouse, France
[6] Inst Nacl Meteorol & Hidrol INAMHI, Inaquito N36-14 & Corea, Quito 160310, Ecuador
关键词
flood; SAR; ENVISAT ASAR; rainfall; Guayas; Ecuadorian Pacific slope; SURFACE SOIL-MOISTURE; RIVER-BASIN; TIME-SERIES; SAR DATA; WETLANDS; PRECIPITATION; INUNDATION; NORTHERN; RADAR; MODE;
D O I
10.3390/w9010012
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The floods are an annual phenomenon on the Pacific Coast of Ecuador and can become devastating during El Nino years, especially in the Guayas watershed (32,300 km(2)), the largest drainage basin of the South American western side of the Andes. As limited information on flood extent in this basin is available, this study presents a monitoring of the spatio-temporal dynamics of floods in the Guayas Basin, between 2005 and 2008, using a change detection method applied to ENVISAT ASAR Global Monitoring SAR images acquired at a spatial resolution of 1 km. The method is composed of three steps. First, a supervised classification was performed to identify pixels of open water present in the Guayas Basin. Then, the separability of their radar signature from signatures of other classes was determined during the four dry seasons from 2005 to 2008. In the end, standardized anomalies of backscattering coefficient were computed during the four wet seasons of the study period to detect changes between dry and wet seasons. Different thresholds were tested to identify the flooded areas in the watershed using external information from the Dartmouth Flood Observatory. A value of -2.30 +/- 0.05 was found suitable to estimate the number of inundated pixels and limit the number of false detection (below 10%). Using this threshold, monthly maps of inundation were estimated during the wet season (December to May) from 2004 to 2008. The most frequently inundated areas were found to be located along the Babahoyo River, a tributary in the east of the basin. Large interannual variability in the flood extent is observed at the flood peak (from 50 to 580 km(2)), consistent with the rainfall in the Guayas watershed during the study period.
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页数:20
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