

FOLLOWUS
1. University of Chinese Academy of Sciences
2. Institute of Geodesy and Geophysics Chinese Academy of Sciences Key Laboratory for Environment and Disaster Monitoring and Evaluation
网络首发:2014-05-04,
纸质出版:2014
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Construction of lake bathymetry from MODIS satellite data and GIS from 2003 to 2011[J]. 海洋湖沼学报(英文), 2014,32(3):720-731.
Yan, Y., Xiao, F. & Du, Y. Construction of lake bathymetry from MODIS satellite data and GIS from 2003 to 2011., Chin. J. Ocean. Limnol. 32, 720–731 (2014). https://doi.org/10.1007/s00343-014-3185-4
Construction of lake bathymetry from MODIS satellite data and GIS from 2003 to 2011[J]. 海洋湖沼学报(英文), 2014,32(3):720-731. DOI: 10.1007/s00343-014-3185-4.
Yan, Y., Xiao, F. & Du, Y. Construction of lake bathymetry from MODIS satellite data and GIS from 2003 to 2011., Chin. J. Ocean. Limnol. 32, 720–731 (2014). https://doi.org/10.1007/s00343-014-3185-4 DOI:
In recent years
sedimentation conditions in Dongting Lake have varied greatly because of signifi cant changes in runoff and sediment load in the Changjiang (Yangtze) River following the construction of Three Gorges Dam. The topography of the lake bottom has changed rapidly because of the intense exchange of water and sediment between the lake and the Changjiang River. However
time series information on lake-bottom topographic change is lacking. In this study
we introduced a method that combines remote sensing data and in situ water level data to extract a record of Dongting Lake bottom topography from 2003 to 2011. Multi-temporal lake land/water boundaries were extracted from MODIS images using the linear spectral mixture model method. The elevation of water/land boundary points were calculated using water level data and spatial interpolation techniques. Digital elevation models of Dongting Lake bottom topography in different periods were then constructed with the multiple heighted waterlines. The mean root-mean-square error of the linear spectral mixture model was 0.036
and the mean predicted error for elevation interpolation was −0.19 m. Compared with fi eld measurement data and sediment load data
the method has proven to be most applicable. The results show that the topography of the bottom of Dongting Lake has exhibited uneven erosion and deposition in terms of time and space over the last nine years. Moreover
lake-bottom topography has undergone a slight erosion trend within this period
with 58.2% and 41.8% of the lake-bottom area being eroded and deposited
respectively.
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