Permanent Water Bodies Mapping in the Mekong River Delta Using Seasonal Time Series C-band SAR Data

Microwave remote sensing or SAR (Synthetic Aperture Radar) data has been employed extensively to map open water bodies and to monitor flood extents, where cloud cover often prohibits the use of satellite sensors operating at other wavelengths. Where total inundation occurs, a low backscatter return...

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Main Authors: Nguyễn, Bá Duy, Trần, Thị Hương Giang
Format: Article
Language:English
Published: H.: ĐHQGHN 2016
Subjects:
SAR
Online Access:http://repository.vnu.edu.vn/handle/VNU_123/4482
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Institution: Vietnam National University, Hanoi
Language: English
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spelling oai:112.137.131.14:VNU_123-44822020-07-03T08:17:28Z Permanent Water Bodies Mapping in the Mekong River Delta Using Seasonal Time Series C-band SAR Data Nguyễn, Bá Duy Trần, Thị Hương Giang Water bodies mapping SAR Time series analysis Microwave remote sensing or SAR (Synthetic Aperture Radar) data has been employed extensively to map open water bodies and to monitor flood extents, where cloud cover often prohibits the use of satellite sensors operating at other wavelengths. Where total inundation occurs, a low backscatter return is expected due to the specular reflection of SAR signal on the water surface. However, low local incidence angle and wind induced waves can cause a roughening of the water surface which result in a high return signal. It is also mean that the temporal variability (TV) of the backscatter from water bodies is higher than other land surfaces. The Mekong River Delta is a region with very long wet season (starting in May and lasting until October-November), resulting in almost crop fields also has low backscatter returns. Where such conditions occur adjacent to open water, this can make the separation of water and land problematic using SAR data. In this paper, we use seasonal time series C-band SAR data (dry season), we also examine how the variability in radar backscatter with incidence angle may be used to differentiate water from land overcoming. We carry out regression over multiple sets of seasonal time series data, determined by a moving window encompassing consecutively-acquired ENVISAT ASAR Wide Swath Mode data, to derive three backscatter model parameters: the slope β of a linear model fitting backscatter against local incidence angle; the backscatter normalized at 50° using the linear model coefficients o(50o), and the minimum backscatter (MiB) from time series data after normalized. A comparison of the three parameters (β, TV and MiB) shows that MiB in combination with TV provides the most robust means to segregate water from land by a simple thresholding algorithm. 2016-01-08T03:40:01Z 2016-01-08T03:40:01Z 2015 Article tr. 1-14 0866-8612 http://repository.vnu.edu.vn/handle/VNU_123/4482 en Tập 31;Số 3 application/pdf H.: ĐHQGHN
institution Vietnam National University, Hanoi
building VNU Library & Information Center
country Vietnam
collection VNU Digital Repository
language English
topic Water bodies mapping
SAR
Time series analysis
spellingShingle Water bodies mapping
SAR
Time series analysis
Nguyễn, Bá Duy
Trần, Thị Hương Giang
Permanent Water Bodies Mapping in the Mekong River Delta Using Seasonal Time Series C-band SAR Data
description Microwave remote sensing or SAR (Synthetic Aperture Radar) data has been employed extensively to map open water bodies and to monitor flood extents, where cloud cover often prohibits the use of satellite sensors operating at other wavelengths. Where total inundation occurs, a low backscatter return is expected due to the specular reflection of SAR signal on the water surface. However, low local incidence angle and wind induced waves can cause a roughening of the water surface which result in a high return signal. It is also mean that the temporal variability (TV) of the backscatter from water bodies is higher than other land surfaces. The Mekong River Delta is a region with very long wet season (starting in May and lasting until October-November), resulting in almost crop fields also has low backscatter returns. Where such conditions occur adjacent to open water, this can make the separation of water and land problematic using SAR data. In this paper, we use seasonal time series C-band SAR data (dry season), we also examine how the variability in radar backscatter with incidence angle may be used to differentiate water from land overcoming. We carry out regression over multiple sets of seasonal time series data, determined by a moving window encompassing consecutively-acquired ENVISAT ASAR Wide Swath Mode data, to derive three backscatter model parameters: the slope β of a linear model fitting backscatter against local incidence angle; the backscatter normalized at 50° using the linear model coefficients o(50o), and the minimum backscatter (MiB) from time series data after normalized. A comparison of the three parameters (β, TV and MiB) shows that MiB in combination with TV provides the most robust means to segregate water from land by a simple thresholding algorithm.
format Article
author Nguyễn, Bá Duy
Trần, Thị Hương Giang
author_facet Nguyễn, Bá Duy
Trần, Thị Hương Giang
author_sort Nguyễn, Bá Duy
title Permanent Water Bodies Mapping in the Mekong River Delta Using Seasonal Time Series C-band SAR Data
title_short Permanent Water Bodies Mapping in the Mekong River Delta Using Seasonal Time Series C-band SAR Data
title_full Permanent Water Bodies Mapping in the Mekong River Delta Using Seasonal Time Series C-band SAR Data
title_fullStr Permanent Water Bodies Mapping in the Mekong River Delta Using Seasonal Time Series C-band SAR Data
title_full_unstemmed Permanent Water Bodies Mapping in the Mekong River Delta Using Seasonal Time Series C-band SAR Data
title_sort permanent water bodies mapping in the mekong river delta using seasonal time series c-band sar data
publisher H.: ĐHQGHN
publishDate 2016
url http://repository.vnu.edu.vn/handle/VNU_123/4482
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