Flood Proxy Mapping with Normalized Difference Sigma-Naught Index and Shannon’s Entropy

Rainfall-induced floods often cause significant loss of life as well as damage to infrastructure and crops. Synthetic Aperture Radar (SAR) Earth Observation Satellites (EOS) can be used to determine the extent of flooding over large geographical areas. Unlike optical sensors, SAR instruments are sui...

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Main Authors: Noel Ivan Ulloa, Shou-Hao Chiang, Sang-Ho Yun
Format: Article
Language:English
Published: MDPI AG 2020-04-01
Series:Remote Sensing
Subjects:
Online Access:https://www.mdpi.com/2072-4292/12/9/1384
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author Noel Ivan Ulloa
Shou-Hao Chiang
Sang-Ho Yun
author_facet Noel Ivan Ulloa
Shou-Hao Chiang
Sang-Ho Yun
author_sort Noel Ivan Ulloa
collection DOAJ
description Rainfall-induced floods often cause significant loss of life as well as damage to infrastructure and crops. Synthetic Aperture Radar (SAR) Earth Observation Satellites (EOS) can be used to determine the extent of flooding over large geographical areas. Unlike optical sensors, SAR instruments are suitable for cloudy weather conditions, making them suitable for flood detection and mapping during extreme weather events. In this study, we explore the application of the Normalized Difference Sigma-Naught Index (NDSI) and Shannon’s entropy of NDSI (SNDSI) of Sentinel-1 data for open water flooding detection, based on automatic thresholding and Bayesian probability. The proposed methodology was tested using the floods in Sofala province, Mozambique, caused by cyclone Idai on March 14–19 of 2019. Results show that thresholding of the NDSI Vertical Transmit-Horizontal Receive (VH) can produce results with Overall Accuracy above 90%, and Kappa higher than 0.6. Considerable performance improvements were obtained by our thresholding method over the entropy of NDSI, yielding results with Kappa of 0.70–0.77. Additionally, it was found that Weibull distribution can properly describe the properties of flooded pixels within the histogram of SNDSI, which allows us to generate a flood probability raster using a Bayesian approach. The final per-pixel flooding probability is useful to indicate certainty in the classification results. The SNDSI Bayesian model produced an AUC (Area Under the Receiver Operating Characteristic Curve) of 0.93–0.97, with cross-polarized data yielding the most accurate results.
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spelling doaj.art-6a324734f3a649ce81209fa24e74e1172023-11-19T22:52:00ZengMDPI AGRemote Sensing2072-42922020-04-01129138410.3390/rs12091384Flood Proxy Mapping with Normalized Difference Sigma-Naught Index and Shannon’s EntropyNoel Ivan Ulloa0Shou-Hao Chiang1Sang-Ho Yun2Department of Civil Engineering, National Central University, Taoyuan City 32001, TaiwanDepartment of Civil Engineering, National Central University, Taoyuan City 32001, TaiwanNASA Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA 91109, USARainfall-induced floods often cause significant loss of life as well as damage to infrastructure and crops. Synthetic Aperture Radar (SAR) Earth Observation Satellites (EOS) can be used to determine the extent of flooding over large geographical areas. Unlike optical sensors, SAR instruments are suitable for cloudy weather conditions, making them suitable for flood detection and mapping during extreme weather events. In this study, we explore the application of the Normalized Difference Sigma-Naught Index (NDSI) and Shannon’s entropy of NDSI (SNDSI) of Sentinel-1 data for open water flooding detection, based on automatic thresholding and Bayesian probability. The proposed methodology was tested using the floods in Sofala province, Mozambique, caused by cyclone Idai on March 14–19 of 2019. Results show that thresholding of the NDSI Vertical Transmit-Horizontal Receive (VH) can produce results with Overall Accuracy above 90%, and Kappa higher than 0.6. Considerable performance improvements were obtained by our thresholding method over the entropy of NDSI, yielding results with Kappa of 0.70–0.77. Additionally, it was found that Weibull distribution can properly describe the properties of flooded pixels within the histogram of SNDSI, which allows us to generate a flood probability raster using a Bayesian approach. The final per-pixel flooding probability is useful to indicate certainty in the classification results. The SNDSI Bayesian model produced an AUC (Area Under the Receiver Operating Characteristic Curve) of 0.93–0.97, with cross-polarized data yielding the most accurate results.https://www.mdpi.com/2072-4292/12/9/1384flood proxy mappingSynthetic Aperture RadarNormalized Difference Sigma-Naught IndexBayesian probabilityShannon’s entropy
spellingShingle Noel Ivan Ulloa
Shou-Hao Chiang
Sang-Ho Yun
Flood Proxy Mapping with Normalized Difference Sigma-Naught Index and Shannon’s Entropy
Remote Sensing
flood proxy mapping
Synthetic Aperture Radar
Normalized Difference Sigma-Naught Index
Bayesian probability
Shannon’s entropy
title Flood Proxy Mapping with Normalized Difference Sigma-Naught Index and Shannon’s Entropy
title_full Flood Proxy Mapping with Normalized Difference Sigma-Naught Index and Shannon’s Entropy
title_fullStr Flood Proxy Mapping with Normalized Difference Sigma-Naught Index and Shannon’s Entropy
title_full_unstemmed Flood Proxy Mapping with Normalized Difference Sigma-Naught Index and Shannon’s Entropy
title_short Flood Proxy Mapping with Normalized Difference Sigma-Naught Index and Shannon’s Entropy
title_sort flood proxy mapping with normalized difference sigma naught index and shannon s entropy
topic flood proxy mapping
Synthetic Aperture Radar
Normalized Difference Sigma-Naught Index
Bayesian probability
Shannon’s entropy
url https://www.mdpi.com/2072-4292/12/9/1384
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