Assessment of Sentinel-2 and Landsat-8 OLI for Small-Scale Inland Water Quality Modeling and Monitoring Based on Handheld Hyperspectral Ground Truthing

This study investigates the best available methods for remote monitoring inland small-scale waterbodies, using remote sensing data from both Landsat-8 and Sentinel-2 satellites, utilizing a handheld hyperspectral device for ground truthing. Monitoring was conducted to evaluate water quality indicators: chlorophyll-a (Chl-a), colored dissolved organic matter (CDOM), and turbidity. Ground truthing was performed to select the most suitable atmospheric correction technique (ACT). Several ACT have been tested: dark spectrum fitting (DSF), dark object subtraction (DOS), atmospheric and topographic correction (ATCOR), and exponential extrapolation (EXP). Classical sampling was conducted first; then, the resulting concentrations were compared to those obtained using remote sensing analysis by the above-mentioned ACT. This research revealed that DOS and DSF achieved the best performance (an advantage ranging between 29% and 47%). Further, we demonstrated the appropriateness of the use of Sentinel-2 red and vegetation red edge reciprocal bands (1/(B4 X B6)) for estimating Chl-a (R2 = 0.82, RMSE = 14.52mg/m3). As for Landsat-8, red to near-infrared ratio (B4/B5) produced the best performing model (R2 = 0.71, RMSE = 39.88 mg/m3), but it did not perform as well as Sentinel-2. Regarding turbidity, the best model (with (R2 =0.85, RMSE = 0.87 NTU) obtained by Sentinel-2 utilized a single band (B4), while the best model (with R2 = 0.64, RMSE = 0.90 NTU) using Landsat-8 was performed by applying two bands (B1/B3). Mapping the water quality parameters using the best performance biooptical model showed the significant effect of the adjacent land on the boundary pixels compared to pixels of deeper water

A semi-analytical algorithm for deriving the particle size distribution slope of turbid inland water based on OLCI data: A case study in Lake Hongze

The particle size distribution (PSD) slope (ξ) can indicate the predominant particle size, material composition, and inherent optical properties (IOPs) of inland waters. However, few semi-analytical methods have been proposed for deriving ξ from the surface remote sensing reflectance due to the variable optical state of inland waters. A semi-analytical algorithm was developed for inland waters having a wide range of turbidity and ξ in this study. Application of the proposed model to Ocean and Land Color Instrument (OLCI) imagery of the water body resulted in several important observations: (1) the proposed algorithm (754 nm and 779 nm combination) was capable of retrieving ξ with R2 being 0.72 (p < 0.01, n = 60), and MAPE and RMSE being 4.37% and 0.22 (n = 30) respectively; (2) the ξ in HZL was lower in summer than other seasons during the period considered, this variation was driven by the phenological cycle of algae and the runoff caused by rainfall; (3) the band optimization proposed in this study is important for calculating the particle backscattering slope (η) and deriving ξ because it is feasible for both algae dominant and sediment governed turbid inland lakes. These observations help improve our understanding of the relationship between IOPs and ξ, which are affected by different bio-optic processes and algal phenology in the lake environment

Evaluating Landsat-8 and Sentinel-2 Data Consistency for High Spatiotemporal Inland and Coastal Water Quality Monitoring

The synergy of fine-to-moderate-resolutin (i.e., 10–60 m) satellite data of the Landsat-8 Operational Land Imager (OLI) and the Sentinel-2 Multispectral Instrument (MSI) provides a possibility to monitor the dynamics of sensitive aquatic systems. However, it is imperative to assess the spectral consistency of both sensors before developing new algorithms for their combined use. This study evaluates spectral consistency between OLI and MSI-A/B, mainly in terms of the topof-atmosphere reflectance (ρt), Rayleigh-corrected reflectance (ρrc), and remote-sensing reflectance (Rrs). To check the spectral consistency under various atmospheric and aquatic conditions, nearsimultaneous same-day overpass images of OLI and MSI-A/B were selected over diverse coastal and inland areas across Mainland China and Hong Kong. The results showed that spectral data obtained from OLI and MSI-A/B were consistent. The difference in the mean absolute percentage error (MAPE) of the OLI and MSI-A products was ~8% in ρt and ~10% in both ρrc and Rrs for all the matching bands, whereas the MAPE for OLI and MSI-B was ~3.7% in ρt , ~5.7% in ρrc, and ~7.5% in Rrs for all visible bands except the ultra-blue band. Overall, the green band was the most consistent, with the lowest MAPE of ≤ 4.6% in all the products. The linear regression model suggested that product difference decreased significantly after band adjustment with the highest reduction rate in Rrs (NIR band) and Rrs (red band) for the OLI–MSI-A and OLI–MSI-B comparison, respectively. Further, this study discussed the combined use of OLI and MSI-A/B data for (i) time series of the total suspended solid concentrations (TSS) over coastal and inland waters; (ii) floating algae area comparison; and (iii) tracking changes in coastal floating algae (FA). Time series analysis of the TSS showed that seasonal variation was well-captured by the combined use of sensors. The analysis of the floating algae bloom area revealed that the algae area was consistent, however, the difference increases as the time difference between the same-day overpasses increases. Furthermore, tracking changes in coastal FA over two months showed that thin algal slicks (width < 500 m) can be detected with an adequate spatial resolution of the OLI and the MSI

Research trends in the use of remote sensing for inland water quality science: Moving towards multidisciplinary applications

Remote sensing approaches to measuring inland water quality date back nearly 50 years to the beginning of the satellite era. Over this time span, hundreds of peer-reviewed publications have demonstrated promising remote sensing models to estimate biological, chemical, and physical properties of inland waterbodies. Until recently, most of these publications focused largely on algorithm development as opposed to implementation of those algorithms to address specific science questions. This slow evolution contrasts with terrestrial and oceanic remote sensing, where methods development in the 1970s led to publications focused on understanding spatially expansive, complex processes as early as the mid-1980s. This review explores the progression of inland water quality remote sensing from methodological development to scientific applications. We use bibliometric analysis to assess overall patterns in the field and subsequently examine 236 key papers to identify trends in research focus and scale. The results highlight an initial 30 year period where the majority of publications focused on model development and validation followed by a spike in publications, beginning in the early-2000s, applying remote sensing models to analyze spatiotemporal trends, drivers, and impacts of changing water quality on ecosystems and human populations. Recent and emerging resources, including improved data availability and enhanced processing platforms, are enabling researchers to address challenging science questions and model spatiotemporally explicit patterns in water quality. Examination of the literature shows that the past 10-15 years has brought about a focal shift within the field, where researchers are using improved computing resources, datasets, and operational remote sensing algorithms to better understand complex inland water systems. Future satellite missions promise to continue these improvements by providing observational continuity with spatial/spectral resolutions ideal for inland waters

Remote sensing and bio-geo-optical properties of turbid, productive inland waters: a case study of Lake Balaton

Algal blooms plague freshwaters across the globe, as increased nutrient loads lead to eutrophication of inland waters and the presence of potentially harmful cyanobacteria. In this context, remote sensing is a valuable approach to monitor water quality over broad temporal and spatial scales. However, there remain several challenges to the accurate retrieval of water quality parameters, and the research in this thesis investigates these in an optically complex lake (Lake Balaton, Hungary). This study found that bulk and specific inherent optical properties [(S)IOPs] showed significant spatial variability over the trophic gradient in Lake Balaton. The relationships between (S)IOPs and biogeochemical parameters differed from those reported in ocean and coastal waters due to the high proportion of particulate inorganic matter (PIM). Furthermore, wind-driven resuspension of mineral sediments attributed a high proportion of total attenuation to particulate scattering and increased the mean refractive index (n̅p) of the particle assemblage. Phytoplankton pigment concentrations [chlorophyll-a (Chl-a) and phycocyanin (PC)] were also accurately retrieved from a times series of satellite data over Lake Balaton using semi-analytical algorithms. Conincident (S)IOP data allowed for investigation of the errors within these algorithms, indicating overestimation of phytoplankton absorption [aph(665)] and underestimation of the Chl-a specific absorption coefficient [a*ph(665)]. Finally, Chl-a concentrations were accurately retrieved in a multiscale remote sensing study using the Normalized Difference Chlorophyll Index (NDCI), indicating hyperspectral data is not necessary to retrieve accurate pigment concentrations but does capture the subtle heterogeneity of phytoplankton spatial distribution. The results of this thesis provide a positive outlook for the future of inland water remote sensing, particularly in light of contemporary satellite instruments with continued or improved radiometric, spectral, spatial and temporal coverage. Furthermore, the value of coincident (S)IOP data is highlighted and contributes towards the improvement of remote sensing pigment retrieval in optically complex waters

Detection and Monitoring of Marine Pollution Using Remote Sensing Technologies

Recently, the marine habitat has been under pollution threat, which impacts many human activities as well as human life. Increasing concerns about pollution levels in the oceans and coastal regions have led to multiple approaches for measuring and mitigating marine pollution, in order to achieve sustainable marine water quality. Satellite remote sensing, covering large and remote areas, is considered useful for detecting and monitoring marine pollution. Recent developments in sensor technologies have transformed remote sensing into an effective means of monitoring marine areas. Different remote sensing platforms and sensors have their own capabilities for mapping and monitoring water pollution of different types, characteristics, and concentrations. This chapter will discuss and elaborate the merits and limitations of these remote sensing techniques for mapping oil pollutants, suspended solid concentrations, algal blooms, and floating plastic waste in marine waters

Changes of water clarity in large lakes and reservoirs across China observed from long-term MODIS

Water clarity is a well-established first-order indicator of water quality and has been used globally by water regulators in their monitoring and management programs. Assessments of water clarity in lakes over large temporal and spatial scales, however, are rare, limiting our understanding of its variability and the driven forces. In this study, we developed and validated a robust Secchi disk depth (ZSD) algorithm for lakes across China based on two water color parameters, namely Forel-Ule Index (FUI) and hue angle α, retrieved from MODIS data. The MODIS ZSD model shows good results when compared with in-situ measurements from 17 lakes, with a 27.4% mean relative difference (MRD) in the validation dataset. Compared with other empirical ZSD models, our FUI and α-based model demonstrates improved performance and adaptability over a wide range of water clarity and trophic states. This algorithm was subsequently applied to MODIS measurements to provide a comprehensive assessment of water clarity in large lakes (N = 153) across China for the first time. The mean summer ZSD of the studied lakes between 2000 and 2017 demonstrated marked spatial and temporal variations. Spatially, the ZSD of large lakes presented a distinct spatial pattern of “high west and low east” over China. This spatial pattern was found to be associated with the significant differences in lake depth and altitude between west and east China while China's population, GDP, temperature, and precipitation distribution have also contributed to a certain extent. Temporally, the ZSD of most lakes increased during this period, with an overall mean rate of 3.3 cm/yr for all lakes. Here, 38.6% (N = 59) of the lakes experienced a significant increase in their ZSD value during the past 18 years while only 8.5% (N = 13) showed a significant decreasing trend. Significant increases in lake ZSD were observed in west China, which were found to correlate with the increase of air temperature and lake surface area. This is possibly a response of the lakes in west China to climate change. In the lake systems of east China, which are predominately used as a drinking water source, the increase in lake ZSD was found to be strongly correlated with changes in local GDP (gross domestic production), NDVI (normalized difference vegetation index) and lake surface area, suggesting a combined effect of the implemented management practices and climatic variability. The results of this study provide important information for water quality conservation and management in China, and also highlight the value of satellite remote sensing in monitoring water quality over lakes at a large scale and long-term

고해상도 초분광영상을 활용한 하천 부유사농도 계측기법 개발

학위논문(박사) -- 서울대학교대학원 : 공과대학 건설환경공학부, 2022. 8. 서일원.기존의 하천 부유사 농도 계측은 샘플링 기반 직접계측 방식에 의존하여 시공간적 고해상도 자료 취득이 어려운 실정이다. 이러한 한계점을 극복하기 위해 최근 위성과 드론을 활용하여 촬영된 다분광 혹은 초분광 영상을 통해 고해상도의 부유사농도 시공간분포를 계측하는 기법에 대한 연구가 활발히 진행되고 있다. 하지만, 다른 하천 물리량 계측에 비해 부유사 계측 연구는 하천에 따라 부유사가 다양하게 분포하고 다른 부유물질 혹은 하상에 의한 바닥 반사의 영향 때문에 분광 자료를 통해 정확한 부유사농도 분포를 재현하기 어려운 실정이다. 특히, 부유사 분광 특성에 영향을 미치는 입도분포, 광물특성, 침강성 등이 하천에 따라 강한 지역성을 나타내기에 이러한 요인에서 야기되는 분광다양성으로 인해 특정 시기와 지역에만 적합한 원격탐사 기반 계측 모형들이 개발되어 왔다. 본 연구에서는 이러한 분광다양성을 반영하여 다양한 하천 및 유사 조건에서 적용 가능한 고해상도 초분광영상을 활용한 하천 부유사농도 계측방법을 개발하기 위해 초분광 군집화 기법과 다양한 파장대의 분광 밴드를 학습할 수 있는 기계학습 회귀 모형을 결합하여 CMR-OV라는 방법론을 제시하였다. CMR-OV 개발 및 검증은 1) 실험적 연구를 통한 하천 부유사 분광 특성의 주요 교란 요인 분석, 2) 최적 회귀모형 선정 및 초분광 클러스터링과의 결합, 3) 현장적용성 평가의 과정을 거쳐 수행되었다. 실험적 연구에서는 우선 실내 실험실에서 횡방향 혼합기를 활용하여 바닥 반사를 제거하고 완전 혼합된 상태에서 부유사의 고유 초분광 스펙트럼 자료를 수집하였다. 이를 바탕으로 실제 하천과 유사한 조건의 실규모 옥외 수로 실험에서 다양한 유사 특성(입도 및 광물)과 하상 특성(식생 및 모래)에 대한 초분광 자료를 수집하여 고유 초분광 스펙트럼과 비교하였다. 그 결과, 부유사의 분광 특성은 유사의 종류 및 입도에 따라 농도 증가에 따른 초분광 스펙트럼의 반사율 변화가 상이하게 나타났다. 또한, 1 m 이하의 얕은 수심 조건에서는 바닥 반사의 영향으로 하상 종류에 따라 초분광 스펙트럼의 개형이 크게 변화하였으며, 고농도의 부유사가 분포할 때도 바닥 반사가 크게 영향을 미치는 것을 확인하였다. 이러한 분광다양성이 반영된 부유사농도와 초분광 자료의 관계를 구축하기 위하여 기계학습 기반 랜덤포레스트 회귀 모형과 가우시안 혼합 모형 기반 초분광 군집 기법을 결합한 CMR-OV를 적용한 결과, 기존 연구들에서 주로 활용된 밴드비 기반의 모형과 단일 기계학습모형에 비해 정확도가 크게 향상하였다. 특히, 기존 최적 밴드비 분석 (OBRA) 방법은 비선형성을 고려해도 좁은 영역의 파장대만을 고려하는 한계점으로 인해 분광다양성을 반영하지 못하는 것으로 밝혀졌다. 하지만, CMR-OV는 폭 넓은 파장대 영역을 고려함과 동시에 높은 정확도를 산출하였다. 최종적으로 CMR-OV를 황강의 직선구간 및 사행구간과 낙동강과 황강의 합류부에 적용하여 현장검증을 수행한 결과, 기존 모형 대비 정확도와 부유사 농도 맵핑의 정밀성에서 큰 개선이 있었으며, 비학습지역에서도 높은 정확도를 산출하였다. 특히, 하천 합류부에서는 초분광 군집을 통해 두 하천 흐름의 경계층을 명확히 구별하였으며, 이를 바탕으로 지류와 본류에 대해 각각 분리된 회귀모형을 구축하여 복잡한 합류부 근역 경계층에서의 부유사 분포를 보다 정확하게 재현하였다. 또한, 나아가서 재현된 고해상도의 부유사 공간분포를 바탕으로 혼합도를 산정한 결과, 기존 점계측 대비 상세하게 부유사 혼합에 대한 정량적 평가가 가능한 것으로 나타났다. 따라서, 본 연구에서 개발한 초분광영상 기반 부유사 계측 기술을 통해 추후 하천 조사 및 관리 실무의 정확성 및 효율성을 크게 증진할 수 있을 것으로 기대된다.The conventional measurement method of suspended sediment concentration (SSC) in the riverine system is labor-intensive and time-consuming since it has been conducted using the sampling-based direct measurement method. For this reason, it is challenging to collect high-resolution datasets of SSC in rivers. In order to overcome this limitation, remote sensing-based techniques using multi- or hyper-spectral images from satellites or UAVs have been recently carried out to obtain high-resolution SSC distributions in water environments. However, suspended sediment in rivers is more dynamic and spatially heterogeneous than those in other fields. Moreover, the sediment and streambed properties have strong regional characteristics depending on the river type; thus, only models suitable for a specific period and region have been developed owing to the increased spectral variability of the water arising from various types of suspended matter in the water and the heterogeneous streambed properties. Therefore, to overcome the limitations of the existing monitoring system, this study proposed a robust hyperspectral imagery-based SSC measurement method, termed cluster-based machine learning regression with optical variability (CMR-OV). This method dealt with the spectral variability problem by combining hyperspectral clustering and machine learning regression with the Gaussian mixture model (GMM) and Random forest (RF) regression. The hyperspectral clustering separated the complex dataset into several homogeneous datasets according to spectral characteristics. Then, the machine learning regressors corresponding to clustered datasets were built to construct the relationship between the hyperspectral spectrum and SSC. The development and validation of the proposed method were carried out through the following processes: 1) analysis of confounding factors in the spectral variability through experimental studies, 2) selection of an optimal regression model and validation of hyperspectral clustering, and 3) evaluation of field applicability. In the experimental studies, the intrinsic hyperspectral spectra of suspended sediment were collected in a completely mixed state after removing the bottom reflection using a horizontal rotating cylinder. Then, hyperspectral data on various sediment properties (particle size and mineral contents) and river bed properties (sand and vegetation) were collected from sediment tracer experiments in field-scale open channels under different hydraulic conditions and compared with intrinsic hyperspectral spectra. Consequently, the change of the hyperspectral spectrum was different according to the sediment type and particle size distribution. In addition, under the shallow water depth condition of 1 m or less, the shape of the hyperspectral spectrum changed significantly depending on the bed type due to the bottom reflectance. The bottom reflectance substantially affected the hyperspectral spectrum even when the high SSC was distributed. As a result of combining the GMM and RF regression with building a relationship between the SSC and hyperspectral data reflecting the spectral variability, the accuracy was substantially improved compared to the other methods. In particular, even when nonlinearity is considered based on the existing optimal band ratio analysis (OBRA) method, spectral variability could not be reflected due to the limitation of considering only a narrow wavelength range. On the other hand, CMR-OV showed high accuracy while considering a wide range of wavelengths with clusters having distinct spectral characteristics. Finally, the CMR-OV was applied to the straight and meandering reaches of the Hwang River and the confluence of the Nakdong and Hwang Rivers in South Korea to assess field applicability. There was a remarkable improvement in the accuracy and precision of SSC mapping under various river conditions compared to the existing models, and CMR-OV showed robust performance even with non-calibrated datasets. At the river confluence, the mixing pattern between the main river and tributary was apparently retrieved from CMR-OV under optically complex conditions. Compared to the non-clustered model, hyperspectral clustering played a primary role in improving the performance by separating the water bodies originating from both rivers. It was also possible to quantitatively evaluate the complicated mixing pattern in detail compared to the existing point measurement. Therefore, it is expected that the accuracy and efficiency of river investigation will be significantly improved through the SSC measurement method presented in this study.Abstract of dissertation i List of figures ix List of tables xvii List of abbreviations xix List of symbols xxii 1. Introduction 1 2. Theoretical research 13 2.1.1 Pre-processing of hyperspectral image (HSI) 19 2.1.2 Optical characteristics of suspended sediment in rivers 28 2.1.2.1 Theory of solar radiation transfer in rivers 28 2.1.2.2 Heterogeneity of sediment properties 33 2.1.2.3 Effects of bottom reflectance 38 2.1.2.4 Vertical distribution of suspended sediment 41 2.1.3 Retrieval of suspended sediment from remote sensing data 46 2.1.3.1 Remote sensing-based regression approach 46 2.1.3.2 Clustering of remote sensing data 52 2.2 Mapping of suspended sediment concentration in rivers 56 2.2.1 Traditional method for spatial measurement 56 2.2.2 Spatial measurement at river confluences 57 2.2.2.1 Dynamics of flow and mixing at river confluences 57 2.2.2.2 Field experiments in river confluences 64 3. Experimental studies 68 3.1 Experimental cases 68 3.2 Laboratory experiment 74 3.2.1 Experimental setup 74 3.2.2 Experimental method 78 3.3 Field-scale experiments in River Experiment Center 83 3.3.1 Experiments in the straight channel 83 3.3.2 Experiments in the meandering channel 96 3.4 Field survey 116 3.4.1 Study area and field measurement 116 3.4.2 Hydraulic and sediment data in rivers with simple geometry 122 3.4.3 Hydraulic and sediment data in river confluences 126 3.5 Analysis of hyperspectral data of suspended sediment 141 3.5.1 Hyperspectral data of laboratory experiment 142 3.5.2 Hyperspectral data of field-scale experiments 146 3.5.2.1 Effect of bottom reflectance 146 3.5.2.2 Principal component analysis of the effect of suspended sediment properties 154 4. Development of suspended sediment concentration estimator using UAV-based hyperspectral imagery 164 4.1 Outline of Cluster-based Machine learning Regression with Optical Variability (CMR-OV) 164 4.2 Pre-processing of hyperspectral images 168 4.3 Regression models and clustering technique 173 4.3.1 Index-based regression models 173 4.3.2 Machine learning regression models 175 4.3.3 Relevant band selection 183 4.3.4 Gaussian mixture model for clustering 185 4.3.5 Performance criteria 188 4.4 Model development and evaluation 189 4.4.1 Comparison of regression models 189 4.4.1.1 OBRA-based explicit models 189 4.4.1.2 Machine learning-based implicit models 194 4.4.2 Assessment of hyperspectral clustering 200 4.4.3 Spatio-temporal SSCV mapping using CMR-OV 215 5. Evaluation of field applicability of CMR-OV 225 5.1 Outline of field applicability test 225 5.2 Cross-applicability validation of CMR-OV 227 5.3 Assessment of field applicability in rivers with simple geometry 234 5.4 Assessment of field applicability in river confluences 241 5.4.1 Classification of river regions using hyperspectral clustering 241 5.4.2 Retrievals of SSCV map 258 5.4.3 Mixing pattern extraction from SSCv map 271 6. Conclusions and future study 274 6.1 Conclusions 274 6.2 Future directions 278 Reference 280 Appendix 308 Appendix A. Breakthrough curve (BTC) analysis 308 Appendix B. Experimental data 310 Appendix B. 1. BTCs of in-situ measured SSC from field-scale experiments 310 Appendix B. 2. Dataset of spectra from hyperspectral images and corresponding SSC in rivers 330 Appendix C. CMR-OV code 331 국문초록 337박

Measuring freshwater aquatic ecosystems: The need for a hyperspectral global mapping satellite mission

AbstractFreshwater ecosystems underpin global water and food security, yet are some of the most endangered ecosystems in the world because they are particularly vulnerable to land management change and climate variability. The US National Research Council's guidance to NASA regarding missions for the coming decade includes a polar orbiting, global mapping hyperspectral satellite remote sensing mission, the Hyperspectral Infrared Imager (HyspIRI), to make quantitative measurements of ecosystem change. Traditionally, freshwater ecosystems have been challenging to measure with satellite remote sensing because they are small and spatially complex, require high fidelity spectroradiometry, and are best described with biophysical variables derived from high spectral resolution data. In this study, we evaluate the contribution of a hyperspectral global mapping satellite mission to measuring freshwater ecosystems. We demonstrate the need for such a mission, and evaluate the suitability and gaps, through an examination of the measurement resolution issues impacting freshwater ecosystem measurements (spatial, temporal, spectral and radiometric). These are exemplified through three case studies that use remote sensing to characterize a component of freshwater ecosystems that drive primary productivity. The high radiometric quality proposed for the HyspIRI mission makes it uniquely well designed for measuring freshwater ecosystems accurately at moderate to high spatial resolutions. The spatial and spectral resolutions of the HyspIRI mission are well suited for the retrieval of multiple biophysical variables, such as phycocyanin and chlorophyll-a. The effective temporal resolution is suitable for characterizing growing season wetland phenology in temperate regions, but may not be appropriate for tracking algal bloom dynamics, or ecosystem responses to extreme events in monsoonal regions. Global mapping missions provide the systematic, repeated measurements necessary to measure the drivers of freshwater biodiversity change. Archival global mapping missions with open access and free data policies increase end user uptake globally. Overall, an archival, hyperspectral global mapping mission uniquely meets the measurement requirements of multiple end users for freshwater ecosystem science and management

A Comprehensive Review on Water Quality Parameters Estimation Using Remote Sensing Techniques

Remotely sensed data can reinforce the abilities of water resources researchers and decision makers to monitor waterbodies more effectively. Remote sensing techniques have been widely used to measure the qualitative parameters of waterbodies (i.e., suspended sediments, colored dissolved organic matter (CDOM), chlorophyll-a, and pollutants). A large number of different sensors on board various satellites and other platforms, such as airplanes, are currently used to measure the amount of radiation at different wavelengths reflected from the water’s surface. In this review paper, various properties (spectral, spatial and temporal, etc.) of the more commonly employed spaceborne and airborne sensors are tabulated to be used as a sensor selection guide. Furthermore, this paper investigates the commonly used approaches and sensors employed in evaluating and quantifying the eleven water quality parameters. The parameters include: chlorophyll-a (chl-a), colored dissolved organic matters (CDOM), Secchi disk depth (SDD), turbidity, total suspended sediments (TSS), water temperature (WT), total phosphorus (TP), sea surface salinity (SSS), dissolved oxygen (DO), biochemical oxygen demand (BOD) and chemical oxygen demand (COD)