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Keywords = Sentinel 3A/OLCI

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21 pages, 4830 KiB  
Article
Optical Classification of the Remote Sensing Reflectance and Its Application in Deriving the Specific Phytoplankton Absorption in Optically Complex Lakes
by Kun Xue, Ronghua Ma, Dian Wang and Ming Shen
Remote Sens. 2019, 11(2), 184; https://doi.org/10.3390/rs11020184 - 18 Jan 2019
Cited by 37 | Viewed by 5674
Abstract
Optical water types (OWTs) were identified from remote sensing reflectance (Rrs(λ)) values in a field-measured dataset of several large lakes in the lower reaches of the Yangtze and Huai River (LYHR) Basin. Four OWTs were determined from normalized remote sensing [...] Read more.
Optical water types (OWTs) were identified from remote sensing reflectance (Rrs(λ)) values in a field-measured dataset of several large lakes in the lower reaches of the Yangtze and Huai River (LYHR) Basin. Four OWTs were determined from normalized remote sensing reflectance spectra (NRrs(λ)) using the k-means clustering approach, and were identified in the Sentinel 3A OLCI (Ocean Land Color Instrument) image data over lakes in the LYHR Basin. The results showed that 1) Each OWT is associated with different bio-optical properties, such as the concentration of chlorophyll-a (Chla), suspended particulate matter (SPM), proportion of suspended particulate inorganic matter (SPIM), and absorption coefficient of each component. One optical water type showed an obvious characteristic with a high contribution of mineral particles, while one type was mostly determined by a high content of phytoplankton. The other types belonged to the optically mixed water types. 2) Class-specific Chla inversion algorithms performed better for all water types, except type 4, compared to the overall dataset. In addition, class-specific inversion algorithms for estimating the Chla-specific absorption coefficient of phytoplankton at 443 nm (a*ph(443)) were developed based on the relationship between a*ph(443) and Chla of each OWT. The spatial variations in the class-specific model-derived a*ph(443) values were illustrated for 2 March 2017, and 24 October 2017. 3) The dominant water type and the Shannon index (H) were used to characterize the optical variability or similarity of the lakes in the LYHR Basin using cloud-free OLCI images in 2017. A high optical variation was located in the western and southern parts of Lake Taihu, the southern part of Lake Hongze, Lake Chaohu, and several small lakes near the Yangtze River, while the northern part of Lake Hongze had a low optical diversity. This work demonstrates the potential and necessity of optical classification in estimating bio-optical parameters using class-specific inversion algorithms and monitoring of the optical variations in optically complex and dynamic lake waters. Full article
(This article belongs to the Special Issue Satellite Monitoring of Water Quality and Water Environment)
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Graphical abstract

Graphical abstract
Full article ">Figure 1
<p>Location of the lakes in the lower reaches of the Yangtze and Huai River (LYHR) Basin. The field samples of Lake Chaohu, Lake Taihu, and Lake Hongze were collected from 2011 to 2017. The validation data were match-up pairs of field data and Ocean Land Color Instrument (OLCI)-derived data.</p>
Full article ">Figure 2
<p>Comparison of the field-measured <span class="html-italic">R<sub>rs</sub></span> and OLCI-derived <span class="html-italic">R<sub>rs</sub></span> using the (<b>a</b>) C2RCC, (<b>b</b>) POLYMER, and (<b>c</b>) 6SV atmospheric correction models for match-up pairs at different OLCI bands (<span class="html-italic">N</span> = 63). (<b>d</b>) MAPE of C2RCC, POLYMER, and 6SV at different OLCI bands, error bars represent one standard deviation of the absolute percentage error in the validation data.</p>
Full article ">Figure 3
<p>Performance of the three unsupervised clustering methods: heritage clustering, fuzzy <span class="html-italic">c</span>-means (FCM), and <span class="html-italic">k</span>-means in clustering waters with different number of types: (<b>a</b>) silhouette coefficient, (<b>b</b>) SSE (sum of the squared errors), and (<b>c</b>) STD (standard deviation).</p>
Full article ">Figure 4
<p>(<b>a</b>–<b>d</b>) <span class="html-italic">NR<sub>rs</sub></span>(λ) sorted into the four optical water types (OWTs) from the <span class="html-italic">k</span>-means cluster analysis (<span class="html-italic">N</span> = 535); blue lines: individual <span class="html-italic">NR<sub>rs</sub></span>(λ) values; red lines: mean <span class="html-italic">NR<sub>rs</sub></span>(λ) of each OWT. (<b>e</b>) The mean spectra of <span class="html-italic">NR<sub>rs</sub></span>(λ) of the four OWTs. The OWT means and covariance matrices are the basis for the membership function. Note that the optical classification was conducted using the <span class="html-italic">NR<sub>rs</sub></span>(λ) of the field data. (<b>f</b>) The mean spectra of <span class="html-italic">R<sub>rs</sub></span>(λ) of the four OWTs.</p>
Full article ">Figure 5
<p>Mean spectrum of the absorption coefficients of phytoplankton (<span class="html-italic">a<sub>ph</sub></span>), NAP (<span class="html-italic">a<sub>d</sub></span>), and CDOM (<span class="html-italic">a<sub>g</sub></span>) in each OWT: (<b>a</b>) type 1, (<b>b</b>) type 2, (<b>c</b>) type 3, and (<b>d</b>) type 4.</p>
Full article ">Figure 6
<p>(<b>a</b>) Mean spectra of the absorption coefficient of phytoplankton normalized to the Chl<span class="html-italic">a</span> concentration (<span class="html-italic">a<sup>*</sup><sub>ph</sub></span>(λ)) of types 1–4. (<b>b</b>) Boxplots of <span class="html-italic">a<sup>*</sup><sub>ph</sub></span>(443)/<span class="html-italic">a<sup>*</sup><sub>ph</sub></span>(675) for each OWT in the field-measured data. (<b>c</b>) Mean spectra of the absorption coefficient of NAP normalized to the SPM concentration (<span class="html-italic">a<sup>*</sup><sub>d</sub></span>(λ)) of types 1–4. (<b>d</b>) Boxplots of <span class="html-italic">a<sup>*</sup><sub>d</sub></span>(443) for each OWT in the field-measured data. The sample median is indicated by a line within the box, the dots represent the mean value, and “x” represents data beyond the bounds of the error bars.</p>
Full article ">Figure 7
<p>(<b>a</b>) Mer-3B versus field-measured Chl<span class="html-italic">a</span> content data for OLCI validation of each OWT and all data. (<b>b</b>) Chl<span class="html-italic">a</span> versus <span class="html-italic">a<sup>*</sup><sub>ph</sub></span>(443) for OLCI validation of each OWT and all data. (<b>c</b>) Comparison of the field-measured Chl<span class="html-italic">a</span> and model-derived Chl<span class="html-italic">a</span> using unclassified models and classified models for each OWT and all data. (<b>d</b>) Comparison of the field-measured <span class="html-italic">a<sup>*</sup><sub>ph</sub></span>(443) and model-derived <span class="html-italic">a<sup>*</sup><sub>ph</sub></span>(443) using unclassified models and classified models for each OWT and all data. Note that the input Chl<span class="html-italic">a</span> data in calculating <span class="html-italic">a<sup>*</sup><sub>ph</sub></span>(443) were the derived Chl<span class="html-italic">a</span> values using the class-specific model of each OWT. The number of samples (<span class="html-italic">N</span>) is 15, 15, 27, and 6, for type 1 to type 4, respectively.</p>
Full article ">Figure 8
<p>(<b>a</b>) Optical water types, (<b>b</b>) Chl<span class="html-italic">a</span> derived using the unclassified Mer-3B Chl<span class="html-italic">a</span> model, (<b>c</b>) Chl<span class="html-italic">a</span> derived using the class-specific Mer-3B Chl<span class="html-italic">a</span> model, and (<b>d</b>) <span class="html-italic">a<sup>*</sup><sub>ph</sub></span>(443) derived using the class-specific model on the 2 March 2017, OLCI image over the lakes in the LYHR Basin. (<b>e</b>) Optical water types, (<b>f</b>) Chl<span class="html-italic">a</span> derived using the unclassified Mer-3B Chl<span class="html-italic">a</span> model, (<b>g</b>) Chl<span class="html-italic">a</span> derived using the class-specific Mer-3B Chl<span class="html-italic">a</span> model, and (<b>h</b>) <span class="html-italic">a<sup>*</sup><sub>ph</sub></span>(443) derived using the class-specific model on the 24 October 2017, OLCI image over the lakes in the LYHR Basin.</p>
Full article ">Figure 9
<p>The comparison of mean <span class="html-italic">R<sub>rs</sub></span>(λ) of the four optical water types with the optical water types in the previous studies [<a href="#B21-remotesensing-11-00184" class="html-bibr">21</a>,<a href="#B23-remotesensing-11-00184" class="html-bibr">23</a>]. The dashed lines represent mean <span class="html-italic">R<sub>rs</sub></span>(λ) of OWTs acquired from Table A1 in Moore et al. (2009) [<a href="#B21-remotesensing-11-00184" class="html-bibr">21</a>] and <a href="#remotesensing-11-00184-t002" class="html-table">Table 2</a> in Moore et al. (2014) [<a href="#B23-remotesensing-11-00184" class="html-bibr">23</a>].</p>
Full article ">Figure 10
<p>(<b>a</b>) Dominant OWTs of the lakes in the LYHR Basin in 2017 (the class most frequently selected as the dominant class over the period); (<b>b</b>) Shannon index (<span class="html-italic">H</span>) computed from the frequency of the different OWTs of the lakes in the LYHR Basin in 2017. (<b>c</b>–<b>f</b>) The annual frequency of the different OWTs: (<b>c</b>) type 1, (<b>d</b>) type 2, (<b>e</b>) type 3, (<b>f</b>) type 4, associated with lakes in the LYHR basin in 2017.</p>
Full article ">Figure 11
<p>Comparison of <span class="html-italic">R<sub>rs</sub></span>(λ) derived using ρ in Mobley (2015) [<a href="#B35-remotesensing-11-00184" class="html-bibr">35</a>] (<span class="html-italic">R<sub>rs</sub></span><sub>-M2015</sub>(λ)) and (<b>a</b>) <span class="html-italic">R<sub>rs</sub></span>(λ) derived using ρ in Mobley (1999) [<a href="#B34-remotesensing-11-00184" class="html-bibr">34</a>] (<span class="html-italic">R<sub>rs</sub></span><sub>-M1999</sub>(λ)), and (<b>b</b>) using ρ = 0.028 for match-up pairs (<span class="html-italic">N</span> = 63). (<b>c</b>) Comparisons between indexes (NR-2B, Mer-3B) derived using M2015 and M1999, 0.028, respectively. (<b>d</b>) Spectral RMSD of <span class="html-italic">R<sub>rs</sub></span>(λ) between ρ of M2015 and M1999 (blue line), 0.028 (red line), respectively.</p>
Full article ">
6882 KiB  
Article
Determination of the Downwelling Diffuse Attenuation Coefficient of Lake Water with the Sentinel-3A OLCI
by Ming Shen, Hongtao Duan, Zhigang Cao, Kun Xue, Steven Loiselle and Herve Yesou
Remote Sens. 2017, 9(12), 1246; https://doi.org/10.3390/rs9121246 - 1 Dec 2017
Cited by 46 | Viewed by 6536
Abstract
The Ocean and Land Color Imager (OLCI) on the Sentinel-3A satellite, which was launched by the European Space Agency in 2016, is a new-generation water color sensor with a spatial resolution of 300 m and 21 bands in the range of 400–1020 nm. [...] Read more.
The Ocean and Land Color Imager (OLCI) on the Sentinel-3A satellite, which was launched by the European Space Agency in 2016, is a new-generation water color sensor with a spatial resolution of 300 m and 21 bands in the range of 400–1020 nm. The OLCI is important to the expansion of remote sensing monitoring of inland waters using water color satellite data. In this study, we developed a dual band ratio algorithm for the downwelling diffuse attenuation coefficient at 490 nm (Kd(490)) for the waters of Lake Taihu, a large shallow lake in China, based on data measured during seven surveys conducted between 2008 and 2017 in combination with Sentinel-3A-OLCI data. The results show that: (1) Compared to the available Kd(490) estimation algorithms, the dual band ratio (681 nm/560 nm and 754 nm/560 nm) algorithm developed in this study had a higher estimation accuracy (N = 26, coefficient of determination (R2) = 0.81, root-mean-square error (RMSE) = 0.99 m−1 and mean absolute percentage error (MAPE) = 19.55%) and validation accuracy (N = 14, R2 = 0.83, RMSE = 1.06 m−1 and MAPE = 27.30%), making it more suitable for turbid inland waters; (2) A comparison of the OLCI Kd(490) product and a similar Moderate Resolution Imaging Spectroradiometer (MODIS) product reveals a high consistency between the OLCI and MODIS products in terms of the spatial distribution of Kd(490). However, the OLCI product has a smoother spatial distribution and finer textural characteristics than the MODIS product and contains notably higher-quality data; (3) The Kd(490) values for Lake Taihu exhibit notable spatial and temporal variations. Kd(490) is higher in seasons with relatively high wind speeds and in open waters that are prone to wind- and wave-induced sediment resuspension. Finally, the Sentinel-3A-OLCI has a higher spatial resolution and is equipped with a relatively wide dynamic range of spectral bands suitable for inland waters. The Sentinel-3B satellite will be launched soon and, together with the Sentinel-3A satellite, will form a two-satellite network with the ability to make observations twice every three days. This satellite network will have a wider range of application and play an important role in the monitoring of inland waters with complex optical properties. Full article
(This article belongs to the Special Issue Remote Sensing of Floodpath Lakes and Wetlands)
Show Figures

Graphical abstract

Graphical abstract
Full article ">Figure 1
<p>Location of Lake Taihu, China. (<b>a</b>) The Lake Taihu Basin is a flat region, and the Tiaoxi River (denoted by the black arrow) exhibits the maximum inflow; (<b>b</b>) following convention, the lake is divided into several segments. The black symbols with different shapes indicate sampling stations during seven cruise surveys in October 2008, January 2011, May 2011, March 2013, November 2016, March 2017, and April 2017. The red flag is the AERONET station, and the red stars are meteorological stations. The blue squares indicate four virtual stations located in different lake segments.</p>
Full article ">Figure 2
<p>Processing procedure of the satellite-derived <span class="html-italic">K</span><sub>d</sub>(490) product.</p>
Full article ">Figure 3
<p>Relationships between <span class="html-italic">K</span><sub>d</sub>(490) and the bio-optical parameters of the water: (<b>a</b>) SPIM; (<b>b</b>) SPOM; (<b>c</b>) Chla; (<b>d</b>) <span class="html-italic">a</span><sub>g</sub>(440).</p>
Full article ">Figure 4
<p>(<b>a</b>) Comparison of the <span class="html-italic">R</span><sub>rs</sub> measured in situ and the OLCI-derived <span class="html-italic">R</span><sub>rs</sub> after the 6S atmospheric correction for 40 matchups obtained in November 2016, March 2017, and April 2017; (<b>b</b>) comparison of the <span class="html-italic">R</span><sub>rs</sub> spectrum measured in situ and the OLCI-derived <span class="html-italic">R</span><sub>rs</sub> spectrum after the 6S atmospheric correction for different <span class="html-italic">K</span><sub>d</sub>(490) values. The lines represent the <span class="html-italic">R</span><sub>rs</sub> spectra from the in situ measurements, and the marks represent the OLCI-derived <span class="html-italic">R</span><sub>rs</sub> spectra after the 6S atmospheric corrections.</p>
Full article ">Figure 5
<p>Development and validation of the algorithm for estimating <span class="html-italic">K</span><sub>d</sub>(490) in Lake Taihu from the OLCI-derived <span class="html-italic">R</span><sub>rs</sub>.</p>
Full article ">Figure 6
<p>Daily OLCI RGB and <span class="html-italic">K</span><sub>d</sub>(490) distributions in Lake Taihu, China, derived from Sentinel OLCI data (November 2016–April 2017). Note that the data influenced by algal blooms and clouds are excluded.</p>
Full article ">Figure 7
<p>Distributions of (<b>a</b>) the mean and (<b>b</b>) the coefficient of variation (CV) of the OLCI-derived <span class="html-italic">K</span><sub>d</sub>(490) in Lake Taihu from November 2016 to April 2017.</p>
Full article ">Figure 8
<p>Temporal variations of the OLCI-derived <span class="html-italic">K</span><sub>d</sub>(490) at four virtual stations in different lake segments from November 2016 to April 2017. Note that the data influenced by algal blooms and cloud are excluded.</p>
Full article ">Figure 9
<p>(<b>a</b>) Variation of RMSE<sub>rel</sub> for <span class="html-italic">K</span><sub>d</sub>(490) derived from the errors introduced by <span class="html-italic">R</span><sub>rs</sub>(681)/<span class="html-italic">R</span><sub>rs</sub>(560) and <span class="html-italic">R</span><sub>rs</sub>(754)/<span class="html-italic">R</span><sub>rs</sub>(560) from the atmospheric correction; (<b>b</b>) comparison of the in situ measured <span class="html-italic">R</span><sub>rs</sub> band ratios and the OLCI-derived <span class="html-italic">R</span><sub>rs</sub> band ratios after the 6S atmospheric correction for <span class="html-italic">R</span><sub>rs</sub>(681)/<span class="html-italic">R</span><sub>rs</sub>(560) and <span class="html-italic">R</span><sub>rs</sub>(754)/<span class="html-italic">R</span><sub>rs</sub>(560); (<b>c</b>,<b>d</b>) examples showing the influence of the aerosol optical depth on the OLCI-derived <span class="html-italic">R</span><sub>rs</sub> band ratios/<span class="html-italic">K</span><sub>d</sub>(490) at virtual station S1 on 14 March 2017.</p>
Full article ">Figure 10
<p>(<b>a</b>) The OLCI RGB image, (<b>b</b>) the single band ratio algorithm-derived <span class="html-italic">K</span><sub>d</sub>(490), and (<b>c</b>) the dual band ratio algorithm-derived <span class="html-italic">K</span><sub>d</sub>(490) from the OLCI for 29 April 2017.</p>
Full article ">Figure 11
<p>(<b>a</b>,<b>b</b>) Validation of the algorithm for estimating <span class="html-italic">K</span><sub>d</sub>(490) in Lake Chaohu using the OLCI-derived <span class="html-italic">R</span><sub>rs</sub> with the default parameterization and local parameterization; (<b>c</b>,<b>d</b>) OLCI RGB and OLCI-derived <span class="html-italic">K</span><sub>d</sub>(490) distributions in Lake Chaohu on 26 February 2017.</p>
Full article ">Figure 12
<p>Distribution of the RMSE (<b>a</b>) and pixel-by-pixel scatter plot (<b>b</b>) between all of the <span class="html-italic">K</span><sub>d</sub>(490) products from the OLCI and MODIS. A total of 18 OLCI-MODIS image matchups were used, and six matchups with large uncertainties in the MODIS atmospheric correction were excluded. Note that bad pixels were removed.</p>
Full article ">Figure 13
<p>(<b>a</b>,<b>b</b>) OLCI and MODIS RGB images, (<b>c</b>,<b>d</b>) OLCI- and MODIS-derived <span class="html-italic">K</span><sub>d</sub>(490) values, (<b>e</b>,<b>f</b>) absolute relative differences (ARE) and pixel-by-pixel scatter plots between the <span class="html-italic">K</span><sub>d</sub>(490) products from the OLCI and MODIS on 14 March 2017, and 29 April 2017. Note that bad pixels were removed.</p>
Full article ">Figure 14
<p>(<b>a</b>) Pearson correlation coefficients (<span class="html-italic">r</span>) between the OLCI-derived <span class="html-italic">K</span><sub>d</sub>(490) and the mean wind speed for different hours (h = 1, 2, 3, …, 96 h) before the satellite image acquisition time at 4 virtual stations; (<b>b</b>) distribution of the maximum Pearson correlation coefficients (<span class="html-italic">r</span>); (<b>c</b>) distribution of hours corresponding to the maximum Pearson correlation coefficients.</p>
Full article ">
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