Dynamics of the Estuarine Turbidity Maximum Zone from Landsat-8 Data: The Case of the Maroni River Estuary, French Guiana
Abstract
:1. Introduction
2. Study Area and Methodology
2.1. Maroni River and Estuary
2.2. Satellite Data
2.2.1. Landsat 8 OLI Data Set
2.2.2. OLI Remote Sensing Reflectance (Rrs) Processing
2.2.3. Post-Treatment of Rrs Data
Clouds and Cloud-Shadow Detection
Estimation of SPM
2.2.4. ETM Detection
- 1-
- SPM normalization: The SPM values of each of the scenes in this study were normalized using the values corresponding to the 95th percentile estimated for each of the scenes. This normalization was performed to compare the different maps and to estimate the position of the ETM. The 95th percentile was selected to avoid outliers in the coastal areas, as in French Guiana SPM concentrations in the nearshore area (intertidal part of the mud banks) are characterized by high values [37].
- 2-
- SPM-normalized average: SPM-normalized values were averaged over time to estimate the different seasonal and inter-annual conditions. SPM-normalized values were also averaged for different tidal and flow-rate conditions (see figure captions in Section 3 for the number of maps used for the different conditions).
- 3-
- Definition of the ETM zone: The limits of the ETM were defined from an envelope of SPM-normalized values higher than 0.6. This > 0.6 threshold value was empirically defined following extensive work using remote sensing data on the muddy coast of the Guianas [29], and it was averaged for the different years and seasonal conditions.
- 4-
- Length and core of the ETM zone: The length was estimated to gain insight on ETM spatio-temporal variations. We use the terminology of Uncles et al. [48] to identify a “tail” and a “nose” (which represent, respectively, the downstream and upstream separation of the ETM from areas of lower turbidity). The core of the ETM was estimated from the barycenter using the geometric properties tool in QGIS software.
2.2.5. Data Processing
- 1-
- Estimate the peak values of the tide series.
- 2-
- Estimate the mean and standard deviation values (peak std) of the identified peaks.
- 3-
- Tides are defined as follows:Neap tides: tidalSpring tides: tidal values>mean peak mean value+((1/3) * peak std).Mean tides: tidal values between those of neap and spring tides.
2.3. Water Levels, River Discharge, Wind and Wave Data
3. Results and Discussion
3.1. Seasonal and Interannual Spatial Patterns
3.2. Tidal Influence
3.3. River Discharge
3.4. SPM and Variability of ETM Extension Due to External Conditions
3.5. Medium-Term (2013–2019) Variation: The Influence of Periodic Amazon-Derived Mud Banks
3.6. Capacity of Satellite Images in Contributing to Analysis of Estuarine Dynamics
4. Conclusions
Author Contributions
Funding
Conflicts of Interest
References
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2013 | 2014 | 2015 | 2016 | 2017 | 2018 | 2019 | |
---|---|---|---|---|---|---|---|
Rainy season | -14 July -30 July | -14 May -17 July | -09 January -25 January -10 February -17 May -02 June -18 June -04 July | -12 January -16 March -01 April -06 July -22 July | -04 April -20 April -25 July | -01 January -22 March -23 April -12 July -28 July | -20 January -21 February -25 March -26 April -28 May |
Dry season | -15 August -31 August -02 October -03 November -19 November -05 December | -18 August -03 September -19 September -05 October -06 November -24 December | -05 August -06 September -22 September -24 October -09 November -11 December | -24 September -10 October -26 October -11 November -27 November -13 December -29 December | -10 August -26 August -27 September -13 October -16 December | -13 August -29 August -14 September -30 September -16 October -01 November -19 December | - |
Extension | 2013 | 2014 | 2015 | 2016 | 2017 | 2018 | 2019 |
---|---|---|---|---|---|---|---|
Extension total (km2) | 55.2 ± 36.9 | 57.9 ± 23.7 | 57.8 ± 13.3 | 61.9 ± 23.1 | 52.6 ± 13.0 | 69.4 ± 19.9 | 76.6 ± 28.7 |
Rainy season (km2) | 40.3 ± 13.6 | 41.8 ± 9.3 | 54.7 ± 9.5 | 74.9 ± 21.4 | 52.1 ± 12.8 | 68.3 ± 27.1 | 76.6 ± 28.7 |
Dry season (km2) | 60.2 ± 27.9 | 61.9 ± 27.4 | 49.7 ± 17.5 | 59.7 ± 22.1 | 53.1 ± 16.5 | 69.9 ± 15.5 | - |
From KP 0 | 2013 | 2014 | 2015 | 2016 | 2017 | 2018 | 2019 |
---|---|---|---|---|---|---|---|
Tail (km) | 4.8 ± 5.5 | 7.4 ± 6.1 | 2.4 ± 5.5 | 2.0 ± 4.1 | −0.2 ± 3.9 | −2.2 ± 5.7 | −1.5 ± 3.4 |
Tail Rainy | 6.1 ± 4.9 | 2.4 ± 11.6 | −0.2 ± 4.1 | −1.1 ± 2.5 | −3.4 ± 2.9 | −3.6 ± 7.7 | −1.5 ± 3.4 |
Tail Dry | 4.5 ± 6.0 | 9.0 ± 3.5 | 5.5 ± 4.5 | 4.2 ± 3.4 | 1.7 ± 6.7 | −1.5 ± 4.8 | - |
Nose (km) | 30.4 ± 15.3 | 31.5 ± 14.9 | 20.6 ± 6.7 | 27.0 ± 7.7 | 19.3 ± 3.7 | 18.7 ± 6.2 | 19.3 ± 3.5 |
Nose Rainy | 33.4 ± 29.7 | 30.1 ± 29.5 | 17.2 ± 4.5 | 29.2 ± 12.0 | 17.2 ± 1.2 | 18.4 ± 9.0 | 19.3 ± 3.5 |
Nose Dry | 29.4 ± 12.0 | 31.9 ± 11.1 | 24.6 ± 6.9 | 25.5 ± 2.9 | 20.5 ± 4.3 | 18.9 ± 5.0 | - |
Core (km) | 15.5 ± 5.3 | 16.3 ± 6.4 | 11.7 ± 5.1 | 13.8 ± 2.2 | 9.4 ± 4.0 | 7.9 ± 5.6 | 9.4 ± 1.6 |
Core Rainy | 16.2 ± 13.3 | 12.7 ± 14.9 | 8.9 ± 3.5 | 11.8 ± 1.5 | 6.9 ± 0.9 | 6.9 ± 8.2 | 9.4 ± 1.6 |
Core Dry | 15.3 ± 2.2 | 17.5 ± 2.6 | 15.1 ± 4.8 | 15.3 ± 1.2 | 10.9 ± 4.5 | 8.5 ± 4.2 | - |
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Abascal-Zorrilla, N.; Vantrepotte, V.; Huybrechts, N.; Ngoc, D.D.; Anthony, E.J.; Gardel, A. Dynamics of the Estuarine Turbidity Maximum Zone from Landsat-8 Data: The Case of the Maroni River Estuary, French Guiana. Remote Sens. 2020, 12, 2173. https://doi.org/10.3390/rs12132173
Abascal-Zorrilla N, Vantrepotte V, Huybrechts N, Ngoc DD, Anthony EJ, Gardel A. Dynamics of the Estuarine Turbidity Maximum Zone from Landsat-8 Data: The Case of the Maroni River Estuary, French Guiana. Remote Sensing. 2020; 12(13):2173. https://doi.org/10.3390/rs12132173
Chicago/Turabian StyleAbascal-Zorrilla, Noelia, Vincent Vantrepotte, Nicolas Huybrechts, Dat Dinh Ngoc, Edward J. Anthony, and Antoine Gardel. 2020. "Dynamics of the Estuarine Turbidity Maximum Zone from Landsat-8 Data: The Case of the Maroni River Estuary, French Guiana" Remote Sensing 12, no. 13: 2173. https://doi.org/10.3390/rs12132173
APA StyleAbascal-Zorrilla, N., Vantrepotte, V., Huybrechts, N., Ngoc, D. D., Anthony, E. J., & Gardel, A. (2020). Dynamics of the Estuarine Turbidity Maximum Zone from Landsat-8 Data: The Case of the Maroni River Estuary, French Guiana. Remote Sensing, 12(13), 2173. https://doi.org/10.3390/rs12132173