Abstract
Water quality monitoring of inland waterbodies is a global challenge due to limited
monitoring infrastructure and availability of high-resolution hydrological data. Timely
assessment and mitigation of water quality threats is constrained by limited data availability.
To address this issue, remote sensing techniques have emerged as a robust tool for continuous
real-time monitoring of inland water quality. In tropical regions, there has been a greater
emphasis on remote sensing techniques for the continuous monitoring of water quality, mainly
in eutrophic or hypereutrophic inland water bodies such as estuaries, rivers, and lakes, while
reservoirs have received comparatively less attention. However, worldwide, tropical reservoirs
are vulnerable to contamination risks due to their multifunctional roles, i.e., drinking, irrigation,
and hydropower generation and long periods of storage times without adequate outflows which
are critical for maintaining downstream water quality. Furthermore, the surrounding catchment
influence contamination dynamics, as rapid changes in land use/land cover (LULC) can
introduce sediments, nutrients, and heavy metals, contributing to elevated levels of physical,
biological, and chemical characteristics of water quality parameters. Identifying the critical
importance of monitoring tropical reservoirs, the present study focuses on employing remote
sensing techniques to estimate water quality parameters, focusing on physio-biological
characteristics, mainly in oligotrophic and mesotrophic reservoirs, and underscores the
significance of catchment-related factors in influencing contamination levels. This approach is
essential for maintaining optimal water quality levels, benefiting both local communities and
the surrounding environment.
The study selected two tropical reservoirs, Bhadra and Tungabhadra, situated within the
same river system and experiencing similar climatic conditions but distinct landscape
characteristics. The primarily aim is to develop a modeling framework to map and quantify the
spatiotemporal variability of Chlorophyll-a (Chl-a), turbidity and surface water temperature
(SWT), along with associated water spread for 2016-2021 using Sentinel 2 and Landsat 8
satellite datasets. The second aim is to examine interconnections among selected water quality
parameters, to improve the accuracy of reservoir water quality assessments and identify
potential correlations and interdependencies. The third aim is to comprehend how the landscape
(land use/land cover (LULC)) and meteorological variables (rainfall, air temperature) of the
contributing catchment influence contamination dynamics. The remote sensing-based results,
validated with field-based observations measured from the Aquaread AP7000 instrument and secondary data include EOMAP (Earth Observation and Mapping) water quality derived
datasets were employed to enhance accuracy and reliability.
Chl-a, used as a proxy for nutrient contamination primarily from agricultural runoff,
estimated using the Maximum Chlorophyll Index (MCI) derived from Sentinel 2 satellite data
in the Google Earth Engine (GEE) platform. The results indicate a consistent and extensive
distribution of Chl-a across the entire water surface of the Tungabhadra reservoir, while the
Bhadra reservoir exhibited a more limited distribution. During the post-monsoon, increase in
Chl-a spread in the Tungabhadra reservoir, primarily attributed to nutrient-rich water inflows
from agricultural and urban areas. This notable rise linked to the harvesting of Kharif crops.
Additionally, the discharge of untreated sewage further contributes to the degradation of water
quality in the Tungabhadra reservoir. In contrast, the Bhadra reservoir, surrounded
predominantly by forested areas, maintained water cleanliness and served as a riparian
boundary. These findings demonstrate how LULC changes drive nutrient contamination in
tropical reservoirs.
Turbidity was considered as a proxy for sediments, detected and mapped using
Sentinel-2 data. The Normalised Difference Turbidity Index (NDTI) values strongly correlated
with EOMAP and field-based observations having values > 10 NTU (nephelometric turbidity
unit) with R
2 = 0.81 and standard error estimate (SEE) of 5.3, respectively. In addition, the
correlation between red band reflectance values with < 10 NTU, demonstrated a strong relation
with an R
2 = 0.74, SEE = 1.7. Combining NDTI and red band reflectance allowed classification
into low, moderate, and high turbidity zones. Further analyses indicated that diverse land use
patterns, particularly high proportions of urban and agriculture area along with rainfall,
significantly influenced the annual and seasonal turbidity variations.
Surface water temperature (SWT) is a significant physical parameter affecting aquatic
metabolism, nutrient cycling, and contaminant interaction was estimated using Landsat 8
Thermal Infrared (TIR) d