India, the seventh-largest country in the world, spans approximately 3.287 million square kilometers and is characterized by a diverse range of geographical features. In the north, the towering snow-covered Himalayas dominate the landscape, while the expansive Indo-Gangetic plains stretch across the heart of the country. To the west, arid regions shape the terrain, whereas the peninsular plateau in the south showcases a distinct topography. India is also home to many significant and life-sustaining rivers like the Ganga, Brahmaputra, Godavari, Narmada, etc. These rivers can further be categorized as perennial and non-perennial rivers. Rivers originating from the snow-clad Himalayan ranges like the Ganga, Indus, and Brahmaputra, are perennial because their flow is sustained throughout the year by glacial melt. In contrast, peninsular rivers like the Godavari, Cauvery, Krishna, etc., are primarily rain-fed and experiences enhanced seasonal fluctuations and reduced flow during dry periods. However, among these rain-fed peninsular rivers, the Narmada River, the longest west-flowing river, stands out as an exception (Narmada Basin Report, 2014). Despite being rain fed, it remains perennial and maintains its flow throughout the year (NIH, 1997). This unique characteristic, along with its distinct geography, hydrology, and cultural significance, makes the Narmada River an ideal subject for the comprehensive monitoring of its environmental aspects.