Introduction
There is a certain assurance in repetition. The otherwise macabre seems to dwindle beneath successive layers of (un)remembering. The eyes learn to adjust, to look away from the portrait of human misery. To live within this recurring reign of terror, to experience it not as an interruption of ordinary life but as one of its conditions, is perhaps the defining character of the flood-prone communities of Assam in general, and of the Brahmaputra Valley in particular. For the people living in this part of the world, witnessing a flood is, in turn, to be flooded. Yet, ever so often, this restless rhythm is interrupted by a rupture; loud and agonising, a rupture which showcases a certain resistance to be absorbed into memory.
I grew up in a village around seven kilometres from Sibsagar town. The river Dikhow flows past our village and, for the twenty-odd years I spent there before moving to Delhi, the sight of the river swell with the onset of the monsoon was neither unfamiliar nor unanticipated. Floods were expected; although fearsome, they also came to be integrated into the seasonal rhythm of life. However, this time around, something seemed to be different.
It is not that this was the first time that Assam witnessed floods, or that the state never has come to experience the destructive power of the Brahmanputra and its tributaries. Even prior to the floods of July 2026, government agencies had already been mapping areas prone to flooding. They had drawn up district disaster management plans, set up a flood forecasting network and been issuing ever more sophisticated weather warnings. Hazard atlases had indicated vulnerable landscapes, the Master Plans had likewise recognised flood-sensitive areas. Also, in the days before the flood, the India Meteorological Department (IMD) had warned of heavy to very heavy rainfall in the Sivasagar and Charaideo districts and in the adjacent areas of Nagaland. Therefore, the hazard nor the possibility of flooding should have come as a surprise.
The question, therefore, should not simply be where and how much it rained.
What warrants our attention is the question of why a hazard that had already been forecasted, mapped and institutionally recognised, still ends up translating into widespread disruption. If one can find an explanation in the physical geography of Assam regarding why floods occur in the first place, it cannot by itself explain how they end up becoming disasters of such magnitude. This distinction, somewhere, requires us to gaze beyond meteorology and towards the institutions, planning practices, and systems of water governance, notably in urban areas, that mediate the relationship between water and the city.
This article focuses on the July 2026 floods in Sivasagar district, particularly in the towns of Sibsagar and Nazira and then uses them as an analytical viewpoint to address and examine a much wider national question.
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