Indian cities experience prolonged waterlogging due to the landscape's memory of past rainfall, a phenomenon called hydrological hysteresis.
Hydrological hysteresis means a landscape's response to rainfall depends on current rainfall and past events, affecting water movement through soils, wetlands, rivers, and cities.
Rivers behave differently during rising and receding floods due to the evolving interaction between water flow and land, impacting water storage and resistance.
In October 2024, Bengaluru's Kogilu and Doddabommasandra lakes overflowed, demonstrating how saturated soils and submerged drains can prolong urban flooding even after rainfall decreases.
Detailed Insights:
Landscapes retain a memory of past rainfall, influencing how water moves; a catchment saturated from weeks of monsoon rain responds differently than a dry one to the same rainfall amount.
Water is stored in soils, aquifers, wetlands, and floodplains, releasing it at varying rates, causing a non-linear relationship between rainfall and river flow that shifts as the land moistens and dries.
During monsoons, dry soils and wetlands initially absorb water, but as they near saturation, infiltration decreases, leading to increased runoff and flooding even without intensified rainfall.
As monsoon rain intensifies, river channels fill rapidly, but once water exceeds the banks, it spreads laterally into floodplains and wetlands, slowing flow and causing sediment to settle.
Floodplains don't drain instantly; stored water seeps slowly through soils, re-entering channels or remaining ponded, delaying drainage as groundwater levels rise, altering the river's physical state.
Bengaluru's interconnected lakes, established in the 16th century, were linked by natural streams and wetlands, but these connections were straightened into concrete channels, causing quick filling, abrupt spilling, and slow emptying.
Recognizing the land’s hydrological memory is crucial for policymakers, emphasizing basin-scale planning and the importance of urban lakes, wetlands, and floodplains as critical infrastructure for water storage and release.
Key Concepts Involved:
Hydrological Hysteresis: The phenomenon where a landscape's response to rainfall depends on both current rainfall and past events.
Floodplain: A flat area of land near a river or stream that is subject to flooding.
Catchment: The area from which rainfall flows into a river or reservoir.