
Nature-Based Solutions
For a Flood-Resilient Kathmandu
Building Urban Flood Resilience Through Rivers, Streets, Public Spaces and Blue-Green Infrastructure
Valley Constraints and Flood Risk Context
Flood risk in Kathmandu Valley is shaped not only by urban development, but also by changes occurring across the wider watershed. The map highlights areas where upstream landscape conditions, settlement growth and downstream river dynamics interact to influence flood behaviour.

Upstream landscape pressures
Changes in vegetation, slopes and land cover can increase surface runoff, reduce infiltration and accelerate the movement of water towards downstream river systems.
Loss of natural retention
Dams, settlements, land transformation and the decline of natural retention areas alter how rainfall is stored, released and conveyed through the watershed.
Rapid urban exposure
As settlements expand into drainage corridors and low-lying areas, more people, infrastructure and assets are exposed to flood impacts.
River corridors under pressure
Encroachment, constrained channels and infrastructure crossings reduce the capacity of river systems to safely convey high flows during intense rainfall.




Flood risk in Kathmandu Valley is shaped not only by urban development, but also by changes occurring across the wider watershed. The map highlights areas where upstream landscape conditions, settlement growth and downstream river dynamics interact to influence flood behaviour.
Upstream landscape pressures
Changes in vegetation, slopes and land cover can increase surface runoff, reduce infiltration and accelerate the movement of water towards downstream river systems.
Loss of natural retention
Dams, settlements, land transformation and the decline of natural retention areas alter how rainfall is stored, released and conveyed through the watershed.
Rapid urban exposure
As settlements expand into drainage corridors and low-lying areas, more people, infrastructure and assets are exposed to flood impacts.
River corridors under pressure
Encroachment, constrained channels and infrastructure crossings reduce the capacity of river systems to safely convey high flows during intense rainfall.



Kathmandu Valley – Landscape classifications



Kathmandu Valley brings together distinct landscape systems, from mountain slopes and headwaters to foothills, river corridors and the highly developed urban basin.
Different landscapes perform different functions within the valley’s water system.
Understanding these landscape zones helps identify where water can be retained, where natural drainage needs to be protected, and where urban areas can introduce new opportunities for infiltration, storage and safe conveyance.
Flood Risk Hotspots
Across KMC, flood risk is not random. 13 flood clusters emerge along the city’s river and drainage network, revealing where water, urbanisation and infrastructure pressures intersect.
A city shaped by water
Bishnumati · Bagmati · Dhobikhola · Manohara
Most clusters trace these river systems and their tributaries — showing how local flooding is connected to the wider urban watershed.
Different places, different pressures
The clusters cut across dense neighbourhoods, markets, major roads, institutional areas, public spaces and culturally important parts of the city. Flooding therefore affects more than property — it can disrupt movement, access, public life and sensitive urban landscapes.
Where risk meets opportunity