India’s climate resilience requires linking monsoon forecasting, disaster management and urban infrastructure. Analyse this requirement using the northeast monsoon and Bay of Bengal cyclone risk. (250 words)

The northeast monsoon supplies a major share of rainfall to the southeastern peninsula, while Bay of Bengal systems can rapidly intensify. Both demand forecast-led, locally implemented resilience.

• October–December rainfall is concentrated in Tamil Nadu, Puducherry, coastal Andhra Pradesh, Rayalaseema, south interior Karnataka and Kerala.
• El Niño often weakens the southwest monsoon but has an uncertain relationship with the northeast monsoon; historical variability makes seasonal averages insufficient.
• Warm seas, coastal exposure and dense urbanisation amplify cyclone, flood and storm-surge risks.

• Forecast uncertainty is wider for the northeast monsoon than for the southwest monsoon.
• Blocked drains, encroached wetlands, weak shelters and fragmented inter-State coordination convert heavy rain into urban disaster.
• Evacuation must reach informal settlements, elderly persons, children and persons with disabilities.

1. Combine IMD nowcasts with district-level impact forecasts and transparent uncertainty communication.
2. Pre-position SDRF/NDRF teams, shelters, medicines, power backups and resilient communications.
3. Restore wetlands, clear stormwater channels and enforce risk-sensitive coastal and urban planning.
4. Institutionalise after-action reviews and coordinate Centre, States, municipalities and communities.

northeast monsoon; ENSO; Bay of Bengal; IMD; deep depression; SDRF; NDRF; impact-based forecasting; wetlands; urban resilience.