ATMOS / Overview
⚡ ATMOS: Adaptive Targeted Monsoon Optimization System — AI Rainfall Post-Processing.
DEMO DATA — NOT OPERATIONAL CYCLE: 14 AUG 2024 • 00:00 UTC NWP: 0.25° ➔ ATMOS: 0.05°
AI-POWERED REGIME-AWARE UNCERTAINTY-AWARE Enhancing NWP — Not Replacing It

Intelligent Post-Processing for Monsoon Rainfall Forecasts

ATMOS (Adaptive Targeted Monsoon Optimization System) learns regime-dependent errors in existing NWP rainfall forecasts and applies uncertainty-aware AI correction using atmospheric and geographical intelligence.

4 + 1 Regime Specialists + Global Expert
0.05° Target High-Resolution Grid
4 Monsoon Regime Classes
Multi-Metric Scientific Verification
INDIA RAINFALL FIELD (0.05°)

Interactive Indian Forecast Map

+24H • INDIA GRID
Active Synoptic Run: DEPRESSION / LOW (68%)
Launch Full Forecast Dashboard →

Why ATMOS?

Monsoon rainfall forecast errors vary across synoptic conditions. ATMOS dynamically tailors post-processing to prevailing regimes and local terrain.

01

REGIME-AWARE

Rainfall forecast errors can change significantly with monsoon synoptic conditions, requiring specialized AI experts.

02

UNCERTAINTY-AWARE

Continuous regime probabilities and Shannon entropy prevent rigid hard-switching between AI models.

03

LOCAL-AWARE

Terrain, elevation, slope aspect, and coastal distance refine precipitation field resolution locally to 0.05° (~5 km).

04

PROBABILISTIC

Heavy-rainfall exceedance probabilities complement deterministic forecasts for disaster decision support.

Four Monsoon Regime Classes

Distinct error distributions call for targeted AI post-processing strategies.

ACTIVE REG-ACT

Large-scale monsoon activity, strong low-level cross-equatorial southwesterly jet, and enhanced rainfall along the monsoon trough.

Typical NWP Failure Mode: Underestimates extreme windward orographic rain along Western Ghats.
ATMOS AI Specialist: Sharpens convective cores & applies slope aspect condensation multipliers.
BREAK REG-BRK

Monsoon trough shifts north to Himalayan foothills. Marked suppression of rainfall across central and peninsular India.

Typical NWP Failure Mode: Spurious "drizzle bias" (predicting 2-10 mm where zero rainfall falls).
ATMOS AI Specialist: Applies zero-hurdle probability filter to eliminate false precipitation.
DEPRESSION REG-DEP

Monsoon depression or cyclonic disturbance moving west-northwest from Bay of Bengal into Central India.

Typical NWP Failure Mode: Tracks low-pressure center well but under-predicts heavy rainband intensity.
ATMOS AI Specialist: Vorticity-guided heavy-rain realignment and extreme probability calibration.
TRANSITION REG-TRN

Atmospheric state undergoing transition between active and break phases with competing wave modes.

Typical NWP Failure Mode: High forecast variance and ensemble spread across operational runs.
ATMOS AI Specialist: Soft gating increases Global Model baseline weighting to prevent overfitting.

Foundational Innovations

Six scientific breakthroughs setting ATMOS apart from conventional NWP bias correction.

Operational Roadmap

Multi-stage progression from research sandbox to real-time national deployment.