Bayesian Convolutional Neural Network (BCNN)

Hyderabad-based Indian National Centre for Ocean Information Services (INCOIS) has created a novel tool 

Key Highlights On Bayesian Convolutional Neural Network

  • The novel tool is Bayesian Convolutional Neural Network (BCNN).
  • Objective: The tool forecasts the onset of El Niño and La Niña phases of the El Niño Southern Oscillation (ENSO).
    • It predicts these climate patterns up to 15 months in advance.
    • According to the bulletin issued on June 5, it is highly likely (70-90% probability) that La Niña conditions will develop from July to September and persist until February 2025.

About Bayesian Convolutional Neural Network (BCNN)

  • It is a variant of the Convolutional Neural Network. 
    • It uses advanced technologies including Artificial Intelligence (AI), deep learning, and machine learning (ML).
  • It forecasts the onset of El Niño and La Niña phases of the El Niño Southern Oscillation (ENSO).
    • It can predict these climate patterns up to 15 months in advance.

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Functionality of the Model

  • Objective: BCNN aims to enhance forecasts related to El Niño and La Niña phases of the ENSO.
  • The model’s predictive capabilities leverage the connection between these phases and gradual oceanic changes, coupled with atmospheric interactions.

Operational Details

  • The model calculates predictions based on the Niño3.4 index value.
  • This index averages sea surface temperature (SST) anomalies in the central equatorial Pacific region, spanning from 5°N to 5°S and 170°W to 120°W.

Significance

  • Early Warning System: Provides early forecasts by analyzing oceanic variations and their atmospheric effects, offering valuable lead time for preparedness and planning.
  • Advancement in ENSO:  The Bayesian Convolutional Neural Network represents a significant advancement in ENSO prediction technology.
    • It aids in better understanding and preparation for climate variability linked to ocean-atmosphere interactions.

What is ENSO?

  • ENSO (El Niño Southern Oscillation) involves fluctuations in the temperature of waters in the central and eastern tropical Pacific Ocean, alongside changes in the overlying atmosphere.
  • Phases of ENSO
    • ENSO operates in irregular cycles lasting 2-7 years and manifests in three main phases: warm (El Niño), cool (La Niña), and neutral.
      • Neutral Phase: During the neutral phase, the eastern Pacific near South America is cooler due to prevailing east-to-west winds displacing warmer waters towards Indonesia.
      • El Niño Phase
        • In El Niño, weakened wind systems reduce the displacement of warm waters.
          • Consequently, the eastern Pacific becomes warmer than usual.
      • La Niña Phase
        • Conversely, in La Niña, strengthened wind systems intensify the displacement of warm waters towards Indonesia. 
          • It leads to cooler-than-normal conditions in the eastern Pacific.
  • Impact on India – Monsoon Effects
    • El Niño: Often results in a weak monsoon and heightened heat waves across India.
    • La Niña: Typically brings about a robust monsoon season in the region.

These phases of ENSO significantly influence global atmospheric circulation, thereby affecting weather patterns worldwide, including in India.

Comparison between Existing Models (Statistical & Dynamic) and BCNN Model

Feature Statistical Models Dynamic Models BCNN Model
Forecasting Approach Uses historical data and statistical relationships 3D mathematical simulations of the atmosphere Combines dynamic modeling with AI
Accuracy Less accurate Highly accurate Enhanced accuracy with AI
Lead Time Up to 6-9 months Up to 15 months for El Niño/La Niña Extends lead time significantly
Data Utilization Historical data sets Real-time data & past climate scenarios Historical runs from CMIP5/CMIP6 + existing data
Development Time Quicker to develop Requires high computational resources 8 months with testing phases
Application Scope Short to medium-term forecasts Detailed climate projections & specific phenomena Long-term ENSO predictions

Challenges in Developing BCNN

  • Limited Data: Weather forecasting models rely on historical data for training. While land-based data is plentiful, data for oceans is scarce, especially for long periods.
    • This scarcity of oceanic data especially impacts El Niño/La Niña prediction.
  • Scarcity in Oceanic Data: Global oceanic temperature records have only been reliably accessible since 1871.
    • This results in fewer than 150 monthly samples available for training deep learning models like BCNN for El Niño and La Niña predictions.
      • It limits the training dataset for such predictions.

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Overcoming Data Challenges

  • Incorporation of Historical Runs
    • Use of CMIP Data:
      • INCOIS addressed the data scarcity by integrating historical runs (1850-2014) from the Coupled Model Intercomparison Project phases 5 and 6 (CMIP5 and CMIP6).
      • This augmentation of the training dataset enriched the model’s capability to forecast ENSO phases.
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