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The recent La Niña event in tropical Pacific has officially ended according to NOAA March 2025 update with ENSO-neutral conditions now prevailing impacting global climate variability & seasonal forecast reliability.
| 
 Aspect  | 
 Details  | 
| 
 Event  | 
 End of La Niña & onset of ENSO-neutral conditions in March 2025  | 
| 
 Agency  | 
 NOAA (National Oceanic & Atmospheric Administration, USA)  | 
| 
 Previous Phase  | 
 A short, mild La Niña phase from late 2024 to early 2025  | 
| 
 Current Phase  | 
 ENSO neutral sea surface temperatures (SSTs) & atmospheric indicators no longer meet La Niña thresholds  | 
| 
 SST Measurement  | 
 Niño 3.4 region SST ~ -0.01°C (much warmer than La Niña threshold of -0.5°C)  | 
| 
 Ocean Indicators  | 
 Warm water spread westward across eastern Pacific  | 
| 
 Atmospheric Indicators  | 
 Trade winds still strong but lack of cold SSTs ends La Niña classification  | 
| 
 Projection (2025)  | 
 >50% chance ENSO-neutral continues through August–October; ~43% chance it lasts into early winter  | 
| 
 Spring Predictability Barrier  | 
 Forecast confidence drops during spring due to natural atmospheric variability  | 
| 
 Historical Record  | 
 Recent La Niña may not qualify for historical inclusion (didn't meet 5 overlapping 3-month criteria)  | 
| 
 Parameter  | 
 El Niño  | 
 La Niña  | 
 ENSO-Neutral  | 
| 
 SST Anomaly (Niño 3.4)  | 
 ≥ +0.5°C above normal  | 
 ≤ –0.5°C below normal  | 
 Between –0.5°C & +0.5°C  | 
| 
 Trade Winds  | 
 Weakened or reversed  | 
 Strengthened  | 
 Near-normal  | 
| 
 Walker Circulation  | 
 Weakened (eastward shift)  | 
 Strengthened (westward shift)  | 
 Balanced  | 
| 
 Rainfall in Pacific  | 
 Increased in east-central Pacific, dry in west  | 
 Enhanced in western Pacific, dry in east  | 
 Typical seasonal variability  | 
| 
 Effect on Indian Monsoon  | 
 Suppressed monsoon (weak rainfall)  | 
 Strengthened monsoon (good rainfall)  | 
 Uncertain & variable  | 
| 
 Impact on South America  | 
 Flooding in Peru, drought in Amazon  | 
 Drought in Peru, floods in Australia  | 
 Normal seasonal variation  | 
| 
 Global Influence  | 
 Warming events globally  | 
 Cooling events globally  | 
 No significant global anomaly  | 
| 
 Duration  | 
 9–12 months  | 
 9–12 months  | 
 Transitional (can last months)  | 
| 
 Parameter  | 
 El Niño Impact  | 
 La Niña Impact  | 
 ENSO-Neutral Impact  | 
| 
 Monsoon Onset  | 
 Delayed  | 
 Early or on time  | 
 Normal or slightly delayed  | 
| 
 Total Rainfall  | 
 Deficit (~10–20% below normal)  | 
 Surplus (~5–15% above normal)  | 
 Near-normal but unpredictable  | 
| 
 Intra-seasonal Variability  | 
 Higher dry spells  | 
 Better distribution  | 
 Unstable, harder to forecast  | 
| 
 Cyclone Activity (Arabian/Bay)  | 
 Suppressed in Bay of Bengal  | 
 Enhanced in Bay & Arabian Sea  | 
 Variable  | 
| 
 Temperature in India  | 
 Warmer summer & drier soil  | 
 Cooler summer, better soil moisture  | 
 Near-normal but unpredictable  | 
| 
 Agriculture Impact  | 
 Reduced kharif yields, food inflation  | 
 Boost in crop output, better sowing  | 
 Depends on local patterns  | 
| 
 Reservoir Levels  | 
 Low inflow  | 
 High inflow  | 
 Balanced or region-specific variability  | 
| 
 Policy Implication  | 
 Need for drought planning, import support  | 
 Fertilizer demand, irrigation stable  | 
 Uncertainty in contingency planning  | 
For more information, please refer to IAS GYAN
Sources:
| 
 PRACTICE QUESTION Q. While La Niña & El Niño offer climatic signals unpredictability of ENSO neutral phases complicates policy response. Analyze how ENSO neutral conditions affect Indian climate resilience strategies.  | 
								
								
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