ENSO Map: Real-Time Sea Surface Temperature Anomaly

Track El Niño and La Niña conditions across the equatorial Pacific with this ENSO map — SST anomaly data across all Niño monitoring regions, updated from NOAA satellite observations.

ENSO Map — Real-time sea surface temperature anomaly visualization for El Niño tracking

What Is an ENSO Map?

An ENSO map visualizes sea surface temperature (SST) anomalies across the equatorial Pacific Ocean — the primary indicator of El Niño and La Niña conditions. Unlike a standard weather map, this visualization focuses on deviations from normal: red and orange shades show where the ocean is warmer than average (El Niño conditions), while blue shades indicate cooler-than-normal water (La Niña conditions). These maps are the single most important visual tool scientists use to track El Niño development in real time.

NOAA's satellite-based SST anomaly maps update daily, combining data from multiple polar-orbiting and geostationary satellites. This ENSO map page compiles key resources and explains how to interpret them — whether you're a researcher, farmer, fisher, or just tracking the 2026 event.

Niño Monitoring Regions on the ENSO Map

The equatorial Pacific is divided into four key monitoring regions. Each region tells a different part of the ENSO story — from the earliest warming signals off South America to the basin-wide index that defines El Niño strength.

Niño 1+2

0–10°S, 90°W–80°W
The easternmost region, directly off the coasts of Peru and Ecuador. This is where Peruvian fishermen first noticed El Niño. Warming here is often the earliest signal, but it does not always spread westward into a full basin-wide event.

Niño 3

5°N–5°S, 150°W–90°W
The eastern-central Pacific. Strong warming in Niño 3 indicates the eastern Pacific El Niño pattern — the classic configuration associated with the strongest global impacts.

Niño 3.4 KEY INDEX

5°N–5°S, 170°W–120°W
This is the one that matters most. NOAA uses Niño 3.4 as the official definition of El Niño/La Niña. When the 3-month running mean SST anomaly here reaches +0.5°C for 5 consecutive seasons, an El Niño is declared.

Niño 4

5°N–5°S, 160°E–150°W
The westernmost region near the dateline. Warming here is characteristic of "central Pacific El Niño" or "El Niño Modoki" — a different flavor of ENSO with distinct global impacts.

Real-Time ENSO Map Resources

These operational maps from NOAA and partner agencies provide the most current SST anomaly data. Bookmark this el nino tracker page to keep these resources in one place.

NOAA OSPO SST Anomaly

Daily global sea surface temperature anomaly map from NOAA's Office of Satellite and Product Operations. The definitive operational SST product, updated every 24 hours from polar orbiter data.

View SST Anomaly Map →

NOAA Coral Reef Watch

High-resolution SST anomaly maps focused on the tropical oceans. Includes 5km resolution data ideal for tracking ENSO development at fine spatial scales along coastlines and reef systems.

View Coral Reef Watch Maps →

CPC Niño Region Indices

Weekly and monthly SST anomaly values for all four Niño regions, tabulated alongside the official Oceanic Niño Index (ONI). The raw data behind every ENSO forecast.

View Niño Region Data →

IRI ENSO Forecast Plume

The International Research Institute's multi-model ensemble forecast — all major dynamical and statistical models in one visualization. Shows where ENSO is projected to go 6-12 months ahead.

View IRI Forecast Plume →

TAO/TRITON Buoy Array

Live data from 70 moored buoys strung across the equatorial Pacific. Shows real-time subsurface temperature profiles down to 500 meters — the hidden engine of ENSO evolution.

View TAO Array Data →

NOAA PSL Map Room

The Physical Sciences Laboratory's interactive ENSO map room with customizable time series, correlation maps, and historical composites for every Niño region.

View PSL Dashboard →

How to Read an ENSO Map

  1. Look at the color scale first. Red/orange = warmer than average (El Niño signal). Blue = cooler than average (La Niña signal). White/near-white = near-normal. The scale typically ranges from -5°C to +5°C anomaly.
  2. Find the equatorial band (5°N to 5°S). This east-west strip across the Pacific is the ENSO engine. Ignore SST anomalies elsewhere for ENSO purposes — they reflect different ocean dynamics.
  3. Check the eastern Pacific first (Niño 1+2 and Niño 3). Warming often begins here near South America, then propagates westward as the event matures. Early and strong warming in these eastern regions is the classic signature of a developing El Niño.
  4. Compare to Niño 3.4, the official metric. If Niño 3.4 shows +0.5°C or more for 5 consecutive 3-month periods, it's an official El Niño. If it reaches +2.0°C, it's a "super" event.
  5. Watch the subsurface. Surface anomaly maps only tell half the story. Subsurface ocean heat content (measured by TAO buoys and Argo floats) often shows warming at 100-200m depth weeks before it appears at the surface.

Pair This ENSO Map with Our Real-Time Dashboard

The el nino tracker dashboard complements these maps with live ONI charts, historical comparisons, and Niño region indices — all in one place, updated monthly from CPC data.

Open ENSO Dashboard →

Frequently Asked Questions About ENSO Maps

How often are ENSO maps updated?

Operational SST anomaly maps from NOAA OSPO are updated daily, with a 24-48 hour latency from satellite overpass to processed product. The CPC Niño region indices are updated weekly every Monday. The Oceanic Niño Index (ONI), which is the official 3-month running mean used to declare El Niño/La Niña, updates monthly — typically within the first week of each month. For the most current snapshot, check the daily OSPO anomaly map; for the official ENSO status, wait for the monthly ONI update.

What's the difference between an ENSO map and a regular weather map?

A regular weather map shows absolute conditions (e.g., today's temperature is 28°C). An ENSO map shows anomalies — how much warmer or cooler the ocean is compared to the long-term average for that date. An anomaly of +1.5°C in the equatorial Pacific is a strong El Niño signal, even though the absolute water temperature (e.g., 27°C) would be unremarkable in the tropics. This is why ENSO maps use red/blue diverging color scales rather than a single temperature gradient.

Can I use an ENSO map to predict weather in my area?

Partially, but with important caveats. An ENSO map tells you the state of the tropical Pacific — whether El Niño, La Niña, or neutral conditions are present. This gives you the statistical tendencies: for example, El Niño typically brings wetter winters to the southern US and drier conditions to Australia. But these are probabilities, not guarantees. Each event behaves differently based on its strength, location of peak warming, and interaction with other climate patterns (MJO, PDO, IOD). Use the ENSO map as a starting point, then check regional seasonal forecasts for your specific location. Source: NOAA CPC, IRI.

Where can I download raw ENSO map data?

NOAA provides free access to all operational SST data. The OISST v2.1 dataset (Optimum Interpolation Sea Surface Temperature) is the standard daily 0.25° resolution product used for most operational ENSO monitoring — available from NOAA NCEI. For higher resolution (5km), use the CoralTemp dataset from Coral Reef Watch. The ERSST v5 dataset provides the long historical record (1854-present) used for computing anomalies and the ONI. All are freely downloadable in NetCDF format.

Explore More El Niño Resources

Real-time

ENSO Dashboard

Live ONI charts, historical El Niño comparison, and Niño region indices — the companion tool to this ENSO map.

Monitoring

Monitoring & Prediction

TAO buoys, satellites, climate models — the full toolkit scientists use to produce the ENSO maps on this page.

Fundamentals

What Is El Niño

Understand the physics behind the SST anomalies you see on ENSO maps — from Walker Circulation to thermocline dynamics.