One Acre Shield

ENSO per country forecasting·

Seasonal rainfall outlooks, ENSO and IOD tracking, and past-season rainfall impacts for One Acre Fund countries.
Start here
Country forecasts
ENSO + IOD analogs
Historical impact
Locust risk
Please read this page before you dig into the tabs. It takes about five minutes. It covers the two ocean drivers behind every number in this tool, what each tab is for, and what the historical record does and does not support, and explains any acronyms. Extra attention here will help you understand everything else better!

The basics

What El Niño is

Normally the trade winds push warm surface water westwards across the Pacific, piling it up near Indonesia. Every few years those winds weaken, the warm water slides back east and settles off South America. That is El Niño. La Niña is the same thing in reverse: stronger winds, colder water in the east.

2026 was a particularly interesting case. In early April a rare triplet of tropical cyclones spun up in the western Pacific, one north of the equator and two south of it. Their combined circulation drove a burst of westerly wind along the equator that reversed the trade winds and pushed warm water east. Niño 3.4 went from +0.26 °C on 8 April to +0.97 °C three weeks later, and the westerlies were running harder than the ones that preceded the 1997–98 super El Niño (Source 1). By late spring, forecasters were already putting the odds on a strong-to-historic event (Source 2).

This matters to us at One Acre Fund because a warmer Pacific changes tropical rainfall patterns around the world. The knock-on effects reach East and Southern Africa several months later.

To make this phenomenon measurable, scientists use average sea-surface temperature over one fixed rectangle in the central Pacific Ocean: 5°N to 5°S, 170°W to 120°W. That rectangle is called Niño 3.4. The temperature quoted everywhere is the anomaly, meaning how far the average sea-surface temperature in that rectangle sits above or below normal, in Celsius. Above +0.5 °C is El Niño, below −0.5 °C is La Niña, and about +1.5 °C upwards is a strong event.

Looping map of weekly sea-surface temperature anomaly across the Pacific this year, with the Niño 3.4 box marked.
Weekly sea-surface temperature against normal across the Pacific, this year so far. Orange is warmer than normal, blue is cooler. The white box is Niño 3.4, the rectangle described above, with its value for that week underneath. Watch the warm tongue build along the equator from April onwards and push east towards South America.

The second driver: the Indian Ocean Dipole

The Indian Ocean runs its own, smaller version of El Niño. The Dipole Mode Index (DMI) is simply the temperature difference between the Western Indian Ocean, off East Africa, and the Eastern Indian Ocean, off Indonesia.

A positive IOD means the West is unusually warm. Warm water evaporates, so there is more moisture in the air moving inland over East Africa, creating heavier than normal rainfall.

Equator WARM Western Indian Ocean COOL Eastern Indian Ocean moisture EAST AFRICA INDIA AUSTRALIA INDONESIA Positive IOD: warm west, cool east, more moisture reaching East Africa
The dashed boxes are the two patches of ocean the DMI is measured from. A negative IOD is the mirror image: a cool West, a warm East, and drier short rains.

The IOD normally only runs from about June to November and peaks around September to November, which lands squarely on the October-November-December (OND) period, or short rains in Kenya. That timing is the reason it matters so much in East Africa and much less in Southern Africa, where growing seasons start later.

Where things stand right now

What the terms meanWorth two minutes before reading the rest

The two ocean drivers
ENSO
El Niño Southern Oscillation. A swing in Pacific Ocean temperature that shifts rainfall right across the tropics, and the largest single source of skill in any seasonal forecast.
El Niño / La Niña
The warm phase and the cool phase of that swing.
Niño 3.4
The patch of central Pacific used to measure it (5°N to 5°S, 170°W to 120°W). Published weekly, which makes it the most current number on this page.
ONI
Oceanic Niño Index. A three-month average of Niño 3.4, and the figure NOAA uses to declare an official El Niño. Because it averages three months of data, and only comes out once the last of those months has finished, it lags well behind the weekly value while an event is still building.
IOD and DMI
Indian Ocean Dipole, and the index that measures it. The temperature difference between the Western and Eastern Indian Ocean. Positive means a warm West, which pushes moisture towards East Africa. It only runs from about June to November.
Anomaly
How far a value sits from its long-run average, in °C or in %.
Reading a forecast
Season codes
Three-letter runs of month initials. OND is October, November, December. MAM is March, April, May. DJF is December, January, February. JAS is July, August, September.
Tercile
One of three equal thirds of the historical record: driest, middle, wettest. The forecast maps give the chance of landing in each.
Above / below normal
In the wettest third, or in the driest third, measured against the 1991–2020 record.
Normal, or climatology
The 1991–2020 average. Every anomaly on this dashboard is measured against it.
Lead time
How far ahead the forecast reaches. Accuracy drops as lead grows.
Issue
The month IRI published a given forecast. A new one lands in the second week of each month.
Our data
OAF area, AEZ
The operating area every headline number is averaged over, built from farmer locations and agro-ecological zones (AEZ). Averaging over it rather than over the whole country sharpens the signal considerably.
TAMSAT
The satellite rainfall record behind the Historical impact tab, running back to 1983.
Composite
The average across every past year that shared a given phase, for example all El Niño years.
n
How many years went into an average. Small n means treat the number loosely.
pp
Percentage points, used here for the gap between two percentages.
ELR
Extended Logistic Regression, the statistical step that turns raw model output into the tercile probabilities on the forecast maps.

How to use this dashboard

1Read the status above. It tells you how unusual this season is, and it reads the same for every country.
2Open Country forecasts and pick your country. Read the summary and the green operations box under the map.
3Check it against Historical impact. See what the same ENSO phase actually did to your growing-season rainfall before you act on it.

Key findingsRecomputed from the historical record on every refresh

What this dashboard cannot tell you

  • These are probabilities. A 45 % chance of below-normal rainfall still leaves 55 % for everything else. Use a forecast to shift the odds on a decision you were already making, and do not treat a chance as a certainty!
  • The samples are small. Most seasons hold only 8 to 14 El Niño years. Every figure in the table above moves when one more year joins it, so lean on the direction more than on the exact percentage.
  • Weak means no information. Where the table says Weak, ENSO tells you nothing about that season, so plan for the full normal range of outcomes.
  • The March–June rains are grouped by the El Niño or La Niña before them. Those rains respond to an event that has already peaked rather than to the Pacific while they fall, so that is how the table groups them. The record here supports it, but it is still a modelling choice: group them by the concurrent reading instead and the numbers move.
  • Accuracy falls off with lead time. The further away a forecast period is, the lower accuracy becomes. So: don’t treat a forecast for a period 4–5 months away as a certain outcome. A lot can still happen and change!
  • ENSO is one driver among several. The IOD matters at least as much in East Africa. Nothing here captures what decides a harvest on the ground: planting date, dry spells inside an otherwise good season, soils, pests or storms. The agricultural season is a lot more complicated and can’t be reduced to ENSO and IOD alone!

IRI Multi-Model Probability Forecast for Precipitation, rendered per One Acre Fund country.

Filters

One Acre Fund country. The map zooms to its growing areas; the ENSO & locust tabs are global (the same for every country).

Show the rainfall outlook or the temperature outlook.

The future 3-month season being forecast. Codes are the months' initials — JJA = Jun-Jul-Aug, SON = Sep-Oct-Nov.

Most users can leave this at the latest. Drag back to compare older forecasts (the month IRI published them).

Colours show the chance the season lands in the wettest, middle, or driest third of the 1991–2020 record (for temperature: coolest / middle / warmest). Deeper colour = more confident; white = no clear signal. Green outline = OAF growing areas.iOAF — One Acre Fund. AEZ — agro-ecological zone (areas with similar climate & soils). Tercile — one of three equal thirds (driest / middle / wettest) of the 1991–2020 record.

Niño 3.4 trajectories from April onwardiNiño 3.4 — the central-equatorial Pacific sea-surface temperature anomaly that defines El Niño (warm) / La Niña (cool). An analog is a past year with a similar starting point.

Weekly Niño 3.4 anomaly (CPC OISST). Each colored line is what Niño 3.4 did over 18 months starting from April of a past El Niño year. The bright-green dotted line is the current trajectory — it extends week by week as CPC publishes new weekly values.

IOD (DMI) weekly trajectories from April onwardiIOD — Indian Ocean Dipole; DMI is its index, the western box minus the eastern box (50–70°E/10°S–10°N minus 90–110°E/10°S–0°). A positive IOD means a warm western Indian Ocean next to a cool east, which pulls convection toward Africa and boosts the East African short rains.

Weekly DMI (BoM, OISST-based). Colored lines are the 2015 & 2023 El Niño short-rains seasons; the bright-green dotted line is the current year, extending week by week as BoM publishes new values. (BoM's weekly record starts 2008, so older El Niño years aren't shown.) A positive IOD, meaning a warm western Indian Ocean beside a cool east, boosts the East African short rains: in El Niño years that also had a positive IOD, Kenya's short rains averaged +37.9% above normal, against −9.0% in El Niño years without one. See the Historical impact tab.

IRI/NMME ENSO forecast plume — Niño 3.4iENSO — El Niño–Southern Oscillation, the Pacific warm/cool cycle. NMME — North American Multi-Model Ensemble (the set of climate models). IRI publishes this plume; SST = sea-surface temperature.

Each thin grey line is one model's Niño 3.4 SST-anomaly forecast. Bold lines are the group means — red = dynamical, blue = statistical, white = all-model; gold = recent observations. Dotted lines mark El Niño strength bands (weak +0.5, moderate +1.0, strong +1.5, very strong +2.0) and La Niña (−0.5). Source: IRI's published plume, read back to its exact values at refresh (works offline).

Controls

All 10 OAF countries. Rainfall is averaged over the OAF growing areas where farmer locations are loaded, otherwise over the whole country. DRC is the exception: OAF works in the western strip (Kongo Central), so it is clipped to that region rather than averaged across the Congo basin.

Each country's actual growing season(s).

The map shows the average rainfall anomaly across those years.

Composite = the phase average. Or pick one season (or click a bar below) to see just that season's map. Each entry reads season months · the ENSO event and its peak strength; the full story is in the headline and the bar tooltips. Seasons that cross the new year are keyed like 2023/24, so a DJF row is never mistaken for calendar 2024. To hunt for past analogues, use the filter chips under the chart rather than this list.

Composite rainfall anomalyiRainfall this season vs the 1991–2020 normal, as a %. Greener = wetter, browner = drier. The headline aggregates over the OAF area (green outline); the map shows the spatial pattern. Source: TAMSAT satellite rainfall.

Greener = wetter than normal, browner = drier. Green outline = OAF growing areas.
Drier
Wetter  OAF area

Every year, by ENSO phase

Each bar = that season's rainfall anomaly over the OAF area in one past year, labelled by the season's own years (2023/24 where it crosses the new year). Hover a bar for the ENSO event behind it, and click to map it. Dashed lines = ENSO-phase composite means; the solid white line = the mean of the filtered selection. Stack the chips to pull out an analogue set: El Niño + very strong, or El Niño + positive IOD. The IOD is seasonal (active ~Jun–Nov, peak SON), so it discriminates years in the OND short rains and in the MAM rains that follow them; for the southern African DJF season nearly every year is Neutral IOD.
ENSO
StrengthiThe peak of the ENSO event this season belongs to, not the ONI during the season alone. So very strong on the Kenyan long rains returns 1998, 2016 and 2024 — the three seasons that followed a super El Niño — even though the Pacific had already cooled by the time those rains fell.
IODiIOD — Indian Ocean Dipole. Each season is grouped by the DMI (east–west Indian Ocean SST gradient) over the same reference window used for ENSO: ≥+0.4 = positive, ≤−0.4 = negative, in between = neutral. A positive IOD reinforces El Niño's wet signal in the East African short rains.
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Desert locust observations across Africa + Arabian Peninsula

Each dot is a PRESENT-state observation reported to FAO DLIS via the eLocust3 system. OAF country outlines are in bright green. Pan and zoom to drill into a region.