El Niño 2026/27
1 in 46
SEAS5's October 2026 forecast of Nov–Mar rain in the south is drier than all 45 of its past October forecasts (seasons starting 1981–2025); 46 is the most a 45-year record can show. It ranks the forecast, not the rain to come (skill r = 0.32).
24%
of the south's forecast anomaly (-3.4 SD) goes with El Niño, if SEAS5's weak past relation to the ONI (r = -0.26) is extended to this year's record 2.16 °C
4 of 7
CERF drought allocations to Angola responded to El Niño seasons (3 seasons); 3 to La Niña seasons (2)
1.5–1.99 million
people in Phase 3+ at the peak (Aug 2026 – Jul 2027), FEWS NET estimate of August 2026
Driest 10% of forecasts for Nov–Mar: Moxico, Huíla, Namibe, Cuando Cubango, Cunene. Wettest 10%: Zaire, Uíge, Bengo, Lunda Norte, Cuanza Norte, Malanje, Lunda Sul, Cuanza Sul. Median skill r = 0.26 in the dry provinces and 0.47 in the wet ones; of the dry provinces, skill is 0.3 or more only in Huíla and Cuando Cubango. A return period of 46 means drier than every past October forecast; without removing the trend it is still the driest in 4 of the 5 dry provinces. In the south the forecast is 83% of the average past October forecast (-3.4 SD); the previous driest, for 1982/83, was 89% (-2.3 SD). The November forecast comes out around 6 November.
Dec–Feb is less dry in Moxico, Huíla and Namibe; in Cuando Cubango and Cunene it stays among the driest 10%. January is in the driest third only in Cuando Cubango. The three-month columns are the same numbers as the seas5-skill viewer for every province it shows.
Target areas will be added as rows once known.
| Province | Forecast Nov–Mar (return period) | Skill r | 2026 forecast (SD) / ENSO part (hindcast r with ONI) | El Niño seasons driest / wettest third | Rain–ONI r | Nov–Mar 2025/26 % of normal | 1 Sep–31 Oct 2026 % of normal | FEWS NET highest phase Oct 2026–Jan 2027 |
|---|---|---|---|---|---|---|---|---|
| Cabinda | 1 in 4 wet | 0.52 | +0.5 / +1.1 (+0.37) | 4 / 8 of 15 | +0.12 | 74% | 62% | 2 Stressed |
| Zaire | 1 in 12 wet | 0.49 | +1.4 / +1.5 (+0.49) | 2 / 6 of 15 | +0.09 | 59% | 57% | 1 Minimal |
| Uíge | 1 in 23 wet | 0.48 | +2.3 / +1.8 (+0.57) | 1 / 3 of 15 | +0.05 | 84% | 82% | 1 Minimal |
| Bengo | 1 in 15 wet | 0.49 | +1.7 / +1.7 (+0.55) | 1 / 6 of 15 | +0.15 | 50% | 61% | 1 Minimal |
| Lunda Norte | 1 in 23 wet | 0.46 | +2.8 / +2.2 (+0.70) | 3 / 8 of 15 | +0.24 | 101% | 96% | 1 Minimal |
| Cuanza Norte | 1 in 23 wet | 0.44 | +2.2 / +1.9 (+0.60) | 3 / 7 of 15 | +0.27 | 73% | 80% | 1 Minimal |
| Malanje | 1 in 46 wet | 0.49 | +2.6 / +2.0 (+0.64) | 3 / 9 of 15 | +0.29 | 96% | 85% | 1 Minimal |
| Luanda | 1 in 5 wet | 0.42 | +0.9 / +1.6 (+0.53) | 1 / 8 of 15 | +0.39 | 41% | — | 2 Stressed |
| Lunda Sul | 1 in 23 wet | 0.16 (low) | +1.5 / +1.6 (+0.52) | 3 / 5 of 15 | +0.16 | 97% | 100% | 1 Minimal |
| Cuanza Sul | 1 in 15 wet | 0.43 | +1.8 / +2.1 (+0.67) | 3 / 9 of 15 | +0.44 | 72% | 73% | 1 Minimal |
| Bié | 1 in 2 wet | 0.31 | +0.3 / +1.4 (+0.44) | 2 / 7 of 15 | +0.21 | 85% | 85% | 1 Minimal |
| Huambo | 1 in 3 wet | 0.38 | +0.4 / +1.6 (+0.53) | 0 / 8 of 15 | +0.38 | 77% | 75% | 1 Minimal |
| Benguela | 1 in 2 dry | 0.43 | -0.3 / +1.5 (+0.47) | 1 / 10 of 15 | +0.49 | 56% | 56% | 3 Crisis |
| Moxico | 1 in 23 dry | 0.13 (low) | -2.4 / -1.0 (-0.33) | 7 / 3 of 15 | -0.16 | 98% | 95% | 1 Minimal |
| Huíla | 1 in 46 dry | 0.41 | -1.8 / +0.7 (+0.24) | 5 / 7 of 15 | +0.28 | 87% | 72% | 3 Crisis |
| Namibe | 1 in 46 dry | 0.26 (low) | -2.3 / +0.2 (+0.08) | 5 / 5 of 15 | +0.04 | 72% | — | 3 Crisis |
| Cuando Cubango | 1 in 46 dry | 0.31 | -3.7 / -1.7 (-0.54) | 12 / 0 of 15 | -0.54 | 113% | — | 3 Crisis |
| Cunene | 1 in 46 dry | 0.22 (low) | -2.7 / -0.6 (-0.21) | 8 / 3 of 15 | -0.23 | 117% | — | 3 Crisis |
| South (Namibe, Huíla, Cunene, Cuando Cubango) | 1 in 46 dry | 0.32 | -3.4 / -0.8 (-0.26) | 9 / 4 of 15 | -0.31 | 105% | — | 3 Crisis |
| Angola | 1 in 2 dry | 0.38 | -0.1 / +1.0 (+0.33) | 5 / 5 of 15 | +0.06 | 93% | 86% | — |
Since 1 September: below 75% of normal in Cabinda 62%, Zaire 57%, Bengo 61%, Cuanza Sul 73%, Benguela 56%, Huíla 72%. Last season (2025/26) the south had 105% of normal Nov–Mar rain; it was the driest on record in Zaire, Bengo, Luanda.
Nov–Mar rain correlates with the ONI at −0.25 or below only in Cuando Cubango, and at +0.25 or above in 7 of 18 provinces. El Niño seasons in the driest third (of 15; chance 5): Cuando Cubango 12, Cunene 8, Namibe 5, Huíla 5. ERA5 agrees with CHIRPS on the sign in 88–100% of cells with |r| ≥ 0.2.
South: forecast -3.4 SD, of which -0.8 SD goes with the ONI, from a weak relation (r = -0.26) extended beyond any past ONI. October forecasts were also among the driest in Cunene, Cuando Cubango in 1982/83, 1997/98. Of the 4 strong El Niño seasons, 3 brought a driest-third Nov–Mar to the south (1982/83, 2015/16, 2023/24). ENSO goes with about 10% of the year-to-year variation in the south's Nov–Mar rain (r = -0.31).
CERF drought allocations for El Niño seasons: 2015/16, 2018/19 (2), 2023/24; for La Niña seasons: 2011/12, 2020/21 (2). The largest FEWS NET needs (2.5–5 million, 2021) followed the 2020/21 La Niña season.
FEWS NET estimates 750,000–999,999 people in Phase 3+ in September 2026 and 1.5–1.99 million at the peak (Aug 2026 – Jul 2027). Its seasonal calendar: rains October–May, lean season November–February, main cereal harvest March–June. IPC has analysed Angola twice, in the southern provinces only: 2019 (421 thousand in Phase 3+) and 2021 (1.3 million).
Attribution studies exist for 2015/16 and 2023/24 in southern Africa: the 2023/24 study leaves Angola out, the 2015/16 study does not say. We found none on the 2019–2021 drought in the south of Angola.
| Study | Area, season | Angola in it | Finding |
|---|---|---|---|
| Kimutai et al. 2024 (World Weather Attribution) | Zimbabwe, Botswana, and the southern parts of Zambia and Mozambique; Dec–Feb 2023/24 | No | El Niño made a drought like 2023/24 about twice as likely; climate change was not a significant driver. |
| Funk et al. 2018 | Southern Africa; Dec–Feb 2015/16 | Not stated | Warming likely made the 2015/16 El Niño stronger, which deepened the drought and the crop losses. |
| Lombe et al. 2026 | Cunene, Huíla, Namibe; 1980–2024 | Yes | 2019 and 2021 were extreme drought years in all three provinces, more so once evaporative demand is counted. ENSO is not tested; the only study we found that is specific to that drought. |
| Lourenço et al. 2023 | Angolan highlands; 1981–2020 | Yes | Eight drought periods since 1981; only two fell solely in El Niño years. |
| Moses et al. 2025 | Okavango basin, including the Cubango and Cuito headwaters; Dec–Feb, 1981–2024 | South-east | Over the Angolan headwaters the weak 2018/19 El Niño was drier than the strong 2023/24 one; more Atlantic moisture reached the basin in 2023/24. |
| Maphugwi et al. 2025 | Eastern Congo Air Boundary region; Jan–Mar, 1979–2024 | Unclear | All five driest late summers were El Niño years, 2023/24 the driest. The strong 1997/98 El Niño brought no drought there; the paper attributes this to an Angola Low that did not weaken. |
| Magadzire et al. 2026 | Southern Africa; rainy season, skill highest Dec–Feb | Partly (skill scored south of 15°S) | El Niño dries the central and southern interior, more so in moderate-to-strong events; little signal over central Angola and a wetter tilt in the west. Rainfall skill is higher in the north of the scored area, including south-eastern Angola (both from the preprint). |
| Howard et al. 2019 | Southern Africa; Dec–Feb | Yes | Rain-bearing tropical lows shift north in El Niño and south in La Niña; they carry much of Angola's year-to-year rainfall variation. |
| Crétat et al. 2019 | Angola and neighbouring countries; Nov–Mar, 1980/81–2014/15 | Yes | A weak or northward Angola Low brings rain to tropical and drought to subtropical southern Africa; weak Angola Low states correlate with rainfall more strongly than ENSO does. |
| Pomposi et al. 2018 | 15–35°S; Dec–Feb, 1981/82–2015/16 | South of 15°S | Below-normal rain in about 80% of strong El Niño seasons and just over 60% of moderate-to-weak ones; strong events weaken the Angola Low. |
| Hoell et al. 2015 | South of 15°S; Dec–Mar, 1950–2010 | South of 15°S | El Niño with a warm Indian Ocean brings less rain; El Niño with a cool Indian Ocean brings more. |
| Blamey et al. 2018 | Southern Africa; Oct–Mar, 2015/16 against past El Niños | Partly | 2015/16 was drier early in the season than past El Niños of similar strength because the Angola Low and the South Indian Ocean High were weak. |
| Nicholson and Kim 1997 | Africa; 1901–1990 | Yes | ENSO tends to bring opposite rainfall anomalies to equatorial and southern Africa. |
| Rouault et al. 2003 | Coast of Angola and Namibia; Feb–Apr | Coast | Warm sea off Angola and Namibia (Benguela Niños) goes with above-average rain on the coast, sometimes inland too. |
OCHA Centre for Humanitarian Data · built 2026-11-02