El Niño 2026/27 · Guatemala, Honduras, El Salvador
Dry Corridor rainfall outlook for 2027: Primera and Postrera
An early indication of the two 2027 rainy seasons in Guatemala, Honduras and El Salvador, for drought anticipatory action readiness: Primera (May–August) and Postrera (September–November). For each country, the departments covered by the Dry Corridor drought framework and every department, it compares what a typical season brings with the range we expect for 2027. The evidence comes from past seasons after strong El Niño events, statistical models built on the Pacific and Atlantic Oceans, and the NMME seasonal forecasts.
Bottom line
Rainfall in the departments the Dry Corridor framework covers*. Typical is the 1991–2020 median: half of seasons are wetter, half drier.
- Primera totals do not lean dry. The evidence centres on a typical season (99–106% in the framework departments, 100–107% nationally). The likely 2027 ranges are as wide as the normal year-to-year range, so a dry Primera is neither ruled out nor more likely than usual.
- The documented risk is a late start to Primera. After strong El Niño winters the rains began 1–2 weeks late on average, and late over about half to three-quarters of the region, against about a third in other years. In 1983, 1992 and 1998 they started one to three weeks late across most of the region; 2024 was late under one of our two onset rules, 2016 in parts, and 2010 on time. In 1983, 1998 and 2016, May–June rain came in at 69–95% of typical in each of the three countries and their framework departments. This winter is far stronger than any of the six, and the models keep March–May 2027 warmer than in any of them.
- Postrera leans slightly below typical, within the noise (93–101% in the framework departments). It depends on the state of El Niño or La Niña in September–November 2027, which no forecast can tell yet. After past strong events, October–November rain was below typical in four of six years in most areas.
- Droughts in the record came while El Niño was under way, not the year after. Nine of the 14 drought years in EM-DAT since 1981 had El Niño conditions during the June–November rains; one (El Salvador, 1998) came the year after a strong event. The framework's reference drought years 2009, 2015 and 2018 were El Niño years, as was 2026, when Primera came in at 48–71% of typical.
- What could change this: El Niño lingering into mid-2027 (the models' own forecast, before correcting their past bias) would pull Primera toward 94–99%. 2023, with a similar mix of a warm Pacific and a very warm Atlantic, came in at 70–94%.
- For readiness: nothing here points to a drier-than-typical season, and the framework's first check of Primera 2027 is the SEAS5 forecast of 5 March 2027. The risk to plan around is a late or broken start in May on top of a failed Primera 2026 and a weak 2025 in Guatemala and Honduras, with needs expected to peak from April to August 2027.
* Guatemala: Chiquimula, Zacapa, Jalapa and El Progreso. Honduras: El Paraíso and Francisco Morazán; the framework's trigger area is five municipalities within them. El Salvador: Ahuachapán and Santa Ana; the framework's trigger uses a national average. This page does not reproduce the framework's trigger or its thresholds.
Where 2026 leaves things
2026 was an El Niño developing year, and it behaved like one. The framework activated in all three countries in March 2026 on the SEAS5 forecast for May–August. Primera 2026 then came in at 48–71% of typical in CHIRPS (51–71% in ERA5) across the three countries and their framework departments, after a Primera 2025 that was below typical in most areas (77–101%). Early Postrera rain is less clear: September 2026 came in at 86–95% of typical in CHIRPS but 64–95% in ERA5, and the two disagree most in El Salvador (95% against 64%). ERA5 has September–October at 71–97%, lowest in El Salvador. FEWS NET expects food insecurity in Guatemala and Honduras to peak between April and August 2027, so the 2027 Primera harvest is the recovery point.
| Area | Primera 2025 | Primera 2026 | Sep 2026 | Sep–Oct 2026 (ERA5) |
|---|
% of the 1991–2020 median, CHIRPS with ERA5 in brackets. CHIRPS from the IRI Data Library runs to September 2026, so September–October is ERA5 only.
Evidence, line by line
Each row is one way of estimating 2027 rainfall, as a share of a typical season. Bars show the likely range, where eight outcomes in ten would fall. For past seasons after strong El Niño winters, each dot is one year. Choose an area and a season.
How the combined outlook is built: the central value averages four central estimates: the median of the six past seasons in CHIRPS and in ERA5, and the two regressions. The likely range averages the regressions' 10th and 90th percentiles. Departments and framework areas use the same recipe. NMME is shown for each country as a check but left out of the combination: it covers whole countries only, its cross-validated skill is nil in Guatemala and modest elsewhere (0.26 in Honduras, 0.42 in El Salvador), and its 2027 tilt comes from its least reliable members (below).
Primera regressions relate log rainfall to the difference between Niño3.4 and the tropical North Atlantic in May–July (Enfield and Alfaro 1999). A warm Pacific dries Primera; a warm Atlantic wets it. This one predictor cross-validates better than Niño3.4 alone in every country and framework area (correlations of 0.25–0.72 with observed rainfall, against 0.06–0.60). The 2027 inputs come from the NMME runs of November: Niño3.4 at +0.68 ± 0.40 °C in May–July after scaling the models back to how their past forecasts verified (they have tended to keep El Niño too long), and the tropical Atlantic at +1.00 ± 0.33 °C, both on a 1991–2020 base. A very warm Atlantic offsets a lingering El Niño, which is why the regressions centre at 102–113%. Without the Atlantic term they centre at 81–95%. Separate Pacific and Atlantic terms fit about as well and centre at 96–121%; the single contrast is simpler and keeps 2027 inside the range seen before, even though an Atlantic at +1 °C is at the edge of the record. The warning case is 2023: its Pacific–Atlantic contrast was close to 2027's, the regressions fit it at 104–116%, and it came in at 70–94%. The model cannot tell an El Niño that is building, as in 2023, from one that is fading, as in 2027.
NMME (five models started in November) puts Primera at 106% in Guatemala, 110% in Honduras and 121% in El Salvador, its second-wettest of 37 November runs in each. The tilt comes mostly from CCSM4 and GEM5.2-NEMO, both at the wet end of their own records (GEM5.2-NEMO beyond it), and in El Salvador also from CFSv2. CESM1, the model with the best record here, is at 100–101%.
Postrera regressions relate log rainfall to Niño3.4 in September–November. The link is weak (cross-validated correlations of up to 0.33, none in El Salvador's framework departments, where the regression falls back to about typical), and the 2027 input is wide: +0.02 ± 0.66 °C, from the NMME September–October forecast, corrected as for Primera. If El Niño returned (+1 °C), Postrera would centre at about 89–92% of typical; if La Niña formed (−1 °C), at about 100–114%.
NMME covers only September–October of Postrera (four models; CFSv2 does not reach that far): 105% in Guatemala, 111% in Honduras, 101% in El Salvador. Only Honduras shows any skill at this range.
Why the Pacific and the Atlantic matter
The survey grades the Dry Corridor's El Niño signal as robust: El Niño dries the rainy season while it is under way, most in July–October (Dai and Wigley 2000; our ERA5 correlation for August–October is about −0.6 in all three countries). In the July–August canícula the link is as strong (r ≈ −0.6). In May–June it is weak or absent. The year after a strong event is different: El Niño fades, and the tropical North Atlantic, which warms in the months after an El Niño peak, adds rain. What matters for Primera is the contrast between the two oceans.
Primera rainfall in CHIRPS (% of the 1991–2020 median) against the May–July difference between Niño3.4 and the tropical North Atlantic (both on a 1991–2020 base). Points to the right had a Pacific warm relative to the Atlantic. Hover over a point for ERA5's value.
Postrera rainfall in CHIRPS (% of the 1991–2020 median) against September–November Niño3.4. The 2027 band uses the NMME forecast for September–October. Hover over a point for ERA5's value.
Where El Niño is heading. Niño3.4 reached +2.2 °C in October 2026 (1991–2020 base). CPC (8 October) expects a strong to very strong event through January–March 2027. The IRI plume of October still gives El Niño a 60% chance in May–July and 37% in June–August. The NMME runs of November average about +2 °C in March–May, +1 °C in May–July and about 0 by September–October, with a spread from La Niña to El Niño. After the seven strongest past winters in their record, the same models were too warm in May–July five times, by about 0.4 °C on average, and over all years their May–July forecasts have overshot. We therefore scale them back to how their past forecasts verified: May–July then sits at +0.68 °C and September–October at +0.02 °C.
The tropical Atlantic was +0.64 °C in September (PSL) and the models warm it to about +1.0 °C by May–July 2027, near the record warmth of 2010, 2023 and 2024. Among those three, 2010 brought a wet Primera as La Niña set in, 2024 a mixed one (84–122% of typical across the three countries and framework departments) as El Niño faded, and 2023 a dry one as El Niño built.
Timing: the start of Primera and the end of the rains
Onset is the first day from 15 April with at least 1 mm that starts three days totalling 20 mm or more, as long as no dry spell of ten days or more (days under 1 mm) follows in the 30 days after those three. It is computed on each 5 km CHIRPS cell for 1981–2025 and then averaged by area. As a check, a simpler rule (the first five days from 15 April totalling 25 mm, with no dry-spell test) gives the same three clearly late years and a smaller average delay. The end of the rains is the last day between 1 September and 28 November that starts three days totalling 20 mm or more. The maps show the median shift over the six seasons after strong El Niño winters.
Start of Primera
Median shift in onset after strong El Niño winters, in days; later is brown. Thick outlines: framework departments.
End of the rains (Postrera)
Median shift in the last heavy rain of the season after strong El Niño winters, in days; earlier is brown.
- A later start is the clearest timing signal. Onset came later than typical in 53 of 54 departments (median of the six seasons, by 6 to 21 days). Typical onset is about 1 May in El Salvador, 7 May in Guatemala and 15 May in Honduras. In 1983, 1992 and 1998 the rains started one to three weeks late across most of the region, under both onset rules. These are the three oldest of the six cases. 2024 was late across most of the region under the main rule but not the simpler one, 2016 was late in parts, and 2010 started on time (early under the simpler rule), which leaves the average delay at 8–14 days by country and framework area under the main rule (5–12 days under the simpler one). The share of the area with a late onset averaged 47–74% in those years, against roughly a quarter to a third in other years.
- How far it reaches. Seasons with El Niño under way were also late, by 4–9 days on average (five cases). Over all 45 years onset is later after a warmer December–February Pacific (correlations of 0.21–0.47), but most of that link comes from the six years above; without them it is weak. The NMME runs put March–May 2027 at about +2 °C, or about +1.5 °C after allowing for their warm bias after strong winters: warmer than in any of the six past cases (+0.4 to +1.0 °C), so 2027 is beyond the range these cases cover.
- The canícula (July–August) has not been the weak spot after strong events. July–August rain was at or above typical in three to six of the six years, depending on the area. Dry-spell counts from CHIRPS cannot be used here: it records rain on about 24–42 of the 62 days of July–August in a typical year, too many for spell lengths to mean much, so the canícula is judged on totals.
- No sign of an early end to Postrera. The last heavy rains came at about the usual time or later (median shifts of −3 to +15 days by department), even though October–November totals were below typical in four of six years in most areas.
By department: seasonal totals
Typical rainfall
1991–2020 median, CHIRPS, in mm. Thick outlines: framework departments.
Expected 2027, compared with typical
Central estimate, as a change from the typical total. Likely ranges are in the table below.
May–June after strong El Niño winters
October–November after strong El Niño winters
Median of the six past seasons, as a change from typical: the weak spot of each season.
Reading these maps
Departments differ far more in how much rain they normally get (about 410 mm in Islas de la Bahía to 1,480 mm in Suchitepéquez) than in the expected change for 2027 (−3% to +11%). The largest expected rises are in Valle, La Unión and Islas de la Bahía.
May–June is where past strong El Niño seasons fell short: the median of the six was below typical in 51 of 54 departments, down to about −20% in Izabal and Santa Rosa. Only Chiquimula, Jalapa and Choluteca are at or just above typical.
Typical Postrera ranges from about 360 mm in Totonicapán to 990 mm in Suchitepéquez. The expected change for 2027 is −10% to +3%, lowest in Chalatenango, Santa Ana and Chiquimula.
October–November fell short in the median of past strong El Niño seasons in 41 of 54 departments, most in northern Honduras (Santa Bárbara and Cortés, about −30%). The Honduran framework departments were the exception (El Paraíso +16%, Francisco Morazán +11%).
Show all department numbers as a table
What the impact record adds
The team's EM-DAT snapshot (records that start up to 2023) lists drought in Guatemala, Honduras or El Salvador starting in 14 different years since 1981. Nine of those years had El Niño conditions during the June–November rains (Niño3.4 of +0.5 °C or more in June–August or September–November): 1987, 1994, 1997, 2002, 2004, 2009, 2015, 2018 and 2023. Four had none: 2000, 2001, 2012 and 2014, the last just before the 2015 event, with a warm Pacific late in the year (+0.4 °C). One, El Salvador from May 1998, came the year after a strong El Niño, and fits the late, dry start of Primera described above. The 2014–2016 records span the 2015 event and the year after it.
Three of the framework's four reference drought years (2009, 2015 and 2018) were El Niño years, and the fourth (2014) led into one; 2026 fits too. So the conditions that the framework, and most past responses, were built around are those of a developing El Niño. 2027 is a different case: a year after, with less evidence and more uncertainty.
What to watch, and when
- 12 Nov 2026CPC ENSO update: strength and expected decay of the El Niño. The first refresh of this page.
- Mid-Nov, then monthlyIRI ENSO plume and NMME runs: how fast El Niño fades through May–July, and whether La Niña is forecast for late 2027.
- 5 Feb 2027SEAS5 February run: the first SEAS5 forecast that covers all of May–August.
- 5 Mar, 5 Apr, 5 MaySEAS5 runs that the Dry Corridor framework checks for Primera.
- Late Apr – JunObserved onset of Primera by department, and May–June totals: where the documented risk sits.
- Apr and Jun 2027Atlantic hurricane season outlooks: a fading El Niño and a warm Atlantic tend to favour an active season, so the Postrera risk may be floods as much as drought.
- 5 Jul, 5 Aug, 5 SepSEAS5 runs that the framework checks for Postrera (August and September only for El Salvador).
What would change this outlook: an El Niño that holds on into June–August, a cooler Atlantic than forecast, or SEAS5 runs from February to May that move Primera toward the dry end of the typical range.
Data, methods and caveats
Rainfall: CHIRPS v2.0 monthly (1981 to September 2026) and daily for April–November 1981–2025, from the IRI Data Library; ERA5 monthly by department from the team's admin-1 statistics. CHIRPS and ERA5 agree well here (correlations of 0.65–0.92 for seasonal totals). Department and framework-area averages are weighted by area with fractional cell coverage. Millimetre figures are on the CHIRPS scale. Boundaries: COD-AB admin 1.
Definitions: typical means the 1991–2020 median (the Haiti page in this series uses the average; the median makes a forecast with no information read as 100%). Each dataset is compared with its own median. The typical range covers 8 of 10 seasons, 1981–2025. Likely ranges run from the 10th to the 90th percentile. Strong El Niño winters have a December–February Niño3.4 of at least +1.0 °C: 1983, 1992, 1998, 2010, 2016 and 2024. Niño3.4 is NOAA PSL ERSSTv6 re-based to 1991–2020; the tropical North Atlantic index is NOAA PSL (HadISST, 1991–2020).
Regressions: fitted on 1981–2025, with uncertainty from both the 2027 ocean forecasts and the fit (bootstrap over years). The NMME ocean forecasts are calibrated by regressing the observed index on the four-model mean (CanESM5, GEM5.2-NEMO, CESM1, CCSM4) over 1991–2026. NMME rainfall comes from CanESM5, GEM5.2-NEMO, CESM1, CCSM4 and CFSv2, started in November 2026 (SPEAR and GEOS-S2S had no November run yet), with ranges from a model of observed rainfall given the forecast, scaled by each system's correlation with observations.
SEAS5 is not used: its November run reaches only May 2027.
EM-DAT is used under its non-commercial terms; only dates are summarised here.
Code: the analysis scripts and their outputs are in deep_dives/data/dry-corridor; the page is built by cadc_deep_dive.py.