Are we facing another very dry period for the summer of 2026/27 due to a change from La Niña to El Niño?
The latest ECMWF seasonal forecast system (SEAS5) indicates a heightened likelihood that El Niño conditions will develop during 2026 and persist into the 2026/27 summer, although there remains uncertainty regarding the eventual strength of the event due to the spring predictability barrier. Current model guidance shows a transition from ENSO‑neutral conditions to El Niño during the second half of 2026, with El Niño the most likely ENSO state through summer 2026/27.
An intensifying El Niño, combined with rising temperatures driven by climate change, is expected to significantly increase the risk of very dry conditions across parts of New Zealand.
In New Zealand, El Niño conditions are typically associated with more frequent westerly airflow, leading to enhanced rainfall in the west of the country and a greater risk of dry conditions in eastern regions, including Otago, Marlborough, Hawkes Bay, Canterbury, etc. During stronger El Niño events, this pattern can substantially reduce rainfall and river inflows from non‑alpine catchments. While the extreme global impacts often highlighted by international agencies are less likely to occur locally, El Niño can place significant strain on water demand and supply, particularly for foothills‑ and rainfall‑fed systems, where restrictions can be prolonged during dry summers.
The influence of El Niño on atmospheric circulation tends to be strongest from December through February, coinciding with the peak of the irrigation season in Canterbury. At this stage it is too early to state with confidence that summer 2026/27 will be a drought, but historical experience shows that some of Canterbury’s most severe droughts have occurred during El Niño years, including 1972–73, 1982–83, 1997–98, and 2015–16. When historical climate data are combined with current levels of irrigation and municipal demand in water‑supply simulations, the summer of 1972–73 consistently emerges as one of the periods of greatest stress on regional water resources.
Following the 1997–98 drought, the Canterbury Strategic Water Study, commissioned by the Canterbury Mayoral Forum in response to concern that Canterbury’s water resources were under unsustainable pressure, found that while the region has sufficient water overall, it is often unavailable at the right place or time. Water storage is therefore critical for managing seasonal variability. Although some progress has been made, gaps remain – particularly in preparing for severe El Niño‑related droughts – and improving short‑term resilience also supports long‑term climate change adaptation. The situation in other east coast regions is likely to be similar: the national-scale assessment of Water Availability and Security commissioned by MPI in 2021 found that opportunities for expansion of high-value land uses with sufficient resilience to climate variability and change would likely depend on the development of storage-based water infrastructure.
Experience from the 2015–16 El Niño drought illustrates this clearly. Irrigators supplied from alpine river systems generally coped well, especially where access to stored alpine water was available. In contrast, many foothills‑sourced schemes were subject to full or partial restrictions from Christmas through to late summer. The following irrigation season highlighted a compounding risk: successive summers with high water demand and limited winter recharge placed considerable pressure on groundwater levels, reducing system resilience even in less extreme climatic conditions.
While there is uncertainty around the precise conditions that will prevail in summer 2026/27, the emerging ENSO signal suggests that a more precautionary approach to water management is warranted. Managing demand early in the season as if drought is a possibility is prudent. Unlike floods, droughts develop slowly and are often well advanced before their impacts are fully recognised. Water users operating under annual volume limits should closely track usage, as the likelihood of allocations being fully utilised – or constrained by restrictions – is higher in El Niño‑influenced summers.