Winter 2015–2016 Irish Floods
📍 Clare · Shannon Lower / North Munster,Lee / Bandon / South Cork,Eastern (Dublin/Wicklow),Corrib,Liffey / Boyne
What caused it
The winter of 2015–16 was characterised by an exceptionally active Atlantic jet stream positioned far south, driven by one of the strongest El Niño events on record. This configuration directed a succession of powerful Atlantic storm systems directly at Ireland and the British Isles throughout December 2015 and January 2016.
Storm Desmond (4–5 December 2015) was the opening blow: 24-hour rainfall records were broken across Connacht and Ulster, with 187 mm recorded at Glendalough, Co. Wicklow in 24 hours. The storm left soils across Ireland fully saturated.
Storm Eva (23–26 December) struck a fully saturated Ireland, producing rapid and severe flooding across Cork, Limerick, and the Shannon basin. Then Storm Frank (29–30 December) hit an Ireland still dealing with the aftermath of Eva, causing additional flooding and preventing any meaningful drainage of the Shannon system.
The combination of exceptional rainfall totals, El Niño's influence on the jet stream position, and the stepwise saturation of catchments created conditions that Ireland's flood infrastructure was entirely unable to handle.
What happened
The flooding of winter 2015–16 was unprecedented in its scale, duration, and geographic spread. The Shannon Valley experienced its worst flooding in 300 years of records. Athlone, Portumna, Banagher, Carrick-on-Shannon and dozens of smaller settlements along the Shannon were flooded for weeks, in some cases over a metre of water entering ground-floor properties.
Cork city flooded badly in Storm Eva, with the Lee overflowing again into the city centre and the Mardyke. Limerick city saw the Abbey River and the Shannon combine to flood the city quays and adjacent streets. Galway and Tuam were badly affected.
In Clare, the scale of flooding led to a State of Emergency declaration. The R462 causeway at Portumna was submerged, cutting off communities. Roads across Clare and Galway were impassable for weeks, with some rural residents entirely cut off.
The Irish Defence Forces conducted their largest peacetime operation since the 1947 snowstorm, deploying engineers, boats, and personnel across multiple counties. Sandbag defences in Cork, Limerick and Galway were overwhelmed repeatedly. The ESB again had to make emergency releases from Lee Valley dams in Storm Eva, repeating the controversial 2009 pattern.
7,500 properties were damaged nationally. 200+ roads were closed at the peak. The Irish Rail Dublin–Cork route was suspended for weeks.
Recovery — how long it took
Recovery from the 2015–16 floods was protracted and politically contentious. Some Shannon valley properties remained flooded until late January 2016. Total economic damage was estimated at over €1 billion — the most expensive natural disaster in Irish history.
The Irish government announced a €5 billion capital flood investment programme, with 118 flood relief schemes to be progressed over the following decade under the National Development Plan. The Shannon flood risk received particular attention, with a new Shannon Flood Risk State Agency Co-ordination Working Group given enhanced powers and resources.
Insurance became a major political issue: tens of thousands of properties in flood-risk areas were either uninsured or unable to get flood cover. The government began discussions with the insurance industry about a flood insurance reinsurance scheme, though this remained unresolved for years afterward.
The 2015–16 floods are generally regarded as the inflection point that forced Ireland to seriously confront its chronic underinvestment in flood defences.
What this tells us about future risk
The 2015–16 floods established several critical lessons for Irish flood risk management:
1. Multi-storm sequences are more dangerous than single events. A succession of storms hitting a fully saturated catchment produces exponentially worse flooding than the first storm alone would have caused.
2. El Niño years correlate strongly with enhanced Atlantic storm activity over Ireland and merit heightened preparedness from October through February.
3. The Shannon system has very long response times — weeks of elevated levels following peak rainfall — meaning any flood relief must be planned for sustained operations, not just emergency response.
4. Infrastructure designed for historical rainfall frequencies is systematically underprovided. Events described as "1-in-100-year floods" are now occurring every 10–15 years in some catchments, reflecting climate change effects on rainfall intensity.
Gauge stations that recorded elevated levels
| Station | River | County | Peak recorded | Exceeded threshold by |
|---|---|---|---|---|
| Carrigadrohid Headrace | Lee (Cork) | Cork | 3.050 m | +1.100 m |
| Ball's Bridge | Shannon (Lower) | Clare | 2.850 m | +0.950 m |
| Portumna Bridge | Shannon (Lower) | Galway | 2.650 m | +0.800 m |
| Clarecastle Barrage D/S | Fergus | Clare | 2.400 m | +0.750 m |
| Galway Barrage | Corrib | Galway | 2.200 m | +0.600 m |
News coverage and official reports
See which stations today share characteristics with this event.