The emergence of a climate change signal in long-term Irish meteorological observations

• Published in: Weather and climate extremes 2023-12, Vol.42, p.100608, Article 100608
• Main Authors: Murphy, Conor, Coen, Amy, Clancy, Ian, Decristoforo, Victoria, Cathal, Steven, Healion, Kevin, Horvath, Csaba, Jessop, Christopher, Kennedy, Shane, Lavery, Rosalynd, Leonard, Kevin, McLoughlin, Ciara, Moore, Rory, O'Hare-Doherty, Daire, Paisley, Ricky, Prakash, Bipendra, Vatu, Julie, Thorne, Peter, Mateus, Carla, Ryan, Ciara, Noone, Simon
• Format: Article
• Language: English
• Subjects: Climate change; Extremes; Ireland; Precipitation; Signal to noise; Temperature
• ISSN: 2212-0947; 2212-0947
• DOI: 10.1016/j.wace.2023.100608

Detecting the emergence of a forced anthropogenic climate change signal from observations is critical for informing adaptation responses. By regressing local variations in climate onto annual Global Mean Surface Temperature (GMST), we track the emergence of an anthropogenic signal in long-term quality assured observations of temperature and precipitation for the island of Ireland, a sentinel location on the western European Atlantic seaboard. Analysis of station based observations, together with island scale composite series is undertaken for annual and seasonal means, together with 16 indices of extremes, with the derived signal-to-noise ratio classified as normal, unusual or unfamiliar relative to early industrial climate. More than half of indices show the emergence of at least unusual conditions relative to early industrial climate. The increase in annual mean temperature has led to the emergence of unfamiliar climate at six of eleven stations. Warming at the island scale is estimated at 0.88 °C per degree warming in GMST. While many stations show the emergence of unusual climate for spring, summer and autumn mean temperature, no forced signal of change is found for winter mean temperature. Changes in cool/warm days and nights are unfamiliar relative to early industrial climate. However, no anthropogenic signal is found for the hottest day annually or in summer – an extreme often associated with climate change in public consciousness. Increases in annual precipitation totals have emerged as unusual for western stations with large increases in winter totals per degree warming in GMST (e.g., 25.2% and 19.7% at Malin Head and Markree, respectively), indicating heightened flood risk with continued warming. By contrast, summer precipitation shows no significant relationship with GMST. Increases in rainfall intensity have emerged as unusual for 30% of stations, with increases consistent with the Clausius-Clapeyron relationship. Our analysis shows that an emerging climate change signal is discernible for Ireland, a location strongly influenced by climate variability.