Air Temperatures at Armagh Observatory, N. Ireland from 1796–2002

• Published in: International Journal of Climatology
• Main Authors: Butler, C. J., García Suárez, A. M., Coughlin, A. D. S., Morrell, C.
• Format: Article in Journal/Newspaper
• Language: unknown
• Published: 2005
• Subjects: North Atlantic; North Atlantic oscillation
• Online Access: https://zenodo.org/record/898682; https://doi.org/10.1002/joc.1148

Three independent mean temperature series for Armagh Observatory, covering the period 1796 – 2002 have been calibrated and corrected for the time of reading and exposure. Agreement between the three series is good in regions of overlap. With a short gap in the Armagh data from 1825 to 1833 filled by data from two stations in Dublin, the resulting series is the longest for the island of Ireland and one of the longest for any single site in the British Isles. Over the past 207 years, we note that temperatures in Armagh, in all seasons, show a gradual overall trend upwards. However, there are seasonal differences: summer and spring temperatures have increased by only half as much as those in autumn and winter. This is partly due to the exceptionally cold winters and autumns experienced prior to 1820. Relative to the overall trend, warm periods occurred in Ireland, as in other parts of Europe, in the mid-19th century, in the mid-20th century and at the end of the 20th century. Relatively cool temperatures prevailed in the early 19th century, in the 1880s and in the 1970s. Thus, if the baseline against which current temperatures are compared were moved from the late 19th century to include the earlier warm period, the apparent warming at the end of the late 20th century would be correspondingly reduced. A gradual decline in the daily temperature range at Armagh since 1844 may have resulted from higher minimum temperatures associated with increased cloudiness. A 7.8 year periodicity is identified in winter and spring mean temperatures at Armagh, which is probably a consequence of the North Atlantic oscillation.