2015
DOI: 10.1002/joc.4425
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A cyclone climatology of the British‐Irish Isles 1871–2012

Abstract: ABSTRACT:The British-Irish Isles (BI) lie beneath the North Atlantic storm track year-round and thus are impacted by the passage of extra-tropical cyclones. Given recent extreme storminess and projections of enhanced winter cyclone activity for this region, there is much interest in assessing the extent to which the cyclone climate of the region may be changing. We address this by assessing a 142-year (1871-2012) record of cyclone frequency, intensity and 'storminess' derived from the 20th Century Reanalysis V… Show more

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Cited by 28 publications
(53 citation statements)
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“…As well as milder/wetter winters characterized by fewer rain‐on‐snow floods, reduced late twentieth century upland flooding is also related to an unusual run of positive summer NAO index values, strong negative rainfall anomalies and a marked decline in summer cyclonic flow. The latter is especially marked between 1961 and 1990 (Matthews et al, ) and corresponds with a reduction in heavy upland rainfall provided by cyclonic weather types (Burt and Horton, ; Burt and Ferranti, ). Such consistently positive summer NAO values have not been recorded in the last 150 years and tree‐ring reconstructions indicate they were last experienced in the early sixteenth century (Figure c; Folland et al, ; Linderholm et al, ).…”
Section: Rainfall Extreme Floods and The North Atlantic Oscillationsupporting
confidence: 58%
See 1 more Smart Citation
“…As well as milder/wetter winters characterized by fewer rain‐on‐snow floods, reduced late twentieth century upland flooding is also related to an unusual run of positive summer NAO index values, strong negative rainfall anomalies and a marked decline in summer cyclonic flow. The latter is especially marked between 1961 and 1990 (Matthews et al, ) and corresponds with a reduction in heavy upland rainfall provided by cyclonic weather types (Burt and Horton, ; Burt and Ferranti, ). Such consistently positive summer NAO values have not been recorded in the last 150 years and tree‐ring reconstructions indicate they were last experienced in the early sixteenth century (Figure c; Folland et al, ; Linderholm et al, ).…”
Section: Rainfall Extreme Floods and The North Atlantic Oscillationsupporting
confidence: 58%
“…Negative summer NAO index values indicate a southerly displacement of the north Atlantic storm track and cyclones towards the UK. Note that the probability of a cyclone over the British Isles is highest during late summer (Matthews et al, ), giving the potential for slow moving torrential downpours and boulder‐berm generation (Foulds et al, ). Positive summer NAO index values are associated with drier, warmer and sunnier weather in the UK and northwest Europe. Although usually drier than average, −NAO winters are often snowy, which increases the likelihood of severe rain‐on‐snow floods as polar or continental air masses are displaced by mild and wet Atlantic air masses (i.e.…”
Section: Rainfall Extreme Floods and The North Atlantic Oscillationmentioning
confidence: 99%
“…The years 1988The years , 1989The years and 1990 were also noteworthy at the time for being the warmest in the Central England Temperature series (Marsh and Monkhouse, 1993). Earlier drought periods in the 1970s were remarkable for the quiescence of summer cyclones (Matthews et al, 2015). Nonetheless, care must be taken when interpreting long-run, low-flow sequences because of their susceptibility to local artificial influences such as river regulation, effluent returns, water storage, or groundwater abstraction (in the case of the Wensum).…”
Section: Discussionmentioning
confidence: 99%
“…Further research is required to assess the extent to which changes in these and other synoptic drivers might be influencing the seasonality of drought terminations in the UK. For instance, Matthews et al (2016) report relatively low frequencies of summer cyclones in the period 1961-1990 but a marked resurgence in counts since the 1990s.…”
Section: Droughtmentioning
confidence: 99%