2017
DOI: 10.1007/s41748-017-0011-0
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Multidecadal Changes in the Relationship of Storm Frequency over Euro-Mediterranean Region and ENSO During Boreal Winter

Abstract: Background The El Niño-Southern Oscillation (ENSO) influence over Euro-Mediterranean boreal winter season (December to February) precipitation anomalies has changed along the twentieth century. Purpose The precipitation anomalies are closely associated with storm track frequency. The changing relationship between the interannual variability of storm track frequency and ENSO is investigated at interannual and multidecadal timescales. Methods The Melbourne University cyclone tracking scheme (MS) is applied to re… Show more

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Cited by 18 publications
(16 citation statements)
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“…Similar trend behavior was observed for the wet season rainfall data ( Figure 3b). The wet season- The wet season rainfall spatial distribution patterns are influenced through the Mediterranean and central Asian troughs [49,50]. Wet season rainfall distributions show maxima in the central parts of Saudi Arabia, with values of more than 150 mm (Figure 2c,d).…”
Section: Rainfall Variability and Trendsmentioning
confidence: 99%
“…Similar trend behavior was observed for the wet season rainfall data ( Figure 3b). The wet season- The wet season rainfall spatial distribution patterns are influenced through the Mediterranean and central Asian troughs [49,50]. Wet season rainfall distributions show maxima in the central parts of Saudi Arabia, with values of more than 150 mm (Figure 2c,d).…”
Section: Rainfall Variability and Trendsmentioning
confidence: 99%
“…erefore, the uncertainty at each location must be considered for climate change impact studies using model data. Further study may require using data from the newly developed Saudi-KAU Global Climate Model and focusing on the simulation of climate over the Arabian Peninsula [52][53][54].…”
Section: Maximum Temperature At Some Major Cities In Saudimentioning
confidence: 99%
“…Our results indicate further drying of the middle‐east region during post‐1980 La Niñas (Figure c). It may be related to changes in post‐1980 IO SST and winter storm activity (Kamil et al, ). Consistent with CRU observations, IMD observational data set also documents similar changes (Figures d–f) in rainfall patterns during post‐1980 La Niña (up to 6% reduction in ISM rainfall), thereby confirming that the results are not just artifacts of data processing.…”
Section: Resultsmentioning
confidence: 99%