2021
DOI: 10.1007/s00382-021-05867-w
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Future changes in winter explosive cyclones over the Southern Hemisphere domains from the CORDEX-CORE ensemble

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Cited by 16 publications
(15 citation statements)
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“…The cyclogenetic region more to the northeast of R4 [142] registers an annual average of 26 cyclogeneses [146], a seasonal average of 7 cases in the summer [145], and a higher frequency in December [142]. Reboita et al [171] verified a positive trend of cyclone occurrence in R4 (on the coast of Uruguay) for the period 1980-2012, as well as a projection of increased cyclogenetic activity in the near (2020-2050) and far (2070-2099) futures [172,173], besides a positive trend of explosive extratropical cyclones, which form mainly on the coast of Uruguay and are associated with extreme winds and severe precipitation [174]. According to the authors, the increase in cyclogenetic activity near Uruguay may be a consequence of the intensification of the subtropical jet at upper levels and the moisture input at lower levels promoted by anomalous northeast-easterly winds from the South Atlantic Ocean [173].…”
Section: Cluster 4-region 4 (R4)mentioning
confidence: 94%
“…The cyclogenetic region more to the northeast of R4 [142] registers an annual average of 26 cyclogeneses [146], a seasonal average of 7 cases in the summer [145], and a higher frequency in December [142]. Reboita et al [171] verified a positive trend of cyclone occurrence in R4 (on the coast of Uruguay) for the period 1980-2012, as well as a projection of increased cyclogenetic activity in the near (2020-2050) and far (2070-2099) futures [172,173], besides a positive trend of explosive extratropical cyclones, which form mainly on the coast of Uruguay and are associated with extreme winds and severe precipitation [174]. According to the authors, the increase in cyclogenetic activity near Uruguay may be a consequence of the intensification of the subtropical jet at upper levels and the moisture input at lower levels promoted by anomalous northeast-easterly winds from the South Atlantic Ocean [173].…”
Section: Cluster 4-region 4 (R4)mentioning
confidence: 94%
“…In this work, we identify cyclones using an automatic scheme specifically developed for the Mediterranean region (Lionello et al 2002), and later adapted to hemispheric scales (Reale and Lionello 2013;Neu et al 2013). This algorithm has been extensively applied in previous studies (Lionello et al 2002;Lionello and Giorgi 2007;Reale and Lionello 2013;Neu et al 2013;Ulbrich et al 2013;Lionello et al 2016;Pinto et al 2016;Flaounas et al 2018;Lionello et al 2019;Reale et al 2019;Reboita et al 2020;Lionello et al 2020;Reboita et al 2021) and it is based on the search of pressure minima in a sequence of MSLP gridded fields. The procedure involves the partition of the MSLP field at time t 0 in a certain number of systems by identifying sets of steepest paths leading to the same MSLP minimum.…”
Section: Cyclone Detection and Tracking Algorithmmentioning
confidence: 99%
“…Regarding cyclone intensity, some studies showed the increase in the occurrence of strong cyclones, considering different intensity measurements for both the current climate (Pezza and Ambrizzi, 2003;Reboita et al, 2015) and future scenarios (Geng and Sugi, 2003;Lambert and Fyfe, 2006;Bengtsson et al, 2009). Moreover, Reboita et al (2021) found an increase of 13% in the occurrence of bomb cyclones in the South Atlantic Ocean, with the worst projected scenario (RCP8.5) presenting deeper, faster and shorter systems. An extratropical cyclone is called an explosive or bomb when it experiences fast deepening over a relatively short time, usually greater than 24 hPa in 24 hours (normalized at 60 • N, Sanders and Gyakum, 1980).…”
Section: Introductionmentioning
confidence: 99%