2021
DOI: 10.1007/s00382-021-05770-4
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Evaluation of multiple downscaling tools for simulating extreme precipitation events over Southeastern South America: a case study approach

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Cited by 17 publications
(14 citation statements)
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“…On the other hand, the models and the observations show high consistency in increasing drought events in the NES region. All of the above align with previous studies (Almeida et al 2017 ; da Silva et al 2019 ; Olmo and Bettolli 2021 ; Solman et al 2021 ; Medeiros and Oliveira 2022 ).…”
Section: Resultssupporting
confidence: 91%
“…On the other hand, the models and the observations show high consistency in increasing drought events in the NES region. All of the above align with previous studies (Almeida et al 2017 ; da Silva et al 2019 ; Olmo and Bettolli 2021 ; Solman et al 2021 ; Medeiros and Oliveira 2022 ).…”
Section: Resultssupporting
confidence: 91%
“…However, some discrepancies among the REMO and RegCM ensembles were detected in areas like Amazonia and southeastern SA when considering ER as one of the extreme events involved in the CE occurrence (for HW + ER.s and DS + ER.s). Heavy rainfall is a complex phenomenon even for the high‐resolution modeling, especially in areas like southeastern SA, where the combination of multiple factors at different spatio‐temporal scales—such as mesoscale convective activity, frontal systems, the strengthening of the SALLJ and baroclinic instability conditions—strongly modulate the occurrence of these events (Lavín‐Gullón et al., 2021; Solman et al., 2021). Furthermore, the Amazon represents the largest tropical rainforest in the world—where land‐atmosphere interactions imply essential dynamical components of the climatic system—and precipitation variability is strongly affected by the Andes orographic effect, that interacts with regional atmospheric circulation, evidencing seasonal‐to‐intraseasonal circulation patterns (Espinoza et al., 2021; Sierra et al., 2021).…”
Section: Summary and Final Remarksmentioning
confidence: 99%
“…In the last decades, some studies have also analysed the uncertainties in the climate projections with a particular focus on South America (Bl azquez and Nuñez, 2013;Joetzjer et al, 2013;Torres and Marengo, 2013). In addition, some studies have analysed the projections of climate extremes events specifically for South America using the results of GCMs from CMIP3-6 (e.g., Marengo et al, 2010;Rusticucci et al, 2010;Natividade et al, 2017;Betts et al, 2018;Almazroui et al, 2021a) or derived from regional climate models or other downscaling methods (e.g., Boulanger et al, 2006Boulanger et al, , 2007Marengo et al, 2009Marengo et al, , 2013Mendes and Marengo, 2009;Valverde and Marengo, 2014;Bl azquez and Silvina, 2020;Avila-Diaz et al, 2020a, 2020bOlmo and Bettolli, 2021;Solman et al, 2021). However, in all the aforementioned studies, the approach to the uncertainties involved in the projection of climate extremes is still little discussed or analysed in depth.…”
Section: Introductionmentioning
confidence: 99%