dc.creatorMora Serrano, Diego Esteban
dc.creatorMendoza Siguenza, Daniel Emilio
dc.creatorAviles Añazco, Alex Manuel
dc.creatorGarcia Avila, Fausto Fernando
dc.creatorMontenegro Ambrosi, Martin Patricio
dc.date.accessioned2023-01-12T16:14:59Z
dc.date.accessioned2023-05-22T16:32:51Z
dc.date.available2023-01-12T16:14:59Z
dc.date.available2023-05-22T16:32:51Z
dc.date.created2023-01-12T16:14:59Z
dc.date.issued2022
dc.identifier0920-4741, e 1573-1650
dc.identifierhttp://dspace.ucuenca.edu.ec/handle/123456789/40692
dc.identifierhttps://www.scopus.com/record/display.uri?eid=2-s2.0-85140432394&origin=resultslist&sort=plf-f&src=s&st1=Extreme+Rainfall+Variations+Under+Climate+Change+Scenarios.+Case+of+Study+in+an+Andean+Tropical+River+Basin&sid=3fc7e37eb45d82852ede20e39e516f19&sot=b&sdt=b&sl=122&s=TITLE-ABS-KEY%28Extreme+Rainfall+Variations+Under+Climate+Change+Scenarios.+Case+of+Study+in+an+Andean+Tropical+River+Basin%29&relpos=0&citeCnt=1&searchTerm=#author-keywords
dc.identifier10.1007/s11269-022-03332-9
dc.identifier.urihttps://repositorioslatinoamericanos.uchile.cl/handle/2250/6326240
dc.description.abstractMaximum rainfall events have triggered hazards that harm ecosystems and populations. Climate change could modify these extreme events, becoming more severe and frequent. Knowing the patterns of Spatio-temporal changes in the distribution of extreme rainfall in Andean regions represents a research challenge due to the complex climate behavior in the tropical mountain basins. The study aimed to analyze future Spatio-temporal changes in maximum daily rainfall patterns. The methods and analysis were performed in the Paute river basin in Ecuador through observed and simulated data from 1985 to 2005. The outputs of an ensemble regional climate model of Ecuador (RCM) based on CMIP5 models were used with two representative concentrations pathways (RCP), scenarios 4.5 and 8.5, in two future periods; future 1 from 2011 to 2040 and future 2 from 2041 to 2070. The General Extreme Value (GEV) distribution was used to fit the maximum annual daily rainfall. The maximum rainfall change factor between historical and future periods was calculated for 5,10,30, 60, and 100 years return periods. The results showed an increment of maximum rainfall spatial average in all return periods for RCP 4.5 and 8.5 in the future 1. Future 2 presented an increment of maximum rainfall spatial average in all return periods for RCP 4.5 and 8.5 scenarios except for the 30,60 and 100 years return periods of the RCP 4.5 scenario, displaying a decrease of maximum rainfall spatial average. Knowing rainfall pattern projections could help formulate actions to diminish the risks of extreme rainfall.
dc.languagees_ES
dc.sourceWater Resources Management
dc.subjectMaximum daily rainfall
dc.subjectAndean tropical river basin
dc.subjectCMIP5
dc.subjectGEV
dc.subjectClimate change
dc.titleExtreme rainfall variations under climate change scenarios. Case of study in an andean tropical river basin
dc.typeARTÍCULO


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