Forecasting El Niño and La Niña events using decision tree classifier

dc.contributor.authorSilva, Karita Almeida [UNESP]
dc.contributor.authorde Souza Rolim, Glauco [UNESP]
dc.contributor.authorde Oliveira Aparecido, Lucas Eduardo [UNESP]
dc.contributor.institutionUniversidade Estadual Paulista (UNESP)
dc.date.accessioned2022-04-28T19:51:28Z
dc.date.available2022-04-28T19:51:28Z
dc.date.issued2022-01-01
dc.description.abstractThe El Niño-Southern Oscillation (ENSO) phenomenon affects the global climate by changing temperature and precipitation patterns mainly in tropical climatic regions and median latitudes. Such event strongly influences agricultural activities and crop yields. The Niño Oceanic Index (ONI) of the US National Oceanic and Atmospheric Administration (NOAA) describes and monitors ENSO intensity from ocean temperature measurements. When ONI in the Niño 3.4 region was + 0.5 °C above normal or − 0.5 °C below normal for 5 consecutive 3-month running averages, El Niño (EN) or La Niña (LN) events, respectively, were established. The prediction of ENSO events is made by modeling at major global weather centers by atmosphere–ocean coupling models; however, no articles were found using decision tree classifier (DTC) for ENSO forecasting purposes. This modeling approach requires much less computational time and capacity. Furthermore, DTC can be sufficiently accurate for agricultural purposes. Thus, the objective of this research was to forecast as early as possible the El Niño and La Niña yearly events using a DTC technique from ONI data from 1950 to 2020. We used as input variables for DTC quarterly ONI values from 15 quarters prior the data of forecasting. The DTC showed an accuracy of 89%, 84%, and 78% to predict La Niña, El Niño, and neutral years, respectively, without training period. For validation, the accuracy was 100%, 79%, and 79% for La Niña, El Niño, and neutral years, respectively. The selected ONI quarters were July–August-September, January–February-March, and February–March-April of the previous year and January–February-March of the current year, allowing an 8-month advance forecast with an average accuracy of 78% (validation).en
dc.description.affiliationDepartment of Mathematical Sciences and Engineering UNESP–São Paulo State University, SP
dc.description.affiliationUnespDepartment of Mathematical Sciences and Engineering UNESP–São Paulo State University, SP
dc.identifierhttp://dx.doi.org/10.1007/s00704-022-03999-5
dc.identifier.citationTheoretical and Applied Climatology.
dc.identifier.doi10.1007/s00704-022-03999-5
dc.identifier.issn1434-4483
dc.identifier.issn0177-798X
dc.identifier.scopus2-s2.0-85125849470
dc.identifier.urihttp://hdl.handle.net/11449/223577
dc.language.isoeng
dc.relation.ispartofTheoretical and Applied Climatology
dc.sourceScopus
dc.subjectBoreal spring
dc.subjectClimate anomalies
dc.subjectENSO
dc.subjectMachine learning
dc.subjectPython
dc.subjectSST anomalies
dc.titleForecasting El Niño and La Niña events using decision tree classifieren
dc.typeArtigo

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