Forecasting El Niño and La Niña events using decision tree classifier

Detalhes bibliográficos
Autor(a) principal: Silva, Karita Almeida [UNESP]
Data de Publicação: 2022
Outros Autores: de Souza Rolim, Glauco [UNESP], de Oliveira Aparecido, Lucas Eduardo [UNESP]
Tipo de documento: Artigo
Idioma: eng
Título da fonte: Repositório Institucional da UNESP
Texto Completo: http://dx.doi.org/10.1007/s00704-022-03999-5
http://hdl.handle.net/11449/223577
Resumo: The 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).
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spelling Forecasting El Niño and La Niña events using decision tree classifierBoreal springClimate anomaliesENSOMachine learningPythonSST anomaliesThe 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).Department of Mathematical Sciences and Engineering UNESP–São Paulo State University, SPDepartment of Mathematical Sciences and Engineering UNESP–São Paulo State University, SPUniversidade Estadual Paulista (UNESP)Silva, Karita Almeida [UNESP]de Souza Rolim, Glauco [UNESP]de Oliveira Aparecido, Lucas Eduardo [UNESP]2022-04-28T19:51:28Z2022-04-28T19:51:28Z2022-01-01info:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/articlehttp://dx.doi.org/10.1007/s00704-022-03999-5Theoretical and Applied Climatology.1434-44830177-798Xhttp://hdl.handle.net/11449/22357710.1007/s00704-022-03999-52-s2.0-85125849470Scopusreponame:Repositório Institucional da UNESPinstname:Universidade Estadual Paulista (UNESP)instacron:UNESPengTheoretical and Applied Climatologyinfo:eu-repo/semantics/openAccess2022-04-28T19:51:28Zoai:repositorio.unesp.br:11449/223577Repositório InstitucionalPUBhttp://repositorio.unesp.br/oai/requestopendoar:29462024-08-05T23:23:40.859303Repositório Institucional da UNESP - Universidade Estadual Paulista (UNESP)false
dc.title.none.fl_str_mv Forecasting El Niño and La Niña events using decision tree classifier
title Forecasting El Niño and La Niña events using decision tree classifier
spellingShingle Forecasting El Niño and La Niña events using decision tree classifier
Silva, Karita Almeida [UNESP]
Boreal spring
Climate anomalies
ENSO
Machine learning
Python
SST anomalies
title_short Forecasting El Niño and La Niña events using decision tree classifier
title_full Forecasting El Niño and La Niña events using decision tree classifier
title_fullStr Forecasting El Niño and La Niña events using decision tree classifier
title_full_unstemmed Forecasting El Niño and La Niña events using decision tree classifier
title_sort Forecasting El Niño and La Niña events using decision tree classifier
author Silva, Karita Almeida [UNESP]
author_facet Silva, Karita Almeida [UNESP]
de Souza Rolim, Glauco [UNESP]
de Oliveira Aparecido, Lucas Eduardo [UNESP]
author_role author
author2 de Souza Rolim, Glauco [UNESP]
de Oliveira Aparecido, Lucas Eduardo [UNESP]
author2_role author
author
dc.contributor.none.fl_str_mv Universidade Estadual Paulista (UNESP)
dc.contributor.author.fl_str_mv Silva, Karita Almeida [UNESP]
de Souza Rolim, Glauco [UNESP]
de Oliveira Aparecido, Lucas Eduardo [UNESP]
dc.subject.por.fl_str_mv Boreal spring
Climate anomalies
ENSO
Machine learning
Python
SST anomalies
topic Boreal spring
Climate anomalies
ENSO
Machine learning
Python
SST anomalies
description The 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).
publishDate 2022
dc.date.none.fl_str_mv 2022-04-28T19:51:28Z
2022-04-28T19:51:28Z
2022-01-01
dc.type.status.fl_str_mv info:eu-repo/semantics/publishedVersion
dc.type.driver.fl_str_mv info:eu-repo/semantics/article
format article
status_str publishedVersion
dc.identifier.uri.fl_str_mv http://dx.doi.org/10.1007/s00704-022-03999-5
Theoretical and Applied Climatology.
1434-4483
0177-798X
http://hdl.handle.net/11449/223577
10.1007/s00704-022-03999-5
2-s2.0-85125849470
url http://dx.doi.org/10.1007/s00704-022-03999-5
http://hdl.handle.net/11449/223577
identifier_str_mv Theoretical and Applied Climatology.
1434-4483
0177-798X
10.1007/s00704-022-03999-5
2-s2.0-85125849470
dc.language.iso.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv Theoretical and Applied Climatology
dc.rights.driver.fl_str_mv info:eu-repo/semantics/openAccess
eu_rights_str_mv openAccess
dc.source.none.fl_str_mv Scopus
reponame:Repositório Institucional da UNESP
instname:Universidade Estadual Paulista (UNESP)
instacron:UNESP
instname_str Universidade Estadual Paulista (UNESP)
instacron_str UNESP
institution UNESP
reponame_str Repositório Institucional da UNESP
collection Repositório Institucional da UNESP
repository.name.fl_str_mv Repositório Institucional da UNESP - Universidade Estadual Paulista (UNESP)
repository.mail.fl_str_mv
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