Forecasting El Niño and La Niña events using decision tree classifier
Autor(a) principal: | |
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Data de Publicação: | 2022 |
Outros Autores: | , |
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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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 |
|
_version_ |
1808129515898011648 |