Didier P. Monselesan, James S. Risbey, Benoit Legresy, Sophie Cravatte, Bastien Pagli, Takeshi Izumo, Christopher C. Chapman, Mandy Freund, Abdelwaheb Hannachi, Damien Irving, P. Jyoteeshkumar Reddy, Doug Richardson, Dougal T. Squire, Carly R. Tozer
{"title":"On the archetypal `flavours', indices and teleconnections of ENSO revealed by global sea surface temperatures","authors":"Didier P. Monselesan, James S. Risbey, Benoit Legresy, Sophie Cravatte, Bastien Pagli, Takeshi Izumo, Christopher C. Chapman, Mandy Freund, Abdelwaheb Hannachi, Damien Irving, P. Jyoteeshkumar Reddy, Doug Richardson, Dougal T. Squire, Carly R. Tozer","doi":"arxiv-2406.08694","DOIUrl":null,"url":null,"abstract":"El Ni\\~no-Southern Oscillation global (ENSO) imprint on sea surface\ntemperature comes in many guises. To identify its tropical fingerprints and\nimpacts on the rest of the climate system, we propose a global approach based\non archetypal analysis (AA), a pattern recognition method based on the\nidentification of extreme configurations in the dataset under investigation.\nRelying on detrended sea surface temperature monthly anomalies over the 1982 to\n2022 period, the technique recovers central and eastern Pacific ENSO types\nidentified by more traditional methods and allows one to hierarchically add\nextra flavours and nuances to both persistent and transient phases of the\nphenomenon. Archetypal patterns found compare favorably to phase identification\nfrom K-means, fuzzy C-means and recently published network-based\nmachine-learning algorithms. The AA implementation is modified for the\nidentification of ENSO phases in sub-seasonal-to-seasonal prediction systems\nand complements current alert systems in characterising the diversity of ENSO\nand its teleconnections. Tropical and extra-tropical teleconnection composites\nfrom various oceanic and atmospheric fields derived from the analysis are shown\nto be robust and physically relevant. Extending AA to sub-surface ocean fields\nimproves the discrimination between phases when the characterisation of ENSO\nbased on sea surface temperature is uncertain. We show that AA on detrended\nsea-level monthly anomalies provides a clearer expression of ENSO types.","PeriodicalId":501065,"journal":{"name":"arXiv - PHYS - Data Analysis, Statistics and Probability","volume":"76 1","pages":""},"PeriodicalIF":0.0000,"publicationDate":"2024-06-12","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"arXiv - PHYS - Data Analysis, Statistics and Probability","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/arxiv-2406.08694","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0
Abstract
El Ni\~no-Southern Oscillation global (ENSO) imprint on sea surface
temperature comes in many guises. To identify its tropical fingerprints and
impacts on the rest of the climate system, we propose a global approach based
on archetypal analysis (AA), a pattern recognition method based on the
identification of extreme configurations in the dataset under investigation.
Relying on detrended sea surface temperature monthly anomalies over the 1982 to
2022 period, the technique recovers central and eastern Pacific ENSO types
identified by more traditional methods and allows one to hierarchically add
extra flavours and nuances to both persistent and transient phases of the
phenomenon. Archetypal patterns found compare favorably to phase identification
from K-means, fuzzy C-means and recently published network-based
machine-learning algorithms. The AA implementation is modified for the
identification of ENSO phases in sub-seasonal-to-seasonal prediction systems
and complements current alert systems in characterising the diversity of ENSO
and its teleconnections. Tropical and extra-tropical teleconnection composites
from various oceanic and atmospheric fields derived from the analysis are shown
to be robust and physically relevant. Extending AA to sub-surface ocean fields
improves the discrimination between phases when the characterisation of ENSO
based on sea surface temperature is uncertain. We show that AA on detrended
sea-level monthly anomalies provides a clearer expression of ENSO types.