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Teleconnections of the Quasi‐Biennial Oscillation in a multi‐model ensemble of QBO‐resolving models

Title: Teleconnections of the Quasi‐Biennial Oscillation in a multi‐model ensemble of QBO‐resolving models
Authors: Anstey, James A.; Simpson, Isla R.; Richter, Jadwiga H.; Naoe, Hiroaki; Taguchi, Masakazu; Serva, Federico; Gray, Lesley J.; Butchart, Neal; Hamilton, Kevin; Osprey, Scott; Bellprat, Omar; Braesicke, Peter; Bushell, Andrew C.; Cagnazzo, Chiara; Chen, Chih-Chieh; Chun, Hye-Yeong; Garcia, Rolando R.; Holt, Laura; Kawatani, Yoshio; Kerzenmacher, Tobias; Kim, Young-Ha; Lott, Francois; McLandress, Charles; Scinocca, John; Stockdale, Timothy N.; Versick, Stefan; Watanabe, Shingo; Yoshida, Kohei; Yukimoto, Seiji
Source: Quarterly journal of the Royal Meteorological Society, 148 (744), 1568-1592 ; ISSN: 0035-9009, 1477-870X
Publisher Information: John Wiley and Sons
Publication Year: 2021
Collection: KITopen (Karlsruhe Institute of Technologie)
Subject Terms: ddc:530; Physics; info:eu-repo/classification/ddc/530
Description: The Quasi-biennial Oscillation (QBO) dominates the interannual variability of the tropical stratosphere and influences other regions of the atmosphere. The high predictability of the QBO implies that its teleconnections could lead to increased skill of seasonal and decadal forecasts provided the relevant mechanisms are accurately represented in models. Here modelling and sampling uncertainties of QBO teleconnections are examined using a multi-model ensemble of QBO-resolving atmospheric general circulation models that have carried out a set of coordinated experiments as part of the Stratosphere-troposphere Processes And their Role in Climate (SPARC) QBO initiative (QBOi). During Northern Hemisphere winter, the stratospheric polar vortex in most of these models strengthens when the QBO near 50 hPa is westerly and weakens when it is easterly, consistent with, but weaker than, the observed response. These weak responses are likely due to model errors, such as systematically weak QBO amplitudes near 50 hPa, affecting the teleconnection. The teleconnection to the North Atlantic Oscillation is less well captured overall, but of similar strength to the observed signal in the few models that do show it. The models do not show clear evidence of a QBO teleconnection to the Northern Hemisphere Pacific-sector subtropical jet.
Document Type: article in journal/newspaper
File Description: application/pdf
Language: English
ISSN: 0035-9009; 1477-870X
Relation: info:eu-repo/semantics/altIdentifier/wos/000661618600001; info:eu-repo/semantics/altIdentifier/issn/0035-9009; info:eu-repo/semantics/altIdentifier/issn/1477-870X; https://publikationen.bibliothek.kit.edu/1000138078; https://publikationen.bibliothek.kit.edu/1000138078/127705981; https://doi.org/10.5445/IR/1000138078
DOI: 10.5445/IR/1000138078
Availability: https://publikationen.bibliothek.kit.edu/1000138078; https://publikationen.bibliothek.kit.edu/1000138078/127705981; https://doi.org/10.5445/IR/1000138078
Rights: https://creativecommons.org/licenses/by/4.0/deed.de ; info:eu-repo/semantics/openAccess
Accession Number: edsbas.8EA3E74E
Database: BASE