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Energy budget characteristics of the subseasonal Scandinavian pattern

Based on daily Japanese 55-year reanalysis data, this study analysed the daily energy budget characteristics of 94 Scandinavian (SCA) events in the positive phase during 62 winters from 1958 to 2020. Low-frequency circulation anomalies characterize the SCA events. The maintenance of low-frequency an...

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Bibliographic Details
Published in:Atmospheric research 2024-06, Vol.303, p.107313, Article 107313
Main Authors: Xing, Shaoying, Shi, Ning, Zhou, Botao
Format: Article
Language:English
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Summary:Based on daily Japanese 55-year reanalysis data, this study analysed the daily energy budget characteristics of 94 Scandinavian (SCA) events in the positive phase during 62 winters from 1958 to 2020. Low-frequency circulation anomalies characterize the SCA events. The maintenance of low-frequency anomalies mainly comes from the extraction of both available potential energy (APE) and kinetic energy (KE) from the background field during both the developing stage and the decaying stage. This energy conversion characteristic is related to the “locking” effect of the background field. During the developing stage, the interactions among the low-frequency circulation anomalies continuously generate KE, which is the main source for initiating the primary circulation anomalies around western Europe and the Scandinavian Peninsula. Meanwhile, the horizontal KE advection maintains the KE of the circulation anomalies around Lake Baikal. The decay process of the SCA events is mainly related to the damping effect on the APE due to diabatic heating and the interactions among the low-frequency circulation anomalies. The SCA event is a type of atmospheric internal dynamic pattern. •Developing stage of SCA events is dominated by the barotropic eddy term.•Decaying stage of SCA events is due to baroclinic eddy term and diabatic heating.•Background field has a locking effect on the formation of the SCA events.•The SCA events belong to an atmospheric internal dynamic pattern.
ISSN:0169-8095
1873-2895
DOI:10.1016/j.atmosres.2024.107313