Search from over 60,000 research works

Advanced Search

Meridional energy transport extremes and the general circulation of Northern Hemisphere mid-latitudes: dominant weather regimes and preferred zonal wavenumbers

[thumbnail of Open access]
Preview
wcd-3-1037-2022.pdf - Published Version (21MB) | Preview
Available under license: Creative Commons Attribution
[thumbnail of Lemboetal2022.pdf]
Lemboetal2022.pdf - Accepted Version (8MB)
Restricted to Repository staff only
Add to AnyAdd to TwitterAdd to FacebookAdd to LinkedinAdd to PinterestAdd to Email

Lembo, V., Fabiano, F., Galfi, V. M., Graversen, R., Lucarini, V. orcid id iconORCID: https://orcid.org/0000-0001-9392-1471 and Messori, G. (2022) Meridional energy transport extremes and the general circulation of Northern Hemisphere mid-latitudes: dominant weather regimes and preferred zonal wavenumbers. Weather and Climate Dynamics, 3 (3). pp. 1037-1062. ISSN 2698-4016 doi: 10.5194/wcd-3-1037-2022

Abstract/Summary

The extratropical meridional energy transport in the atmosphere is fundamentally intermittent in nature, having extremes large enough to affect the net seasonal transport. Here, we investigate how these extreme transports are associated with the dynamics of the atmosphere at multiple spatial scales, from planetary to synoptic. We use the ERA5 reanalysis data to perform a wavenumber decomposition of meridional energy transport in the Northern Hemisphere mid-latitudes during winter and summer. We then relate extreme transport events to atmospheric circulation anomalies and dominant weather regimes, identified by clustering 500 hPa geopotential height fields. In general, planetary-scale waves determine the strength and meridional position of the synoptic-scale baroclinic activity with their phase and amplitude, but important differences emerge between seasons. During winter, large wavenumbers (k = 2–3) are key drivers of the meridional-energy-transport extremes, and planetary- and synoptic-scale transport extremes virtually never co-occur. In summer, extremes are associated with higher wavenumbers (k = 4–6), identified as synoptic-scale motions. We link these waves and the transport extremes to recent results on exceptionally strong and persistent co-occurring summertime heat waves across the Northern Hemisphere mid-latitudes. We show that the weather regime structures associated with these heat wave events are typical for extremely large poleward-energy-transport events.

Altmetric Badge

Item Type Article
URI https://reading-clone.eprints-hosting.org/id/eprint/106793
Item Type Article
Refereed Yes
Divisions Interdisciplinary Research Centres (IDRCs) > Centre for the Mathematics of Planet Earth (CMPE)
Science > School of Mathematical, Physical and Computational Sciences > Department of Mathematics and Statistics
Publisher European Geosciences Union
Download/View statistics View download statistics for this item

Downloads

Downloads per month over past year

University Staff: Request a correction | Centaur Editors: Update this record

Search Google Scholar