Historical variability and lifecycles of North Atlantic midlatitude cyclones originating in the tropics

[thumbnail of Baker_et_al_2021_PTCs_v8_JGRAtm_accepted.pdf]
Text
- Accepted Version
· Restricted to Repository staff only
[thumbnail of Open access]
Preview
Text (Open access)
- Published Version
· Available under License Creative Commons Attribution Non-commercial No Derivatives.

Please see our End User Agreement.

It is advisable to refer to the publisher's version if you intend to cite from this work. See Guidance on citing.

Add to AnyAdd to TwitterAdd to FacebookAdd to LinkedinAdd to PinterestAdd to Email

Baker, A. J. orcid id iconORCID: https://orcid.org/0000-0003-2697-1350, Hodges, K. I. orcid id iconORCID: https://orcid.org/0000-0003-0894-229X, Schiemann, R. K. H. orcid id iconORCID: https://orcid.org/0000-0003-3095-9856 and Vidale, P. L. orcid id iconORCID: https://orcid.org/0000-0002-1800-8460 (2021) Historical variability and lifecycles of North Atlantic midlatitude cyclones originating in the tropics. Journal of Geophysical Research: Atmospheres, 126 (9). e2020JD033924. ISSN 2169-8996 doi: 10.1029/2020JD033924

Abstract/Summary

North Atlantic tropical and post‐tropical cyclones impact midlatitude regions, but the inhomogeneous observational record of the latter stages of tropical cyclones precludes many climatological analyses. The frequency of tropical‐origin storms basin‐wide is projected to increase under anthropogenic climate change, so establishing confidence in our knowledge of their historical variability and lifecycles—against which climate model simulations may be evaluated—is important. We used a Lagrangian feature‐tracking algorithm to identify tropical cyclones that impacted Northeast North America and Europe in seven global reanalysis datasets, distinguishing systems that retained warm‐core structures or underwent warm seclusion from those that underwent extratropical transition, acquiring cold‐core, frontal structures. Over the last four decades, ∼25 % and ∼10 % of tropical‐origin cyclones made landfall across Northeast North America and Europe, respectively, as warm‐core systems, with, on average, higher wind speeds than cold‐core systems. Historical warm‐ and cold‐core landfalls also exhibit distinct tracks, likely responding to differing steering flow and midlatitude conditions.

Altmetric Badge

Item Type Article
URI https://reading-clone.eprints-hosting.org/id/eprint/97427
Identification Number/DOI 10.1029/2020JD033924
Refereed Yes
Divisions Science > School of Mathematical, Physical and Computational Sciences > NCAS
Science > School of Mathematical, Physical and Computational Sciences > Department of Meteorology
Publisher American Geophysical 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