Accessibility navigation


A minimal model to diagnose the contribution of the stratosphere to tropospheric forecast skill

Charlton-Perez, A. J. ORCID: https://orcid.org/0000-0001-8179-6220, Broecker, J. ORCID: https://orcid.org/0000-0002-0864-6530, Karpechko, A. Y. ORCID: https://orcid.org/0000-0003-0902-0414, Lee, S. H. ORCID: https://orcid.org/0000-0003-0986-0093, Sigmond, M. ORCID: https://orcid.org/0000-0003-2191-9756 and Simpson, I. R. ORCID: https://orcid.org/0000-0002-2915-1377 (2021) A minimal model to diagnose the contribution of the stratosphere to tropospheric forecast skill. Journal of Geophysical Research: Atmospheres, 126 (24). ISSN 2169-8996

[img]
Preview
Text (Open Access) - Published Version
· Available under License Creative Commons Attribution.
· Please see our End User Agreement before downloading.

1MB
[img] Text - Accepted Version
· Restricted to Repository staff only
· The Copyright of this document has not been checked yet. This may affect its availability.

918kB

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

To link to this item DOI: 10.1029/2021JD035504

Abstract/Summary

Many recent studies have confirmed that variability in the stratosphere is a significant source of surface sub-seasonal prediction skill during Northern Hemisphere winter. It may be beneficial, therefore, to think about times in which there might be windows-of-opportunity for skillful sub-seasonal predictions based on the initial or predicted state of the stratosphere. In this study, we propose a simple, minimal model that can be used to understand the impact of the stratosphere on tropospheric predictability. Our model purposefully excludes state dependent predictability in either the stratosphere or troposphere or in the coupling between the two. Model parameters are set up to broadly represent current sub-seasonal prediction systems by comparison with four dynamical models from the Sub-Seasonal to Seasonal Prediction Project database. The model can reproduce the increases in correlation skill in sub-sets of forecasts for weak and strong lower stratospheric polar vortex states over neutral states despite the lack of dependence of coupling or predictability on the stratospheric state. We demonstrate why different forecast skill diagnostics can give a very different impression of the relative skill in the three sub-sets. Forecasts with large stratospheric signals and low amounts of noise are demonstrated to also be windows-of-opportunity for skillful tropospheric forecasts, but we show that these windows can be obscured by the presence of unrelated tropospheric signals.

Item Type:Article
Refereed:Yes
Divisions:Science > School of Mathematical, Physical and Computational Sciences > Department of Meteorology
ID Code:102160
Publisher:American Geophysical Union

Downloads

Downloads per month over past year

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

Page navigation