A global blended tropopause based on ERA data, Part I: Climatology

[thumbnail of 951_ftp.pdf]
Text - Published Version
· Please see our End User Agreement before downloading.
[thumbnail of Wilcox_part1_centaur.pdf]
Preview
Text - Accepted Version
· Please see our End User Agreement before downloading.
| Preview

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

Wilcox, L. orcid id iconORCID: https://orcid.org/0000-0001-5691-1493, Hoskins, B. and Shine, K. orcid id iconORCID: https://orcid.org/0000-0003-2672-9978 (2012) A global blended tropopause based on ERA data, Part I: Climatology. Quarterly Journal of the Royal Meteorological Society, 138 (664). pp. 561-575. ISSN 1477-870X doi: 10.1002/qj.951

Abstract/Summary

A new tropopause definition, based on a flow-dependent blending of the traditional thermal tropopause with one based on potential vorticity, has been developed. The benefits of such a blending algorithm are most apparent in regions with synoptic scale fluctuations between tropical and extratropical airmasses. The properties of the local airmass determine the relative contributions to the location of the blended tropopause, rather than this being determined by a specified function of latitude. Global climatologies of tropopause height, temperature, potential temperature and zonal wind, based on European Centre for Medium-Range Weather Forecasts (ECMWF) reanalysis (ERA) ERA-Interim data, are presented for the period 1989-2007. Features of the seasonal-mean tropopause are discussed on a global scale, alongside a focus on selected monthly climatologies for the two high latitude regions and the tropical belt. The height differences between climatologies based on ERA-Interim and ERA-40 data are also presented. Key spatial and temporal features seen in earlier climatologies, based mainly on the World Meteorological Organization thermal tropopause definition, are reproduced with the new definition. Tropopause temperatures are consistent with those from earlier climatologies, despite some differences in height in the extratropics.

Altmetric Badge

Item Type Article
URI https://reading-clone.eprints-hosting.org/id/eprint/25077
Identification Number/DOI 10.1002/qj.951
Refereed Yes
Divisions Science > School of Mathematical, Physical and Computational Sciences > Department of Meteorology
Uncontrolled Keywords ERA-Interim;high latitudes;Tropics;ENSO
Publisher Royal Meteorological Society
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