A global hail climatology using the UK Met Office convection diagnosis procedure (CDP) and model analyses.
In: Meteorological Applications, Jg. 18 (2011-12-01), Heft 4, S. 446-458
Online
academicJournal
Zugriff:
Five years of UK Met Office global model analyses from 1 January 2004 to 31 December 2008 have been used to generate a global hail climatology at 1° latitude by 1° longitude resolution. Hail has been diagnosed from model vertical profiles of temperature and humidity using a simple algorithm based on a paper by Fawbush and Miller (). Results have been compared with published observational climatologies on both a global and regional basis. The model diagnoses compare favourably with the observed data with both orographic and seasonal signals. However, there are differences, and possible reasons for these are discussed. These include limitations of the simple algorithm, the difficulty of observing hail in sparsely populated areas and the problem of population growth influencing the number of hail reports. Copyright © 2011 Royal Meteorological Society and Crown Copyright [ABSTRACT FROM AUTHOR]
Copyright of Meteorological Applications is the property of Wiley-Blackwell and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)
Titel: |
A global hail climatology using the UK Met Office convection diagnosis procedure (CDP) and model analyses.
|
---|---|
Autor/in / Beteiligte Person: | Hand, Will H. ; Cappelluti, Gennaro |
Link: | |
Zeitschrift: | Meteorological Applications, Jg. 18 (2011-12-01), Heft 4, S. 446-458 |
Veröffentlichung: | 2011 |
Medientyp: | academicJournal |
ISSN: | 1350-4827 (print) |
DOI: | 10.1002/met.236 |
Schlagwort: |
|
Sonstiges: |
|