How much Northern Hemisphere precipitation is associated with extratropical cyclones?

Extratropical cyclones are often associated with heavy precipitation events and can have major socio‐economic impacts. This study investigates how much of the total precipitation in the Northern Hemisphere is associated with extratropical cyclones. An objective feature tracking algorithm is used to...

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Bibliographic Details
Published inGeophysical research letters Vol. 39; no. 24
Main Authors Hawcroft, M. K., Shaffrey, L. C., Hodges, K. I., Dacre, H. F.
Format Journal Article
LanguageEnglish
Published Washington, DC Blackwell Publishing Ltd 28.12.2012
American Geophysical Union
John Wiley & Sons, Inc
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Summary:Extratropical cyclones are often associated with heavy precipitation events and can have major socio‐economic impacts. This study investigates how much of the total precipitation in the Northern Hemisphere is associated with extratropical cyclones. An objective feature tracking algorithm is used to locate cyclones and the precipitation associated with these cyclones is quantified to establish their contribution to total precipitation. Climatologies are produced from the Global Precipitation Climatology Project (GPCP) daily dataset and the ERA‐Interim reanalysis. The magnitude and spatial distribution of cyclone associated precipitation and their percentage contribution to total precipitation is closely comparable in both datasets. In some regions, the contribution of extratropical cyclones exceeds 90/85% of the total DJF/JJA precipitation climatology. The relative contribution of the most intensely precipitating storms to total precipitation is greater in DJF than JJA. The most intensely precipitating 10% of storms contribute over 20% of total storm associated precipitation in DJF, whereas they provide less than 15% of this total in JJA. Key Points Extratropical cyclones contribute over 50% of NH precipitation Cyclones contribute up to 90/85% of precipitation in some regions in DJF/JJA The most intense storms contribute significantly to the total climatology
Bibliography:ark:/67375/WNG-7NV3SKSL-Z
istex:C62AF818A0E25700A8628BE4F5F3FB55F0AEE00C
ArticleID:2012GL053866
ObjectType-Article-1
SourceType-Scholarly Journals-1
ObjectType-Feature-2
content type line 23
ISSN:0094-8276
1944-8007
DOI:10.1029/2012GL053866