dc.contributor.author
Osinski, Robert
dc.contributor.author
Lorenz, P.
dc.contributor.author
Kruschke, T.
dc.contributor.author
Voigt, M.
dc.contributor.author
Ulbrich, U.
dc.contributor.author
Leckebusch, G. C.
dc.contributor.author
Faust, E.
dc.contributor.author
Hofherr, T.
dc.contributor.author
Majewski, D.
dc.date.accessioned
2018-06-08T03:34:40Z
dc.date.available
2015-05-21T20:24:27.336Z
dc.identifier.uri
https://refubium.fu-berlin.de/handle/fub188/15484
dc.identifier.uri
http://dx.doi.org/10.17169/refubium-19672
dc.description.abstract
The properties of European wind storms under present climate conditions are
estimated on the basis of surface wind forecasts from the European Center of
Medium- Range Weather Forecast (ECMWF) Ensemble Prediction System (EPS). While
the EPS 5 is designed to provide forecast information of the range of possible
weather developments starting from the observed state of weather, we use its
archive in a climatological context. It provides a large number of
modifications of observed storm events, and includes storms that did not occur
in reality. Thus it is possible to create a large sample of storm events,
which entirely originate from a physically consistent model, 10 whose ensemble
spread represents feasible alternative storm realizations of the covered
period. This paper shows that the huge amount of identifiable events in the
EPS is applicable to reduce uncertainties in a wide range of fields of
research focusing on winter storms. Wind storms are identified and tracked in
this study over their lifetime using an algorithm, based on the local
exceedance of the 98th percentile of instanta15 neous 10m wind speed,
calculating a storm severity measure. After removing inhomogeneities in the
dataset arising from major modifications of the operational system, the
distributions of storm severity, storm size and storm duration are computed.
The overall principal properties of the homogenized EPS storm data set are in
good agreement with storms from the ERA-Interim dataset, making it suitable
for climatological investi20 gations of these extreme events. A demonstrated
benefit in the climatological context by the EPS is presented. It gives a
clear evidence of a linear increase of maximum storm intensity and wind field
size with storm duration. This relation is not recognizable from a sparse ERA-
Interim sample for long lasting events, as the number of events in the
reanalysis is not sufficient to represent these characteristics.
en
dc.rights.uri
http://creativecommons.org/licenses/by/3.0/
dc.subject.ddc
500 Naturwissenschaften und Mathematik::550 Geowissenschaften, Geologie::551 Geologie, Hydrologie, Meteorologie
dc.title
An approach to build an event set of European wind storms based on ECMWF EPS
dc.type
Wissenschaftlicher Artikel
dcterms.bibliographicCitation
Nat. Hazards Earth Syst. Sci. Discuss., 3, 1231–1268, 2015
dcterms.bibliographicCitation.doi
10.5194/nhessd-3-1231-2015
dcterms.bibliographicCitation.url
http://www.nat-hazards-earth-syst-sci-discuss.net/3/1231/2015/nhessd-3-1231-2015.html
refubium.affiliation
Geowissenschaften
de
refubium.affiliation.other
Institut für Meteorologie
refubium.funding
Deutsche Forschungsgemeinschaft (DFG)
refubium.mycore.fudocsId
FUDOCS_document_000000021972
refubium.note.author
Gefördert durch die DFG und den Open-Access-Publikationsfonds der Freien
Universität Berlin
refubium.resourceType.isindependentpub
no
refubium.mycore.derivateId
FUDOCS_derivate_000000004619
dcterms.accessRights.openaire
open access