Influence of the circumglobal wave-train on European summer precipitation

We investigate European summer (July-August) precipitation variability and its global teleconnections using the NCEP/NCAR reanalysis data (1950-2010) and a historical Coupled Model Intercomparison Project climate simulation (1901-2005) carried out using the ECHAM6/MPIOM climate model. A wavelike pat...

Full description

Bibliographic Details
Published in:Climate Dynamics
Main Authors: Saeed, S., Van Lipzig, N., Mueller, W., Saeed, F., Zanchettin, D.
Format: Article in Journal/Newspaper
Language:English
Published: 2014
Subjects:
Online Access:http://hdl.handle.net/11858/00-001M-0000-0014-3E8E-4
id ftpubman:oai:pure.mpg.de:item_1833496
record_format openpolar
spelling ftpubman:oai:pure.mpg.de:item_1833496 2024-09-15T18:23:48+00:00 Influence of the circumglobal wave-train on European summer precipitation Saeed, S. Van Lipzig, N. Mueller, W. Saeed, F. Zanchettin, D. 2014-07 http://hdl.handle.net/11858/00-001M-0000-0014-3E8E-4 eng eng info:eu-repo/semantics/altIdentifier/doi/10.1007/s00382-013-1871-0 http://hdl.handle.net/11858/00-001M-0000-0014-3E8E-4 Climate Dynamics info:eu-repo/semantics/article 2014 ftpubman https://doi.org/10.1007/s00382-013-1871-0 2024-07-31T09:31:27Z We investigate European summer (July-August) precipitation variability and its global teleconnections using the NCEP/NCAR reanalysis data (1950-2010) and a historical Coupled Model Intercomparison Project climate simulation (1901-2005) carried out using the ECHAM6/MPIOM climate model. A wavelike pattern is found in the upper tropospheric levels (200 hPa) similar to the summer circumglobal wave train (CGT) extending from the North Pacific to the Eurasian region. The positive phase of the CGT is associated with upper level anomalous low (high) pressure over western (eastern) Europe. It is further associated with a dipole-like precipitation pattern over Europe entailing significantly enhanced (reduced) precipitation over the western (eastern) region. The anomalous circulation features and associated summer precipitation pattern over Europe inverts for the negative CGT phase. Accordingly, the global teleconnection pattern of a precipitation index summarizing summer precipitation over Western Europe entails an upper level signature which consists of a CGT-like wave pattern extending from the North Pacific to Eurasia. The imprint of the CGT on European summer precipitation is distinct from that of the summer North Atlantic Oscillation, despite the two modes of variability bear strong similarities in their upper level atmospheric pattern over Western Europe. The analysis of simulated CGT features and of its climatic implications for the European region substantiates the existence of the CGT-European summer precipitation connection. The summer CGT in the mid-latitude therefore adds to the list of the modes of large-scale atmospheric variability significantly influencing European summer precipitation variability. © 2013 Springer-Verlag Berlin Heidelberg. Article in Journal/Newspaper North Atlantic North Atlantic oscillation Max Planck Society: MPG.PuRe Climate Dynamics 43 1-2 503 515
institution Open Polar
collection Max Planck Society: MPG.PuRe
op_collection_id ftpubman
language English
description We investigate European summer (July-August) precipitation variability and its global teleconnections using the NCEP/NCAR reanalysis data (1950-2010) and a historical Coupled Model Intercomparison Project climate simulation (1901-2005) carried out using the ECHAM6/MPIOM climate model. A wavelike pattern is found in the upper tropospheric levels (200 hPa) similar to the summer circumglobal wave train (CGT) extending from the North Pacific to the Eurasian region. The positive phase of the CGT is associated with upper level anomalous low (high) pressure over western (eastern) Europe. It is further associated with a dipole-like precipitation pattern over Europe entailing significantly enhanced (reduced) precipitation over the western (eastern) region. The anomalous circulation features and associated summer precipitation pattern over Europe inverts for the negative CGT phase. Accordingly, the global teleconnection pattern of a precipitation index summarizing summer precipitation over Western Europe entails an upper level signature which consists of a CGT-like wave pattern extending from the North Pacific to Eurasia. The imprint of the CGT on European summer precipitation is distinct from that of the summer North Atlantic Oscillation, despite the two modes of variability bear strong similarities in their upper level atmospheric pattern over Western Europe. The analysis of simulated CGT features and of its climatic implications for the European region substantiates the existence of the CGT-European summer precipitation connection. The summer CGT in the mid-latitude therefore adds to the list of the modes of large-scale atmospheric variability significantly influencing European summer precipitation variability. © 2013 Springer-Verlag Berlin Heidelberg.
format Article in Journal/Newspaper
author Saeed, S.
Van Lipzig, N.
Mueller, W.
Saeed, F.
Zanchettin, D.
spellingShingle Saeed, S.
Van Lipzig, N.
Mueller, W.
Saeed, F.
Zanchettin, D.
Influence of the circumglobal wave-train on European summer precipitation
author_facet Saeed, S.
Van Lipzig, N.
Mueller, W.
Saeed, F.
Zanchettin, D.
author_sort Saeed, S.
title Influence of the circumglobal wave-train on European summer precipitation
title_short Influence of the circumglobal wave-train on European summer precipitation
title_full Influence of the circumglobal wave-train on European summer precipitation
title_fullStr Influence of the circumglobal wave-train on European summer precipitation
title_full_unstemmed Influence of the circumglobal wave-train on European summer precipitation
title_sort influence of the circumglobal wave-train on european summer precipitation
publishDate 2014
url http://hdl.handle.net/11858/00-001M-0000-0014-3E8E-4
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
op_source Climate Dynamics
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1007/s00382-013-1871-0
http://hdl.handle.net/11858/00-001M-0000-0014-3E8E-4
op_doi https://doi.org/10.1007/s00382-013-1871-0
container_title Climate Dynamics
container_volume 43
container_issue 1-2
container_start_page 503
op_container_end_page 515
_version_ 1810464073789210624