Winter and summer blocking variability in the North Atlantic region – evidence from long-term observational and proxy data from southwestern Greenland

We investigate the interannual and decadal variability of the North Atlantic atmospheric blocking frequency and distribution in connection with long-term observational and proxy records from southwestern Greenland. It is shown that warm (cold) conditions in southwestern Greenland during winter are r...

Full description

Bibliographic Details
Published in:Climate of the Past
Main Authors: Rimbu, N., Lohmann, G.
Format: Text
Language:English
Published: 2018
Subjects:
Online Access:https://doi.org/10.5194/cp-7-543-2011
https://cp.copernicus.org/articles/7/543/2011/
_version_ 1821523200228458496
author Rimbu, N.
Lohmann, G.
author_facet Rimbu, N.
Lohmann, G.
author_sort Rimbu, N.
collection Copernicus Publications: E-Journals
container_issue 2
container_start_page 543
container_title Climate of the Past
container_volume 7
description We investigate the interannual and decadal variability of the North Atlantic atmospheric blocking frequency and distribution in connection with long-term observational and proxy records from southwestern Greenland. It is shown that warm (cold) conditions in southwestern Greenland during winter are related with high (low) blocking activity in the Greenland-Scandinavian region. The pattern of winter temperature-blocking variability is more complex than the blocking pattern associated to the North Atlantic Oscillation (NAO). We find, furthermore, that a North Atlantic blocking index is significantly correlated with seasonally resolved stable isotope records from Greenland ice cores. Both suggest a possible reconstruction of blocking variability in this region. During summer, high (low) blocking activity in the Euro-Atlantic region is associated with cold (warm) conditions in southwestern Greenland. We conclude that historical temperature records, as well as proxy data from Greenland, can be used to obtain information related to interannual and multidecadal variation of winter and summer blocking during past periods.
format Text
genre Greenland
Greenland ice cores
North Atlantic
North Atlantic oscillation
genre_facet Greenland
Greenland ice cores
North Atlantic
North Atlantic oscillation
geographic Greenland
geographic_facet Greenland
id ftcopernicus:oai:publications.copernicus.org:cp2196
institution Open Polar
language English
op_collection_id ftcopernicus
op_container_end_page 555
op_doi https://doi.org/10.5194/cp-7-543-2011
op_relation doi:10.5194/cp-7-543-2011
https://cp.copernicus.org/articles/7/543/2011/
op_source eISSN: 1814-9332
publishDate 2018
record_format openpolar
spelling ftcopernicus:oai:publications.copernicus.org:cp2196 2025-01-16T22:04:53+00:00 Winter and summer blocking variability in the North Atlantic region – evidence from long-term observational and proxy data from southwestern Greenland Rimbu, N. Lohmann, G. 2018-09-27 application/pdf https://doi.org/10.5194/cp-7-543-2011 https://cp.copernicus.org/articles/7/543/2011/ eng eng doi:10.5194/cp-7-543-2011 https://cp.copernicus.org/articles/7/543/2011/ eISSN: 1814-9332 Text 2018 ftcopernicus https://doi.org/10.5194/cp-7-543-2011 2020-07-20T16:26:08Z We investigate the interannual and decadal variability of the North Atlantic atmospheric blocking frequency and distribution in connection with long-term observational and proxy records from southwestern Greenland. It is shown that warm (cold) conditions in southwestern Greenland during winter are related with high (low) blocking activity in the Greenland-Scandinavian region. The pattern of winter temperature-blocking variability is more complex than the blocking pattern associated to the North Atlantic Oscillation (NAO). We find, furthermore, that a North Atlantic blocking index is significantly correlated with seasonally resolved stable isotope records from Greenland ice cores. Both suggest a possible reconstruction of blocking variability in this region. During summer, high (low) blocking activity in the Euro-Atlantic region is associated with cold (warm) conditions in southwestern Greenland. We conclude that historical temperature records, as well as proxy data from Greenland, can be used to obtain information related to interannual and multidecadal variation of winter and summer blocking during past periods. Text Greenland Greenland ice cores North Atlantic North Atlantic oscillation Copernicus Publications: E-Journals Greenland Climate of the Past 7 2 543 555
spellingShingle Rimbu, N.
Lohmann, G.
Winter and summer blocking variability in the North Atlantic region – evidence from long-term observational and proxy data from southwestern Greenland
title Winter and summer blocking variability in the North Atlantic region – evidence from long-term observational and proxy data from southwestern Greenland
title_full Winter and summer blocking variability in the North Atlantic region – evidence from long-term observational and proxy data from southwestern Greenland
title_fullStr Winter and summer blocking variability in the North Atlantic region – evidence from long-term observational and proxy data from southwestern Greenland
title_full_unstemmed Winter and summer blocking variability in the North Atlantic region – evidence from long-term observational and proxy data from southwestern Greenland
title_short Winter and summer blocking variability in the North Atlantic region – evidence from long-term observational and proxy data from southwestern Greenland
title_sort winter and summer blocking variability in the north atlantic region – evidence from long-term observational and proxy data from southwestern greenland
url https://doi.org/10.5194/cp-7-543-2011
https://cp.copernicus.org/articles/7/543/2011/