Loss of Persistence of the North Atlantic Oscillation and its Biological Implication

Winter sea-level pressure fields in the northern hemisphere were analysed with respect to regimes and regime shifts (RS). Classification of the North Atlantic Oscillation (NAO) patterns resulted in the identification of two longer lasting climate regimes: a persistent NAO− period from 1976 to 1988 f...

Full description

Bibliographic Details
Published in:Frontiers in Ecology and Evolution
Main Authors: Joachim W. Dippner, Caroline eMöller, Ingrid eKröncke
Format: Article in Journal/Newspaper
Language:English
Published: Frontiers Media S.A. 2014
Subjects:
Online Access:https://doi.org/10.3389/fevo.2014.00057
https://doaj.org/article/1295ce96d5a645088b90b22ee949521e
id ftdoajarticles:oai:doaj.org/article:1295ce96d5a645088b90b22ee949521e
record_format openpolar
spelling ftdoajarticles:oai:doaj.org/article:1295ce96d5a645088b90b22ee949521e 2023-05-15T17:28:30+02:00 Loss of Persistence of the North Atlantic Oscillation and its Biological Implication Joachim W. Dippner Caroline eMöller Ingrid eKröncke 2014-09-01T00:00:00Z https://doi.org/10.3389/fevo.2014.00057 https://doaj.org/article/1295ce96d5a645088b90b22ee949521e EN eng Frontiers Media S.A. http://journal.frontiersin.org/Journal/10.3389/fevo.2014.00057/full https://doaj.org/toc/2296-701X 2296-701X doi:10.3389/fevo.2014.00057 https://doaj.org/article/1295ce96d5a645088b90b22ee949521e Frontiers in Ecology and Evolution, Vol 2 (2014) North Atlantic Oscillation Benthic macrofauna Persistency regime shift composite analysis AMOEBA model Evolution QH359-425 Ecology QH540-549.5 article 2014 ftdoajarticles https://doi.org/10.3389/fevo.2014.00057 2022-12-30T23:08:52Z Winter sea-level pressure fields in the northern hemisphere were analysed with respect to regimes and regime shifts (RS). Classification of the North Atlantic Oscillation (NAO) patterns resulted in the identification of two longer lasting climate regimes: a persistent NAO− period from 1976 to 1988 followed by a persistent NAO+ period from 1989 to 2000. A further persistent NAO− period from 1956 to 1966 cannot be related to climate regime shifts. After 2000, the NAO lost its persistence and the autocorrelation disappeared, while the variance in the benthic data increased. The consequence was a decrease in potential predictability. The impact of the 1988/89 and 2000/2001 RS on the dominant species and taxonomic groups of benthic macrofauna as well as on benthic community structure was evaluated using an AMOEBA model, a quantitative method used in water management to represent the status of the ecosystem. The model confirmed the effects of the smooth RS in 1988/1989 and the abrupt RS in 2000/2001 on the macrofauna communities provided by earlier data analyses. Article in Journal/Newspaper North Atlantic North Atlantic oscillation Directory of Open Access Journals: DOAJ Articles Frontiers in Ecology and Evolution 2
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic North Atlantic Oscillation
Benthic macrofauna
Persistency
regime shift
composite analysis
AMOEBA model
Evolution
QH359-425
Ecology
QH540-549.5
spellingShingle North Atlantic Oscillation
Benthic macrofauna
Persistency
regime shift
composite analysis
AMOEBA model
Evolution
QH359-425
Ecology
QH540-549.5
Joachim W. Dippner
Caroline eMöller
Ingrid eKröncke
Loss of Persistence of the North Atlantic Oscillation and its Biological Implication
topic_facet North Atlantic Oscillation
Benthic macrofauna
Persistency
regime shift
composite analysis
AMOEBA model
Evolution
QH359-425
Ecology
QH540-549.5
description Winter sea-level pressure fields in the northern hemisphere were analysed with respect to regimes and regime shifts (RS). Classification of the North Atlantic Oscillation (NAO) patterns resulted in the identification of two longer lasting climate regimes: a persistent NAO− period from 1976 to 1988 followed by a persistent NAO+ period from 1989 to 2000. A further persistent NAO− period from 1956 to 1966 cannot be related to climate regime shifts. After 2000, the NAO lost its persistence and the autocorrelation disappeared, while the variance in the benthic data increased. The consequence was a decrease in potential predictability. The impact of the 1988/89 and 2000/2001 RS on the dominant species and taxonomic groups of benthic macrofauna as well as on benthic community structure was evaluated using an AMOEBA model, a quantitative method used in water management to represent the status of the ecosystem. The model confirmed the effects of the smooth RS in 1988/1989 and the abrupt RS in 2000/2001 on the macrofauna communities provided by earlier data analyses.
format Article in Journal/Newspaper
author Joachim W. Dippner
Caroline eMöller
Ingrid eKröncke
author_facet Joachim W. Dippner
Caroline eMöller
Ingrid eKröncke
author_sort Joachim W. Dippner
title Loss of Persistence of the North Atlantic Oscillation and its Biological Implication
title_short Loss of Persistence of the North Atlantic Oscillation and its Biological Implication
title_full Loss of Persistence of the North Atlantic Oscillation and its Biological Implication
title_fullStr Loss of Persistence of the North Atlantic Oscillation and its Biological Implication
title_full_unstemmed Loss of Persistence of the North Atlantic Oscillation and its Biological Implication
title_sort loss of persistence of the north atlantic oscillation and its biological implication
publisher Frontiers Media S.A.
publishDate 2014
url https://doi.org/10.3389/fevo.2014.00057
https://doaj.org/article/1295ce96d5a645088b90b22ee949521e
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
op_source Frontiers in Ecology and Evolution, Vol 2 (2014)
op_relation http://journal.frontiersin.org/Journal/10.3389/fevo.2014.00057/full
https://doaj.org/toc/2296-701X
2296-701X
doi:10.3389/fevo.2014.00057
https://doaj.org/article/1295ce96d5a645088b90b22ee949521e
op_doi https://doi.org/10.3389/fevo.2014.00057
container_title Frontiers in Ecology and Evolution
container_volume 2
_version_ 1766121233017995264