Differences in the persistency of the North Atlantic Oscillation signal among lakes

Large‐scale climatic fluctuations, such as the El Niño Southern Oscillation and the North Atlantic Oscillation (NAO), are known to influence variability in abiotic site conditions and organism population dynamics in both terrestrial and aquatic ecosystems. Here we demonstrate that the influence of t...

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Published in:Limnology and Oceanography
Main Authors: Gerten, Dieter, Adrian, Rita
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2001
Subjects:
Online Access:http://dx.doi.org/10.4319/lo.2001.46.2.0448
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.4319%2Flo.2001.46.2.0448
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spelling crwiley:10.4319/lo.2001.46.2.0448 2024-06-23T07:55:01+00:00 Differences in the persistency of the North Atlantic Oscillation signal among lakes Gerten, Dieter Adrian, Rita 2001 http://dx.doi.org/10.4319/lo.2001.46.2.0448 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.4319%2Flo.2001.46.2.0448 https://aslopubs.onlinelibrary.wiley.com/doi/pdf/10.4319/lo.2001.46.2.0448 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Limnology and Oceanography volume 46, issue 2, page 448-455 ISSN 0024-3590 1939-5590 journal-article 2001 crwiley https://doi.org/10.4319/lo.2001.46.2.0448 2024-06-11T04:42:59Z Large‐scale climatic fluctuations, such as the El Niño Southern Oscillation and the North Atlantic Oscillation (NAO), are known to influence variability in abiotic site conditions and organism population dynamics in both terrestrial and aquatic ecosystems. Here we demonstrate that the influence of the NAO on lake water temperatures—one of the major factors controlling ecological processes in lakes—differs substantially among lake types of different thermal structures and mixing regimes, even under identical climatic forcing. A frequently circulating polymictic lake was found to be least influenced by the winter effects of the NAO, with an effect lasting only into early spring. In contrast, in a deep dimictic lake with stable summer stratification, the NAO signal persisted in the hypolimnion until the following winter. A shallow dimictic lake revealed an intermediate response, as weather conditions both in April and midsummer probably modified the strength and persistency of the NAO signal in the hypolimnion of that lake. Based on these results, it is to be expected that NAO effects on ecological processes vary significantly among lakes. Because the study period (1979–1998) includes a series of uncommonly warm winter and spring seasons, our findings also suggest that the influence of anticipated climate warming will vary substantially among lake types. Article in Journal/Newspaper North Atlantic North Atlantic oscillation Wiley Online Library Limnology and Oceanography 46 2 448 455
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description Large‐scale climatic fluctuations, such as the El Niño Southern Oscillation and the North Atlantic Oscillation (NAO), are known to influence variability in abiotic site conditions and organism population dynamics in both terrestrial and aquatic ecosystems. Here we demonstrate that the influence of the NAO on lake water temperatures—one of the major factors controlling ecological processes in lakes—differs substantially among lake types of different thermal structures and mixing regimes, even under identical climatic forcing. A frequently circulating polymictic lake was found to be least influenced by the winter effects of the NAO, with an effect lasting only into early spring. In contrast, in a deep dimictic lake with stable summer stratification, the NAO signal persisted in the hypolimnion until the following winter. A shallow dimictic lake revealed an intermediate response, as weather conditions both in April and midsummer probably modified the strength and persistency of the NAO signal in the hypolimnion of that lake. Based on these results, it is to be expected that NAO effects on ecological processes vary significantly among lakes. Because the study period (1979–1998) includes a series of uncommonly warm winter and spring seasons, our findings also suggest that the influence of anticipated climate warming will vary substantially among lake types.
format Article in Journal/Newspaper
author Gerten, Dieter
Adrian, Rita
spellingShingle Gerten, Dieter
Adrian, Rita
Differences in the persistency of the North Atlantic Oscillation signal among lakes
author_facet Gerten, Dieter
Adrian, Rita
author_sort Gerten, Dieter
title Differences in the persistency of the North Atlantic Oscillation signal among lakes
title_short Differences in the persistency of the North Atlantic Oscillation signal among lakes
title_full Differences in the persistency of the North Atlantic Oscillation signal among lakes
title_fullStr Differences in the persistency of the North Atlantic Oscillation signal among lakes
title_full_unstemmed Differences in the persistency of the North Atlantic Oscillation signal among lakes
title_sort differences in the persistency of the north atlantic oscillation signal among lakes
publisher Wiley
publishDate 2001
url http://dx.doi.org/10.4319/lo.2001.46.2.0448
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.4319%2Flo.2001.46.2.0448
https://aslopubs.onlinelibrary.wiley.com/doi/pdf/10.4319/lo.2001.46.2.0448
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
op_source Limnology and Oceanography
volume 46, issue 2, page 448-455
ISSN 0024-3590 1939-5590
op_rights http://onlinelibrary.wiley.com/termsAndConditions#vor
op_doi https://doi.org/10.4319/lo.2001.46.2.0448
container_title Limnology and Oceanography
container_volume 46
container_issue 2
container_start_page 448
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