Climate-driven changes in spring plankton dynamics and the sensitivity of shallow polymictic lakes to the North Atlantic Oscillation

Climate is increasingly recognized as a major factor driving long-term changes in plankton communities in both marine and limnetic ecosystems. In a shallow and polymictic lake, marked changes in the dynamics of phytoplankton and in the timing of distinctive successional events in spring were observe...

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Main Authors: Dieter Gerten, Rita Adrian
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Published: 2000
Subjects:
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.499.9542
http://www.aslo.org/lo/toc/vol_45/issue_5/1058.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.499.9542 2023-05-15T17:31:21+02:00 Climate-driven changes in spring plankton dynamics and the sensitivity of shallow polymictic lakes to the North Atlantic Oscillation Dieter Gerten Rita Adrian The Pennsylvania State University CiteSeerX Archives 2000 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.499.9542 http://www.aslo.org/lo/toc/vol_45/issue_5/1058.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.499.9542 http://www.aslo.org/lo/toc/vol_45/issue_5/1058.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.aslo.org/lo/toc/vol_45/issue_5/1058.pdf text 2000 ftciteseerx 2016-01-08T08:59:34Z Climate is increasingly recognized as a major factor driving long-term changes in plankton communities in both marine and limnetic ecosystems. In a shallow and polymictic lake, marked changes in the dynamics of phytoplankton and in the timing of distinctive successional events in spring were observed during two recent decades. We studied whether and how these changes were linked to a series of uncommonly warm winter and spring seasons, focusing on the predictive power of a macroscale atmospheric circulation pattern, the North Atlantic Oscillation (NAO). In the warm period 1988–1998, phytoplankton developed about 1 month earlier than in the cool period 1979–1987, and high total phytoplankton biomass was recorded in early spring. These changes were significantly related to the NAO, which explained about 35 % of the variance, and can be attributed to a shortening or lack of ice cover periods in winter. Zooplankton (Keratella, Bosmina, Daphnia) developed about 2 weeks earlier in the warm period, con-sequently leading to an early establishment of the clearwater phase. The shift in the timing of the daphnid peak and of the clearwater phase required an additional warming trend in late April and early May and was not signif-icantly correlated with the winter situation. The memory effect of the NAO was restricted to a rather short postwinter period and was overtaken by the prevailing weather in April. Our results suggest that assessments of potential impacts of climate warming on biological processes in freshwater ecosystems demand basic knowledge about the Text North Atlantic North Atlantic oscillation Unknown
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description Climate is increasingly recognized as a major factor driving long-term changes in plankton communities in both marine and limnetic ecosystems. In a shallow and polymictic lake, marked changes in the dynamics of phytoplankton and in the timing of distinctive successional events in spring were observed during two recent decades. We studied whether and how these changes were linked to a series of uncommonly warm winter and spring seasons, focusing on the predictive power of a macroscale atmospheric circulation pattern, the North Atlantic Oscillation (NAO). In the warm period 1988–1998, phytoplankton developed about 1 month earlier than in the cool period 1979–1987, and high total phytoplankton biomass was recorded in early spring. These changes were significantly related to the NAO, which explained about 35 % of the variance, and can be attributed to a shortening or lack of ice cover periods in winter. Zooplankton (Keratella, Bosmina, Daphnia) developed about 2 weeks earlier in the warm period, con-sequently leading to an early establishment of the clearwater phase. The shift in the timing of the daphnid peak and of the clearwater phase required an additional warming trend in late April and early May and was not signif-icantly correlated with the winter situation. The memory effect of the NAO was restricted to a rather short postwinter period and was overtaken by the prevailing weather in April. Our results suggest that assessments of potential impacts of climate warming on biological processes in freshwater ecosystems demand basic knowledge about the
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author Dieter Gerten
Rita Adrian
spellingShingle Dieter Gerten
Rita Adrian
Climate-driven changes in spring plankton dynamics and the sensitivity of shallow polymictic lakes to the North Atlantic Oscillation
author_facet Dieter Gerten
Rita Adrian
author_sort Dieter Gerten
title Climate-driven changes in spring plankton dynamics and the sensitivity of shallow polymictic lakes to the North Atlantic Oscillation
title_short Climate-driven changes in spring plankton dynamics and the sensitivity of shallow polymictic lakes to the North Atlantic Oscillation
title_full Climate-driven changes in spring plankton dynamics and the sensitivity of shallow polymictic lakes to the North Atlantic Oscillation
title_fullStr Climate-driven changes in spring plankton dynamics and the sensitivity of shallow polymictic lakes to the North Atlantic Oscillation
title_full_unstemmed Climate-driven changes in spring plankton dynamics and the sensitivity of shallow polymictic lakes to the North Atlantic Oscillation
title_sort climate-driven changes in spring plankton dynamics and the sensitivity of shallow polymictic lakes to the north atlantic oscillation
publishDate 2000
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.499.9542
http://www.aslo.org/lo/toc/vol_45/issue_5/1058.pdf
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
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http://www.aslo.org/lo/toc/vol_45/issue_5/1058.pdf
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