Complex effects of winter warming on the physicochemical characteristics of a deep lake

Recent winter warming over Central Europe associated with a positive phase of the North Atlantic Oscillation (NAO) strongly influenced the thermal and water column stability properties of deep Lake Constance (zmean = 101 m).Volumet- rically weighted average water temperatures have increased since th...

Full description

Bibliographic Details
Published in:Limnology and Oceanography
Main Authors: Straile, Dietmar, Jöhnk, Klaus D., Rossknecht, Henno
Format: Article in Journal/Newspaper
Language:English
Published: 2003
Subjects:
Online Access:http://nbn-resolving.de/urn:nbn:de:bsz:352-opus-38387
https://doi.org/10.4319/lo.2003.48.4.1432
id ftubkonstanz:oai:kops.uni-konstanz.de:123456789/7872
record_format openpolar
spelling ftubkonstanz:oai:kops.uni-konstanz.de:123456789/7872 2024-02-11T10:06:17+01:00 Complex effects of winter warming on the physicochemical characteristics of a deep lake Straile, Dietmar Jöhnk, Klaus D. Rossknecht, Henno 2003 application/pdf http://nbn-resolving.de/urn:nbn:de:bsz:352-opus-38387 https://doi.org/10.4319/lo.2003.48.4.1432 eng eng http://nbn-resolving.de/urn:nbn:de:bsz:352-opus-38387 http://dx.doi.org/10.4319/lo.2003.48.4.1432 272995312 http://creativecommons.org/licenses/by-nc-nd/2.0/ Limnology and Oceanography. 2003, 48(4), pp. 1432-1438. eISSN 0024-3590. Available under: doi:10.4319/lo.2003.48.4.1432 North Atlantic Oscillation monomictic lake winter warming Lake Constance trophic changes eutrophication ddc:570 doc-type:article doc-type:Text 2003 ftubkonstanz https://doi.org/10.4319/lo.2003.48.4.1432 2024-01-21T23:52:11Z Recent winter warming over Central Europe associated with a positive phase of the North Atlantic Oscillation (NAO) strongly influenced the thermal and water column stability properties of deep Lake Constance (zmean = 101 m).Volumet- rically weighted average water temperatures have increased since the 1960s by an average of 0.017 degree C yr-1, and its interannual variability was strongly related to the variability in winter air temperature and the NAO winter index (NAOW). The influence of NAOw on water temperature was more persistent than its influence on air temperature. The seasonal persistence of the NAOw signal increased with water depth. Deep-water temperatures were related to the NAOw from one spring mixing period to the next. This caused a time lag of 1 yr in the response of deep-water winter temperatures to the NAOw. Reduced winter cooling during high-NAOw years resulted in the persistence of small temperature gradients that possibly resisted complete mixing. This, in turn, resulted in less upward mixing of nutrients (total phosphorus and total silica), which accumulated in the hypolimnion during the previous stratification period. A second effect of incomplete mixing was the lack of the replenishment of deepwater oxygen during high-NAOw years. Hence, besides its strong impact on the thermal regime, climate variability influenced both the causes (nutrient supply for phytoplankton growth) and symptoms (the degree of hypolimnetic oxygen deficiency) of trophic changes in Lake Constance. published published Article in Journal/Newspaper North Atlantic North Atlantic oscillation KOPS - The Institutional Repository of the University of Konstanz Limnology and Oceanography 48 4 1432 1438
institution Open Polar
collection KOPS - The Institutional Repository of the University of Konstanz
op_collection_id ftubkonstanz
language English
topic North Atlantic Oscillation
monomictic lake
winter warming
Lake Constance
trophic changes
eutrophication
ddc:570
spellingShingle North Atlantic Oscillation
monomictic lake
winter warming
Lake Constance
trophic changes
eutrophication
ddc:570
Straile, Dietmar
Jöhnk, Klaus D.
Rossknecht, Henno
Complex effects of winter warming on the physicochemical characteristics of a deep lake
topic_facet North Atlantic Oscillation
monomictic lake
winter warming
Lake Constance
trophic changes
eutrophication
ddc:570
description Recent winter warming over Central Europe associated with a positive phase of the North Atlantic Oscillation (NAO) strongly influenced the thermal and water column stability properties of deep Lake Constance (zmean = 101 m).Volumet- rically weighted average water temperatures have increased since the 1960s by an average of 0.017 degree C yr-1, and its interannual variability was strongly related to the variability in winter air temperature and the NAO winter index (NAOW). The influence of NAOw on water temperature was more persistent than its influence on air temperature. The seasonal persistence of the NAOw signal increased with water depth. Deep-water temperatures were related to the NAOw from one spring mixing period to the next. This caused a time lag of 1 yr in the response of deep-water winter temperatures to the NAOw. Reduced winter cooling during high-NAOw years resulted in the persistence of small temperature gradients that possibly resisted complete mixing. This, in turn, resulted in less upward mixing of nutrients (total phosphorus and total silica), which accumulated in the hypolimnion during the previous stratification period. A second effect of incomplete mixing was the lack of the replenishment of deepwater oxygen during high-NAOw years. Hence, besides its strong impact on the thermal regime, climate variability influenced both the causes (nutrient supply for phytoplankton growth) and symptoms (the degree of hypolimnetic oxygen deficiency) of trophic changes in Lake Constance. published published
format Article in Journal/Newspaper
author Straile, Dietmar
Jöhnk, Klaus D.
Rossknecht, Henno
author_facet Straile, Dietmar
Jöhnk, Klaus D.
Rossknecht, Henno
author_sort Straile, Dietmar
title Complex effects of winter warming on the physicochemical characteristics of a deep lake
title_short Complex effects of winter warming on the physicochemical characteristics of a deep lake
title_full Complex effects of winter warming on the physicochemical characteristics of a deep lake
title_fullStr Complex effects of winter warming on the physicochemical characteristics of a deep lake
title_full_unstemmed Complex effects of winter warming on the physicochemical characteristics of a deep lake
title_sort complex effects of winter warming on the physicochemical characteristics of a deep lake
publishDate 2003
url http://nbn-resolving.de/urn:nbn:de:bsz:352-opus-38387
https://doi.org/10.4319/lo.2003.48.4.1432
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
op_source Limnology and Oceanography. 2003, 48(4), pp. 1432-1438. eISSN 0024-3590. Available under: doi:10.4319/lo.2003.48.4.1432
op_relation http://nbn-resolving.de/urn:nbn:de:bsz:352-opus-38387
http://dx.doi.org/10.4319/lo.2003.48.4.1432
272995312
op_rights http://creativecommons.org/licenses/by-nc-nd/2.0/
op_doi https://doi.org/10.4319/lo.2003.48.4.1432
container_title Limnology and Oceanography
container_volume 48
container_issue 4
container_start_page 1432
op_container_end_page 1438
_version_ 1790603895686299648