Water level fluctuations in selected Wielkopolski National Park lakes in 2012 against changes noted in 2007-2008
The results presented in this paper of water level fluctuations in selected lakes of Wielkopolski National Park have a preliminary character, contributing new information to the knowledge on this area. Five lakes situated in three distinct tunnel valleys were selected for research: Jarosławieckie, G...
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Series: | Limnological Review |
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Online Access: | https://doi.org/10.2478/limre-2013-0016 |
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doaj-3d31f6711cf04dc2bfa0f2f44f81fb442021-09-06T19:22:23ZengSciendoLimnological Review2300-75752013-09-0113314715310.2478/limre-2013-0016Water level fluctuations in selected Wielkopolski National Park lakes in 2012 against changes noted in 2007-2008Lorenc Michał0Dondajewska Renata1Kaczmarek Lech2Adam Mickiewicz University, Jeziory Ecological Station, PO Box 40, 62-050 Mosina, Poznań, PolandAdam Mickiewicz University, Faculty of Biology, Department of Water Protection, Umultowska 89, 61-614 Poznań, PolandAdam Mickiewicz University, Jeziory Ecological Station, PO Box 40, 62-050 Mosina, Poznań, PolandThe results presented in this paper of water level fluctuations in selected lakes of Wielkopolski National Park have a preliminary character, contributing new information to the knowledge on this area. Five lakes situated in three distinct tunnel valleys were selected for research: Jarosławieckie, Góreckie, Budzyńskie, Witobelskie and Łódzko-Dymaczewskie. The water level was measured from December 2006 till January 2008 and from January till December of 2012 with ca. monthly frequency. An increase in the water stage was noted in the autumn-winter period, which was rather unusual. The comparison of years 2007 and 2012 indicated higher water levels in the latter. The amplitude of the water level was higher in flow-through lakes due to the reaction to precipitation in early spring as well as different catchment features. Specific water level fluctuations in Lake Góreckie are probably related to the influence of groundwater of the Wielkopolska fossil valley.https://doi.org/10.2478/limre-2013-0016lakeswater level fluctuationswielkopolski national park |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Lorenc Michał Dondajewska Renata Kaczmarek Lech |
spellingShingle |
Lorenc Michał Dondajewska Renata Kaczmarek Lech Water level fluctuations in selected Wielkopolski National Park lakes in 2012 against changes noted in 2007-2008 Limnological Review lakes water level fluctuations wielkopolski national park |
author_facet |
Lorenc Michał Dondajewska Renata Kaczmarek Lech |
author_sort |
Lorenc Michał |
title |
Water level fluctuations in selected Wielkopolski National Park lakes in 2012 against changes noted in 2007-2008 |
title_short |
Water level fluctuations in selected Wielkopolski National Park lakes in 2012 against changes noted in 2007-2008 |
title_full |
Water level fluctuations in selected Wielkopolski National Park lakes in 2012 against changes noted in 2007-2008 |
title_fullStr |
Water level fluctuations in selected Wielkopolski National Park lakes in 2012 against changes noted in 2007-2008 |
title_full_unstemmed |
Water level fluctuations in selected Wielkopolski National Park lakes in 2012 against changes noted in 2007-2008 |
title_sort |
water level fluctuations in selected wielkopolski national park lakes in 2012 against changes noted in 2007-2008 |
publisher |
Sciendo |
series |
Limnological Review |
issn |
2300-7575 |
publishDate |
2013-09-01 |
description |
The results presented in this paper of water level fluctuations in selected lakes of Wielkopolski National Park have a preliminary character, contributing new information to the knowledge on this area. Five lakes situated in three distinct tunnel valleys were selected for research: Jarosławieckie, Góreckie, Budzyńskie, Witobelskie and Łódzko-Dymaczewskie. The water level was measured from December 2006 till January 2008 and from January till December of 2012 with ca. monthly frequency. An increase in the water stage was noted in the autumn-winter period, which was rather unusual. The comparison of years 2007 and 2012 indicated higher water levels in the latter. The amplitude of the water level was higher in flow-through lakes due to the reaction to precipitation in early spring as well as different catchment features. Specific water level fluctuations in Lake Góreckie are probably related to the influence of groundwater of the Wielkopolska fossil valley. |
topic |
lakes water level fluctuations wielkopolski national park |
url |
https://doi.org/10.2478/limre-2013-0016 |
work_keys_str_mv |
AT lorencmichał waterlevelfluctuationsinselectedwielkopolskinationalparklakesin2012againstchangesnotedin20072008 AT dondajewskarenata waterlevelfluctuationsinselectedwielkopolskinationalparklakesin2012againstchangesnotedin20072008 AT kaczmareklech waterlevelfluctuationsinselectedwielkopolskinationalparklakesin2012againstchangesnotedin20072008 |
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