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...

Full description

Bibliographic Details
Main Authors: Lorenc Michał, Dondajewska Renata, Kaczmarek Lech
Format: Article
Language:English
Published: Sciendo 2013-09-01
Series:Limnological Review
Subjects:
Online Access:https://doi.org/10.2478/limre-2013-0016
id doaj-3d31f6711cf04dc2bfa0f2f44f81fb44
record_format Article
spelling 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
_version_ 1717772233596731392