Wpływ Oscylacji Północnoatlantyckiej na zmiany stabilności reżimu stanów wody jezior w Polsce

The paper presents results of research on the stability of water stage regime of Polish lakes in different phases of the North Atlantic Oscillation. The stability of the regime was defined as the degree of regularity of occurrence of a particular phase of the hydrological regime, i.e. high and low w...

Full description

Bibliographic Details
Main Authors: Plewa, Katarzyna, Wrzesiński, Dariusz
Format: Article in Journal/Newspaper
Language:Polish
Published: Wydawnictwo Poznańskiego Towarzystwa Przyjaciół Nauk 2017
Subjects:
Online Access:http://hdl.handle.net/10593/23655
https://doi.org/10.14746/bfg.2017.8.9
id ftmickiewiczuni:oai:repozytorium.amu.edu.pl:10593/23655
record_format openpolar
spelling ftmickiewiczuni:oai:repozytorium.amu.edu.pl:10593/23655 2023-07-30T04:05:13+02:00 Wpływ Oscylacji Północnoatlantyckiej na zmiany stabilności reżimu stanów wody jezior w Polsce Plewa, Katarzyna Wrzesiński, Dariusz 2017 application/pdf http://hdl.handle.net/10593/23655 https://doi.org/10.14746/bfg.2017.8.9 pol pol Wydawnictwo Poznańskiego Towarzystwa Przyjaciół Nauk Seria A - Geografia Fizyczna Tom 68; Badania Fizjograficzne, Seria A, Tom 68, 2017, s. 127-138 doi:10.14746/bfg.2017.8.9 2081-6014 http://hdl.handle.net/10593/23655 info:eu-repo/semantics/openAccess lakes water level regime stability coefficient North Atlantic Oscillation Artykuł 2017 ftmickiewiczuni https://doi.org/10.14746/bfg.2017.8.9 2023-07-17T18:29:13Z The paper presents results of research on the stability of water stage regime of Polish lakes in different phases of the North Atlantic Oscillation. The stability of the regime was defined as the degree of regularity of occurrence of a particular phase of the hydrological regime, i.e. high and low water stages. The determination of the stability of water stage regime in lakes applied the stability coefficient. The analysis covered data concerning mean monthly values of water stages from 1976–2010 for 34 lakes located in Polish lakelands. According to the study, the effect of changes in the North Atlantic Oscillation on water stages in lakes is variable in time and space. In the positive NAO phase, maximums on lakes occur earlier than on average – in winter and spring, and in the negative phase - later. Minimums change in a lower range, particularly in the positive NAO phase. In the negative phase, on the majority of lakes, the term of appearance of Imin was later than on average. The term of occurrence of minimums is considerably variable, particularly in the positive phase, and in the negative phase it is usually later, and occurs in autumn. Article in Journal/Newspaper North Atlantic North Atlantic oscillation AMUR - Adam Mickiewicz University Repository, Poznan
institution Open Polar
collection AMUR - Adam Mickiewicz University Repository, Poznan
op_collection_id ftmickiewiczuni
language Polish
topic lakes
water level regime
stability coefficient
North Atlantic Oscillation
spellingShingle lakes
water level regime
stability coefficient
North Atlantic Oscillation
Plewa, Katarzyna
Wrzesiński, Dariusz
Wpływ Oscylacji Północnoatlantyckiej na zmiany stabilności reżimu stanów wody jezior w Polsce
topic_facet lakes
water level regime
stability coefficient
North Atlantic Oscillation
description The paper presents results of research on the stability of water stage regime of Polish lakes in different phases of the North Atlantic Oscillation. The stability of the regime was defined as the degree of regularity of occurrence of a particular phase of the hydrological regime, i.e. high and low water stages. The determination of the stability of water stage regime in lakes applied the stability coefficient. The analysis covered data concerning mean monthly values of water stages from 1976–2010 for 34 lakes located in Polish lakelands. According to the study, the effect of changes in the North Atlantic Oscillation on water stages in lakes is variable in time and space. In the positive NAO phase, maximums on lakes occur earlier than on average – in winter and spring, and in the negative phase - later. Minimums change in a lower range, particularly in the positive NAO phase. In the negative phase, on the majority of lakes, the term of appearance of Imin was later than on average. The term of occurrence of minimums is considerably variable, particularly in the positive phase, and in the negative phase it is usually later, and occurs in autumn.
format Article in Journal/Newspaper
author Plewa, Katarzyna
Wrzesiński, Dariusz
author_facet Plewa, Katarzyna
Wrzesiński, Dariusz
author_sort Plewa, Katarzyna
title Wpływ Oscylacji Północnoatlantyckiej na zmiany stabilności reżimu stanów wody jezior w Polsce
title_short Wpływ Oscylacji Północnoatlantyckiej na zmiany stabilności reżimu stanów wody jezior w Polsce
title_full Wpływ Oscylacji Północnoatlantyckiej na zmiany stabilności reżimu stanów wody jezior w Polsce
title_fullStr Wpływ Oscylacji Północnoatlantyckiej na zmiany stabilności reżimu stanów wody jezior w Polsce
title_full_unstemmed Wpływ Oscylacji Północnoatlantyckiej na zmiany stabilności reżimu stanów wody jezior w Polsce
title_sort wpływ oscylacji północnoatlantyckiej na zmiany stabilności reżimu stanów wody jezior w polsce
publisher Wydawnictwo Poznańskiego Towarzystwa Przyjaciół Nauk
publishDate 2017
url http://hdl.handle.net/10593/23655
https://doi.org/10.14746/bfg.2017.8.9
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
op_relation Seria A - Geografia Fizyczna Tom 68;
Badania Fizjograficzne, Seria A, Tom 68, 2017, s. 127-138
doi:10.14746/bfg.2017.8.9
2081-6014
http://hdl.handle.net/10593/23655
op_rights info:eu-repo/semantics/openAccess
op_doi https://doi.org/10.14746/bfg.2017.8.9
_version_ 1772817002536108032