Thermal-oxygen conditions in Lakes Ros and Rospuda Filipowska (North-Eastern Poland) in the summer half-year 2005-2014

• Autorzy: Ptak M. , Nowak B.

Warianty tytułu

PL

Warunki termiczno-tlenowe jeziora Roś i Rospuda Filipowska (północno-wschodnia Polska) w półroczu letnim 2005-2014

• Języki publikacji: EN

Abstrakty

EN

Thermal and oxygen conditions of lake ecosystems are important for their functioning. The availability of detailed information is of particular importance in the context of the observed environmental changes. The paper presents thermal-oxygen conditions in Lakes Roś and Rospuda Filipowska in north-eastern Poland in the years 2005–2014 for the summer half-year (May – October). Both of the lakes are classified as stratified lakes. The mean water temperature throughout the water column in Lake Roś was 11.3oC, and in Lake Rospuda 9.4oC. The temperature distribution was evidently affected by wind. In the case of Lake Roś with better conditions for water mixing due to the orientation of the lake’s axis in relation to the direction of dominant winds, the epilimnion covered approximately 25% of the water column (in July), whereas in the case of Lake Rospuda (with axis notaligned with the direction of dominant winds), the zone covered approximately 18%. In both of the lakes, a correlation was recorded between oxygen dissolved in water and water temperature. It was more evident in the case of Lake Roś, where the oxygen curve in all months was similar to that of temperature. In Lake Rospuda, no such situation was recorded for May and June. No statistically significant changes in both of the parameters were recorded in the analysed multiannual

PL

Istotne dla funkcjonowania ekosystemów jeziornych są warunki termiczne i tlenowe w nich panujące. Posiadanie szczegółowych informacji na ten temat jest ważne w kontekście obserwowanych zmian środowiska. W pracy przeanalizowano warunki termiczno-tlenowe jeziora Roś i Rospuda Filipowska w północno-wschodniej Polsce w latach 2005–2014 dla półrocza letniego (maj– październik). Oba jeziora należą do stratyfikowanych. Średnia temperatura wody całego pionu jeziora Roś wyniosła 11,3oC, a jeziora Rospuda 9,4oC. Na rozkład temperatury widoczny był wpływ wiatru. W przypadku jeziora Roś, w którym występują lepsze warunki do mieszania wody z uwagi na orientację osi jeziora w stosunku do kierunku dominujących wiatrów, epilimnion obejmował ok. 25%(w lipcu), podczas gdy w przypadku jeziora Rospuda (niezorientowanego osią do kierunku przeważających wiatrów) strefa ta wyniosła ok. 18%. W obu jeziorach odnotowano związek rozkładu tlenu rozpuszczonego w wodzie z jej temperaturą. Był on bardziej wyraźny w przypadku jeziora Roś,gdzie krzywa tlenowa była we wszystkich miesiącach współkształtna z krzywą temperatury. W Rospudzie takiej sytuacji nie odnotowano dla maja i czerwca. W analizowanym wieloleciu nie wykryto istotnych statystycznie zmian obu parametrów

• Wydawca: -
• Czasopismo: Polish Journal of Natural Sciences
• Rocznik: 2017
• Tom: 32
• Numer: 2
• Opis fizyczny: p.343-355,fig.,ref.

Twórcy

autor

Ptak M.

• Institute of Physical Geography and Environmental Planning, Adam Mickiewicz University in Poznan, B.Krygowskiego 10, 61-680 Poznan, Poland

autor

Nowak B.

• Institute of Meteorology and Water Management - National Research Institute in Warsaw, Warsaw, Poland

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