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Georgiy Kirillin; Ilia Zverev; Arkady Terzhevik; Sergey Golosov; Cristof Engelhardt (2012)
Publisher: Taylor & Francis Group
Journal: Tellus: Series A
Languages: English
Types: Article
Subjects: anaerobic zone, thermal and mixing conditions, Meteorology. Climatology, QC851-999, atmospheric forcing, GC1-1581, oxygen depletion, Oceanography, DO deficit; oxygen depletion; anaerobic zone; thermal and mixing conditions; atmospheric forcing; climatic scenarios, DO deficit, climatic scenarios
Among the numerous processes that govern the functioning of a lake ecosystem, the regime of dissolved oxygen (DO) is of primary importance. The DO content is strongly affected by the temperature regime, mixing conditions and by the duration of the ice-covered period. These are formed due to atmospheric forcing and are, therefore, subject to variations in regional climate. Despite the large amount of data revealing the physical effect on the biological and chemical regimes in lakes, there is still insufficient understanding, both qualitative and quantitative, of how a lake ecosystem would be affected by changes in the lake temperature and mixing conditions due to changes in the atmospheric forcing. Below, the study of shallow lakes’ response to climatic changes using the coupled FLake-FLakeEco modelling system is presented. The results obtained reveal the extreme vulnerability of the lakes’ ecosystems to changes in atmospheric forcing. In ‘future’ climate the permanent existence of potentially dangerous anaerobic zones in shallow lakes is expected. The projected decreased oxygen concentrations are caused by: (1) the reduced oxygen flux from the atmosphere to the lakes due to increased temperature; and (2) strengthened density stratification of the water columns which would prevent aeration of the near-bottom layers.Keywords: DO deficit; oxygen depletion; anaerobic zone; thermal and mixing conditions; atmospheric forcing; climatic scenarios(Published: 21 February 2012)Citation: Tellus A 2012, 64, 17264, DOI: 10.3402/tellusa.v64i0.17264
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    • Anneville, O., Ginot, V., Druart, J.-C. and Angeli, N. 2003. Longterm study (1974 1998) of seasonal changes in the phytoplankton in Lake Geneva: a multi-table approach. J. Plankton Res. 24, 993 1008.
    • Anneville, O., Souissi, S., Gammeter, S. and Straile, D. 2004. Seasonal and inter-annual scales of variability in phytoplankton assemblages: comparison of phytoplankton dynamics in three peri-alpine lakes over a period of 28 years. Freshwat. Biol. 49(1), 98 115.
    • Balsamo, G., Dutra, E., Stepanenko, V. M., Viterbo, P., Miranda, P. M. A. and co-authors. 2010. Deriving an effective lake depth from satellite lake surface temperature data: a feasibility study with MODIS data. Boreal Env. Res. 15, 178 190.
    • Barica, J. and Mathias, J. A. 1979. Oxygen depletion and winterkill risk in small prairie lakes under extended ice cover. J. Fish. Res. Board Can. 36, 980 986.
    • Carvalho, L. and Kirika, A. 2003. Changes in shallow lake functioning: response to climate change and nutrient reduction. Hydrobiologia 506(1), 789 796.
    • George, D. and Hurley, M. 2004. The influence of sampling frequency on the detection of long-term change in three lakes in the English Lake District. Aquat. Ecosyst. Health Manage. 7(1), 1 14.
    • Gerten, D. and Adrian, R. 2001. Differences in the persistency of the North Atlantic Osicllation signal among lakes. Limnol. Oceanogr. 46(2), 448 455.
    • Golosov, S. and Ignatieva, N. 1999. Hydrothermodynamic features of mass exchange across the sediment water interface in shallow lakes. Hydrobiologia 408/409, 153 157.
    • Golosov, S., Maher, O., Schipunova, E., Terzhevik, A., Zdorovennova, G. and co-authors. 2007. Physical background of the development of oxygen depletion in ice-covered lakes. Oecologia 151(2), 331 340.
    • Greenbank, J. 1945. Limnological conditions in ice-covered lakes, especially as related to winter-kill of fish. Ecol. Monogr. 15(4), 343 392.
    • Hargeby, A., Blindow, I. and Hansson, L.-A. 2004. Shifts between clear and turbid states in a shallow lake: multi-causal stress from climate, nutrients and biotic interactions. Arch. Hydrobiol. 161(4), 433 454.
    • Ha˚ kanson, L. 2004. Break-through in predictive modelling opens new possibilities for aquatic eoclogy and management a review. Hydrobiologia 518(1 3), 135 157.
    • Hargrave, B. 1972. A comparison of sediment oxygen uptake, hypolimnetic oxygen deficit and primary production in Lake Esrom, Denmark. Vehr. Int. Ver. Limnol. 18, 134 139.
    • Hutchinson, G. E. 1957. A Treatise on Limnology Vol. I. J. Wiley and Son, Inc., NY, 1015 p.
    • Jacob, D. and Gerstengarbe, F.-W. 2005. Klimaszenarien fu¨ r den deutschen Teil des Elbe-Einzugsgebietes. In: Integrierte Analyse der Auswirkungen des globalen Wandels auf Wasser, Umwelt und Gesellschaft im Elbegebiet (eds F. Wechsung, A. Becker, and P. Gra¨ fe). Berlin, Weissensee, 85 118.
    • Kirillin, G. 2010. Modelling the impact of global warming on water temperature and seasonal mixing regimes in small temperate lakes. Boreal Environ. Res. 15, 279 293.
    • Kondratiev, S., Golosov, S., Kreiman, K. and Ignatieva, N. 1998. Modelling hydrological processes and mass transfer in a watershed-lake system. Water Resources (Vodnye Resursy) 25, 571 580.
    • Liss, P. and Slinn, G. 1983. Air sea exchange of gases and particles. In: Proceeding of the NATO Advanced Study Institute on Air Sea Exchange on Gases and Particles, University of New Hampshire, USA, 19 30 July 1982. Reidel Publishing Company, Dordrecht, Holland, pp. 241 289.
    • Mironov, D. 2010. Implementation of the lake parameterization scheme FLake into the numerical weather prediction model COSMO. Boreal Environ. Res. 15, 218 230.
    • Naki c´enovic´ , N. and Swart, R. (eds.) 2000. Special Report on Emissions Scenarios. A Special Report of Working Group III of the Intergovernmental Panel on Climate Change. Cambridge University Press, Cambridge and NY.
    • Odum, E. and Barret, G. 2004. Fundamentals of Ecology. 5th ed. Brooks Cole, Florence, KY, 624 p.
    • Ra¨ is a¨nen, J., Hansson, U., Ullerstig, A., Do¨ scher, R., Graham, L. P. and co-authors. 2004. European climate in the late twentyfirst century: regional simulations with two driving global models and two forcing scenarios. Climate Dynamics 22, 13 31.
    • Roeckner, E., Bengtsson, L., Feichter, J., Lelieveld, J. and Rodhe, H. 1999. Transient climate change simulations with a coupled atmosphere-ocean GCM including the tropospheric sulfur cycle. J. Climate 12, 3004 3032.
    • Salmaso, N. 2005. Effect of climatic fluctuations and vertical mixing on inter-annual trophic variability of Lake Garda, Italy. Limnol. Oceanogr. 50(2), 553 565.
    • Scheffer, M., Straile, D., van Nes, E. and Hosper, H. 2003. Climatic effetc on regime shifts in lakes. Limnol. Oceanogr. 48(3), 1353 1356.
    • Seki, H. 1982. Organic Materials in Aquatic Ecosystems. CRC Press Inc., Boca Raton, FL, 201 p.
    • Szabo´ , C. 2007. Hydrogen sulphide and its therapeutic potential. Nat. Rev. 6, 918 935.
    • Vesely, J., Majer, V., Kopachek, J. and Norton, S. 2003. Increasing temperature decreases aluminium concentrations in Central European lakes recovering from acidification. Limnol. Oceanogr. 48(6), 2346 2354.
    • Watson, R. T. 2001. Climate Change 2001: Synthesis Report. A Contribution of Working Groups I, II and III to the Third Assessment Report of the Intergovernmental Panel on Climate Change. Cambridge University Press, Cambridge.
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