http://www.cnr.it/ontology/cnr/individuo/prodotto/ID71732
Trends in the water chemistry of high altitude lakes in Europe (Articolo in rivista)
- Type
- Label
- Trends in the water chemistry of high altitude lakes in Europe (Articolo in rivista) (literal)
- Anno
- 2002-01-01T00:00:00+01:00 (literal)
- Alternative label
Mosello R., Lami A., Marchetto A., Rogora M., Wathne B., Lien L., Catalan J., Camarero L., Ventura M., Psenner R., Koinig K., Thies H., Sommaruga-Wograth S., Nickus U., Tait D., Thaler B., Barbieri A., Harriman R. (2002)
Trends in the water chemistry of high altitude lakes in Europe
in Water, air, & soil pollution. Focus
(literal)
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- Mosello R., Lami A., Marchetto A., Rogora M., Wathne B., Lien L., Catalan J., Camarero L., Ventura M., Psenner R., Koinig K., Thies H., Sommaruga-Wograth S., Nickus U., Tait D., Thaler B., Barbieri A., Harriman R. (literal)
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- CNR Istituto Italiano di Idrobiologia, Verbania Pallanza, Italy; 2 Norwegian Institute for Water
Research, Kjelsas, Oslo, Norway; 3 University of Barcelona, Dept. Ecology, Barcelona, Spain;
4 University of Innsbruck, Inst. Zoology and Limnology, Innsbruck, Austria; 5 University of
Innsbruck, Inst. Meteorology, Innsbruck, Austria; 6 Laboratorio Biologico - APPA, Laives (BZ),
Italy; 7 Laboratorio Studi Ambientali, Sez. Protezione Aria Acqua, Dip. Territorio Ambiente,
Lugano, Switzerland; 8 Freshwater Fisheries Laboratory, Pitlochry, Perthshire, Scotland, U.K. (literal)
- Titolo
- Trends in the water chemistry of high altitude lakes in Europe (literal)
- Abstract
- Here we present the chemical trends of seven high altitude lakes, analysed within the
AL:PE and MOLAR Projects of the EU (1999) and selected on the basis of the availability of
complete and reliable data for the period 1984-1999. The lakes are representative of the Scandinavian
Alps, the Cairngorm Mountains in Scotland, the Alps and the Pyrenees. Significant trends
were identified for some indicators of acidification, for instance pH and alkalinity, but not all lakes
reacted similarly to decreasing depositions of sulphate and base cations. Differences in lake response
are discussed in relation to recent variations of atmospheric deposition chemistry and associated
changes in climatic conditions. Beside individual variations of the studied lakes, depending, among
other things, on altitude and morphology, catchment characteristics and climate trends play a major
role for the reaction of high altitude lakes on changes in atmospheric depositions. (literal)
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