Publikation: Using transient conservative and environmental tracers to study water exchange in Lake Issyk-Kul
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Mixing and transport processes are of major importance for the ecology of lakes [1]. In particular, deep-water renewal determines to a large extent the distribution of nutrients and dissolved oxygen in deep lakes such as Lake Issyk-Kul (Kyrgyzstan). The characterization and quantification of deep-water exchange is therefore essential for the understanding of the functioning of such lake ecosystems. Rates of vertical water exchange can be estimated from concentrations of transient tracers, whereas the processes responsible for transport can be identified by environmental tracers such as temperature, salinity, dissolved oxygen and light transmissivity. In the following we first describe the use of transient and other environmental tracers for water age determination and for the characterization of water exchange processes. Then we discuss the application of these methods to Lake Issyk-Kul and present first tentative results on the mechanism of deep-water exchange based on data from two expeditions, one conducted in September 1996 and one in March 2001.
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KIPFER, Rolf, Frank PEETERS, 2002. Using transient conservative and environmental tracers to study water exchange in Lake Issyk-Kul. In: KLERKX, Jean, ed. and others. Lake Issyk-Kul. Kluwer, 2002, pp. 89-100. Available under: doi: 10.1007/978-94-010-0491-6_8BibTex
@incollection{Kipfer2002Using-7729, year={2002}, doi={10.1007/978-94-010-0491-6_8}, title={Using transient conservative and environmental tracers to study water exchange in Lake Issyk-Kul}, publisher={Kluwer}, booktitle={Lake Issyk-Kul}, pages={89--100}, editor={Klerkx, Jean}, author={Kipfer, Rolf and Peeters, Frank} }
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