Publikation: High-frequency internal waves in the littoral zone of a large lake
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2006
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Limnology and Oceanography. 2006, 51(4), pp. 1935-1939. eISSN 0024-3590. Available under: doi: 10.4319/lo.2006.51.4.1935
Zusammenfassung
Observations in the littoral zone of a large lake(Lake Constance) revealed strong and periodic fluctuations of temperature and current velocity on timescales between 10 and 15 min associated with high-frequency internal waves. The peak in the spectral energy of the current velocity fluctuations associated with high-frequency internal waves follows the seasonal dynamics of stratification, described by the stability frequency N. A comparison between the nearshore current velocity measurements in the littoral zone with temperature measurements in the pelagic of Lake Constance revealed a strong coupling between the occurrence of high-frequency internal waves in the littoral zone and the passage of the basin-scale internal Kelvin wave with a period of about 4 d.
Zusammenfassung in einer weiteren Sprache
Fachgebiet (DDC)
570 Biowissenschaften, Biologie
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high-frequency internal waves, littoral zone, large lake, Lake Constance, pelagic
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LORKE, Andreas, Frank PEETERS, Erich BÄUERLE, 2006. High-frequency internal waves in the littoral zone of a large lake. In: Limnology and Oceanography. 2006, 51(4), pp. 1935-1939. eISSN 0024-3590. Available under: doi: 10.4319/lo.2006.51.4.1935BibTex
@article{Lorke2006Highf-8013,
year={2006},
doi={10.4319/lo.2006.51.4.1935},
title={High-frequency internal waves in the littoral zone of a large lake},
number={4},
volume={51},
journal={Limnology and Oceanography},
pages={1935--1939},
author={Lorke, Andreas and Peeters, Frank and Bäuerle, Erich}
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<dcterms:abstract xml:lang="eng">Observations in the littoral zone of a large lake(Lake Constance) revealed strong and periodic fluctuations of temperature and current velocity on timescales between 10 and 15 min associated with high-frequency internal waves. The peak in the spectral energy of the current velocity fluctuations associated with high-frequency internal waves follows the seasonal dynamics of stratification, described by the stability frequency N. A comparison between the nearshore current velocity measurements in the littoral zone with temperature measurements in the pelagic of Lake Constance revealed a strong coupling between the occurrence of high-frequency internal waves in the littoral zone and the passage of the basin-scale internal Kelvin wave with a period of about 4 d.</dcterms:abstract>
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