Water temperatures and ice cover in lakes of the Tatra Mountains View Full Text


Ontology type: schema:ScholarlyArticle      Open Access: True


Article Info

DATE

2006-09

AUTHORS

Ferdinand Šporka, David M. Livingstone, Evžen Stuchlík, Jan Turek, Joanna Galas

ABSTRACT

In 2000 and 2001, miniature thermistors with integrated data loggers were employed to measure lake surface water temperatures (LSWTs) and temperature profiles in high-altitude mountain lakes lying between 1580 and 2145 m a.s.l. on both the Slovak and Polish sides of the Tatra Mountains. This allowed the annual cycle of water temperatures and ice cover in these lakes to be described quantitatively, and their dependence on lake altitude above sea level to be investigated. LSWTs in the Tatra Mountains are found to decrease approximately linearly with increasing altitude from late spring to autumn. LSWT in summer can be modelled well in terms of exponentially smoothed ambient air temperature. Although the timing of ice-off is dependent on altitude, the timing of ice-on is not; the dependence of the duration of ice cover on altitude is therefore wholly due to the altitudinal dependence of the timing of ice-off. The temperature profile measurements allow quantitative characterization of summer and winter stagnation, and spring and autumn turnover. More... »

PAGES

s77-s90

References to SciGraph publications

Identifiers

URI

http://scigraph.springernature.com/pub.10.2478/s11756-006-0121-x

DOI

http://dx.doi.org/10.2478/s11756-006-0121-x

DIMENSIONS

https://app.dimensions.ai/details/publication/pub.1035026112


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