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Temperature changes in the tidal excursion front and surface sediment of a subtropical mudflat in autumn

Identifieur interne : 000811 ( Main/Exploration ); précédent : 000810; suivant : 000812

Temperature changes in the tidal excursion front and surface sediment of a subtropical mudflat in autumn

Auteurs : Mekiel J. Birt [Australie] ; Ian R. Tibbetts [Australie]

Source :

RBID : Pascal:07-0412192

Descripteurs français

English descriptors

Abstract

Temperature changes in sediment and the inundating water of a subtropical mudflat were determined using a series of data-loggers to monitor the temperature on fine days around the equinox at Lota, Queensland, Australia. On fine days the temperature of the forward shallow (ca. 5 cm) section of an incoming tide is up to 8 °C higher than that of the body of water from which it originates. Stationary data-loggers in the sediment indicate that during the day heat exchange occurred between the sediment and inundating waters, the sediment temperatures dropping from up to 10 °C higher than channel waters to temperatures approaching that of channel water in as little as 30 min following inundation. The implications for intertidal nekton and benthos are discussed.


Affiliations:


Links toward previous steps (curation, corpus...)


Le document en format XML

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<term>Tides</term>
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<term>Température superficielle</term>
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<div type="abstract" xml:lang="en">Temperature changes in sediment and the inundating water of a subtropical mudflat were determined using a series of data-loggers to monitor the temperature on fine days around the equinox at Lota, Queensland, Australia. On fine days the temperature of the forward shallow (ca. 5 cm) section of an incoming tide is up to 8 °C higher than that of the body of water from which it originates. Stationary data-loggers in the sediment indicate that during the day heat exchange occurred between the sediment and inundating waters, the sediment temperatures dropping from up to 10 °C higher than channel waters to temperatures approaching that of channel water in as little as 30 min following inundation. The implications for intertidal nekton and benthos are discussed.</div>
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   |texte=   Temperature changes in the tidal excursion front and surface sediment of a subtropical mudflat in autumn
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