Temperature changes in the tidal excursion front and surface sediment of a subtropical mudflat in autumn
Identifieur interne : 000811 ( Main/Exploration ); précédent : 000810; suivant : 000812Temperature 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 :
- Journal of sea research : (Den Burg) [ 1385-1101 ] ; 2007.
Descripteurs français
- Pascal (Inist)
- Wicri :
- topic : Milieu marin.
English descriptors
- KwdEn :
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...)
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Le document en format XML
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<author><name sortKey="Birt, Mekiel J" sort="Birt, Mekiel J" uniqKey="Birt M" first="Mekiel J." last="Birt">Mekiel J. Birt</name>
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<sourceDesc><biblStruct><analytic><title xml:lang="en" level="a">Temperature changes in the tidal excursion front and surface sediment of a subtropical mudflat in autumn</title>
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<term>Mud flats</term>
<term>Sediments</term>
<term>Surface temperature</term>
<term>Tides</term>
</keywords>
<keywords scheme="Pascal" xml:lang="fr"><term>Température superficielle</term>
<term>Marée</term>
<term>Sédiment</term>
<term>Vasière</term>
<term>Milieu marin</term>
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<keywords scheme="Wicri" type="topic" xml:lang="fr"><term>Milieu marin</term>
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<front><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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