Water and sediment temperature dynamics in shallow tidal environments: The role of the heat flux at the sediment-water interface

Published

Journal Article

© 2018 Elsevier Ltd In the present study, we investigate the energy flux at the sediment-water interface and the relevance of the heat exchanged between water and sediment for the water temperature dynamics in shallow coastal environments. Water and sediment temperature data collected in the Venice lagoon show that, in shallow, temperate lagoons, temperature is uniform within the water column, and enabled us to estimate the net heat flux at the sediment-water interface. We modeled this flux as the sum of a conductive component and of the solar radiation reaching the bottom, finding the latter being negligible. We developed a “point” model to describe the temperature dynamics of the sediment-water continuum driven by vertical energy transfer. We applied the model considering conditions characterized by negligible advection, obtaining satisfactory results. We found that the heat exchange between water and sediment is crucial for describing sediment temperature but plays a minor role on the water temperature.

Full Text

Duke Authors

Cited Authors

  • Pivato, M; Carniello, L; Gardner, J; Silvestri, S; Marani, M

Published Date

  • March 1, 2018

Published In

Volume / Issue

  • 113 /

Start / End Page

  • 126 - 140

International Standard Serial Number (ISSN)

  • 0309-1708

Digital Object Identifier (DOI)

  • 10.1016/j.advwatres.2018.01.009

Citation Source

  • Scopus