Abstract
A THERMOPROBE capable of measuring temperatures both 2.5 m into the sediment and in the water up to 3.3 m above the sediment has been designed, constructed and used to monitor the temperatures across the water-sediment interface at oceanic stations west of Oregon.
Similar content being viewed by others
References
Collins, C. A., Creech, H. C., and Pattullo, J. G., A Compilation of Observations from Moored Current Meters and Thermoprobes, Corvallis, Oregon, State University, Department of Oceanography (Data Report 23, Reference 66–11) (1966).
Lee, W. H. K., and Cox, C. S., J. Geophys. Res., 71, 2101 (1966).
US Coast and Geodetic Survey, tide tables: High and Low Water Predictions, West Coast of North and South America, including the Hawaiian Islands, Washington, DC (1966).
Author information
Authors and Affiliations
Rights and permissions
About this article
Cite this article
MESECAR, R., BODVARSSON, G. & BURT, W. Time-dependent Vertical Temperature Measurements across the Water-sediment Interface on the Continental Shelf West of Oregon. Nature 224, 901–902 (1969). https://doi.org/10.1038/224901a0
Received:
Revised:
Issue Date:
DOI: https://doi.org/10.1038/224901a0
- Springer Nature Limited
This article is cited by
-
An improved Ewing heat probe frame
Marine Geophysical Researches (1972)
-
Extending the versatility of the Bullard heat probe
Marine Geophysical Researches (1971)