Description
In situ sediment temperatures measured during cruise PS134 on the Bellingshausen Sea Shelf. Five Miniaturized Temperature Data-Loggers (MTL) were mounted on a 5 m lance for measuring sediment temperatures. One MTL was mounted on the weight head (Sensor 0) and reports here the bottom water temperature.
Depth, sediment/rock [m] = penetration depth with seafloor at 0 m and negative depths as meters above seafloorDepth, relative [m] = Sensor depth relative to the top of the heat flow probe/beginning of the weight head
Depth, sediment/rock [m] = penetration depth with seafloor at 0 m and negative depths as meters above seafloorDepth, relative [m] = Sensor depth relative to the top of the heat flow probe/beginning of the weight head
| Date made available | 2025 |
|---|---|
| Publisher | PANGAEA |
| Geospatial polygon | 73.52065,-92.69322999999997, 73.52065,-72.67754000000002, -73.63678,-72.67754000000002, -73.63678,-92.69322999999997, 73.52065,-92.69322999999997 |
Research output
- 1 Article
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Influence of Transient Bottom Water Temperature Variations on Geothermal Heat Flow Measurements From the Bellingshausen Sea, West Antarctica, and the Baltic Sea
Brand, C., Kaul, N., Lösing, M. & Gohl, K., Aug 2025, In: Journal of Geophysical Research: Oceans. 130, 8, e2024JC022034.Research output: Contribution to journal › Article › peer-review
Open Access
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