Permafrost: Fourth International Conference, Proceedings, July 17-22, 1983 (1983)
Chapter: Heat and Salt Transport Processes in Thawing Subsea Permafrost at Prudhoe Bay Alaska
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Previous Chapter:
Ventifacts as Paleowind Indicators in a Former Periglacial Area of Southern Scandinavia
Next Chapter: Excavation Resistance of Frozen Soils Under Vibrating Cuttings
Suggested Citation:
"Heat and Salt Transport Processes in Thawing Subsea Permafrost at Prudhoe Bay Alaska." National Research Council. 1983. Permafrost: Fourth International Conference, Proceedings, July 17-22, 1983. Washington, DC: The National Academies Press.
doi: 10.17226/28727.
Suggested Citation:
"Heat and Salt Transport Processes in Thawing Subsea Permafrost at Prudhoe Bay Alaska." National Research Council. 1983. Permafrost: Fourth International Conference, Proceedings, July 17-22, 1983. Washington, DC: The National Academies Press.
doi: 10.17226/28727.
Suggested Citation:
"Heat and Salt Transport Processes in Thawing Subsea Permafrost at Prudhoe Bay Alaska." National Research Council. 1983. Permafrost: Fourth International Conference, Proceedings, July 17-22, 1983. Washington, DC: The National Academies Press.
doi: 10.17226/28727.
Suggested Citation:
"Heat and Salt Transport Processes in Thawing Subsea Permafrost at Prudhoe Bay Alaska." National Research Council. 1983. Permafrost: Fourth International Conference, Proceedings, July 17-22, 1983. Washington, DC: The National Academies Press.
doi: 10.17226/28727.
Suggested Citation:
"Heat and Salt Transport Processes in Thawing Subsea Permafrost at Prudhoe Bay Alaska." National Research Council. 1983. Permafrost: Fourth International Conference, Proceedings, July 17-22, 1983. Washington, DC: The National Academies Press.
doi: 10.17226/28727.
Suggested Citation:
"Heat and Salt Transport Processes in Thawing Subsea Permafrost at Prudhoe Bay Alaska." National Research Council. 1983. Permafrost: Fourth International Conference, Proceedings, July 17-22, 1983. Washington, DC: The National Academies Press.
doi: 10.17226/28727.
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