Mixing and circulation of meltwater outflow plumes in polar fjords
This dissertation is concerned with the physical oceanography of meltwater plumes emerging at the base of glaciers at heads of fjords. First, a numerical model is developed and simulations to show the use of such a model are presented. Field work to verify the model was carried out, and the results...
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| Format: | Doctoral or Postdoctoral Thesis |
| Language: | English |
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University of Cambridge
1994
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| Online Access: | https://www.repository.cam.ac.uk/handle/1810/292648 https://doi.org/10.17863/CAM.39804 |
| Summary: | This dissertation is concerned with the physical oceanography of meltwater plumes emerging at the base of glaciers at heads of fjords. First, a numerical model is developed and simulations to show the use of such a model are presented. Field work to verify the model was carried out, and the results of these surveys are discussed in conjunction with other field data. Finally, laboratory experiments are presented, simulating the scenario of a plume of meltwater emerging at the surface of the fjord some distance from the glacier face. A brief summary of each of the three areas of research are given below. Circulation and mixing resulting from melt-driven convection in the proximity of ice have important oceanographic consequences, as well as being of interest to biologists studying organisms in these regions. A simple steady state, one-dimensional numerical model has been developed to simulate the characteristics of a cold, fresh meltwater plume emerging at the base of a vertical glacier face, at the head of a fjord. The importance of the initial width, speed and temperature of the outflow is shown. Simulations showing meltrates with depth are presented, and profiles of the retreat of the glacier face are given. Sensitivity of the model to varying the entrainment constant and the slope of the ice face are examined, as well as the sensitivity to other parameters of the model. Relevance to the Ice Pump Mechanism is made. Field work was undertaken in a fjord on the west coast of Spitsbergen, Svalbard to verify the results and characteristics of the meltwater plume of the numerical model developed. The data showed the fjord to agree well with previous work carried out in fjords with glaciers at their heads. Using a simple approach, the dynamic method, and from observations, it was conjectured that the Coriolis force has an effect on the circulation in the fjord. Data collected parallel to the glaciers in the fjord supported this conjecture. The field data used as comparisons comprised of a set from a fjord in the ... |
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