Ice Growth and Platelet Crystals in Antarctica

• Main Author: Crook, Jonathan
• Format: Thesis
• Language: unknown
• Published: 2010
• Subjects: Pure Mathematics not elsewhere classified; Antarctica; Ice; Platelet; School: School of Mathematics; Statistics and Operations Research; 010199 Pure Mathematics not elsewhere classified; Marsden: 230107 Differential; Difference and Integral Equations; Marsden: 230113 Dynamical Systems; Marsden: 230120 Mathematics not Elsewhere Classified; Degree Discipline: Mathematics; Degree Level: Doctoral; Degree Name: Doctor of Philosophy; Arctic; Antarctic; The Antarctic; Marsden; Antarc*; Sea ice
• Online Access: https://doi.org/10.26686/wgtn.16984669.v1; https://figshare.com/articles/thesis/Ice_Growth_and_Platelet_Crystals_in_Antarctica/16984669

First-year land-fast sea ice growth in both the Arctic and the Antarctic is characterised by the formation of an initial ice cover, followed by the direct freezing of seawater at the ice-water interface. Such growth usually results, through geometric selection, in congelation ice. This is, in general, the typical crystal structure observed in first-year ice growth in the Arctic. However, in certain regions of the Antarctic, platelet crystals are observed to contribute significantly to the ice growth, beyond a depth of 1 m. This thesis will investigate a number of ideas as to why the platelet crystals only appear in the ice after a significant amount of congelation growth has occurred. One of the key premises will be that platelet ice forms when smaller frazil crystals, beneath the ice, rise up and attach to the interface. They are then incorporated into the ice cover and become the platelets seen in ice cores. The Shields criterion is used to find the strength of turbulence, associated with tidal flow, required to keep a frazil crystal from adhering to the interface. It is shown that the sub-ice flow is sufficient to keep most crystals in motion. However, this turbulence may weaken or dissipate completely as the tide turns. The velocity associated with brine rejection is suggested as an alternative to keep the crystals in suspension during these periods of low shear turbulence. Brine rejection occurs as the sea ice grows, rejecting salt into the seawater below. By comparing this velocity with a model for the frazil rise velocity it is shown that brine rejection has sufficient strength to keep crystals in suspension. This effect weakens as the ice gets thicker, allowing larger frazil crystals to rise to the interface. The early work in this thesis shows that a flow can keep a single crystal from adhering to the interface. This can be regarded as the competence of a flow to keep a crystal in suspension. However, of equal importance is the capacity of a flow to keep a mass of crystals in suspension. It is shown ...