The temperature change shortcut: effects of mid-experiment temperature changes on the deformation of polycrystalline ice

• Published in: The Cryosphere
• Main Authors: L. Craw, A. Treverrow, S. Fan, M. Peternell, S. Cook, F. McCormack, J. Roberts
• Format: Article in Journal/Newspaper
• Language: English
• Published: Copernicus Publications 2021
• Subjects: Environmental sciences; GE1-350; Geology; QE1-996.5; Ice Shelves; The Cryosphere
• Online Access: https://doi.org/10.5194/tc-15-2235-2021; https://doaj.org/article/6045c4a9c9524f8f903727c553847f4c

It is vital to understand the mechanical properties of flowing ice to model the dynamics of ice sheets and ice shelves and to predict their behaviour in the future. We can increase our understanding of ice physical properties by performing deformation experiments on ice in laboratories and examining its mechanical and microstructural responses. However, natural conditions in ice sheets and ice shelves extend to low temperatures ( <math xmlns="http://www.w3.org/1998/Math/MathML" id="M1" display="inline" overflow="scroll" dspmath="mathml"><mrow><mo>≪</mo><mo>-</mo><mn mathvariant="normal">10</mn></mrow></math> <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="36pt" height="10pt" class="svg-formula" dspmath="mathimg" md5hash="1be5049de7f8a69fcd20dac38a5ac4c9"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="tc-15-2235-2021-ie00001.svg" width="36pt" height="10pt" src="tc-15-2235-2021-ie00001.png"/></svg:svg> ∘ C), and high octahedral strains ( > 0.08), and emulating these conditions in laboratory experiments can take an impractically long time. It is possible to accelerate an experiment by running it at a higher temperature in the early stages and then lowering the temperature to meet the target conditions once the tertiary creep stage is reached. This can reduce total experiment run-time by > 1000 h; however it is not known whether this could affect the final strain rate or microstructure of the ice and potentially introduce a bias into the data. We deformed polycrystalline ice samples in uniaxial compression at −2 ∘ C before lowering the temperature to either −7 or −10 ∘ C, and we compared the results to constant-temperature experiments. Tertiary strain rates adjusted to the change in temperature very quickly (within 3 % of the total experiment run-time), with no significant deviation from strain rates measured in constant-temperature experiments. In experiments with a smaller temperature step ( −2 to −7 ∘ C) ...