2015 Articles
Chaotic dynamics of a glaciohydraulic model
A model subglacial drainage system, coupled to an ice-dammed reservoir that receives a time-varying meltwater input, is described and analysed. In numerical experiments an ice-marginal lake drains through a subglacial channel, producing periodic floods, and fills with meltwater at a rate dependent on air temperature, which varies seasonally with a peak value of T m. The analysis reveals regions of T m parameter space corresponding to 'mode locking', where flood repeat time is independent of T m; resonance, where decreasing T m counter-intuitively increases flood size; and chaotic dynamics, where flood cycles are sensitive to initial conditions, never repeat and exhibit phase-space mixing. Bifurcations associated with abrupt changes in flood size and timing within the year separate these regions. This is the first time these complex dynamics have been displayed by a glaciohydraulic model and these findings have implications for our understanding of ice-marginal lakes, moulins and subglacial lakes.
Files
- Kingslake_202015.pdf application/pdf 2.49 MB Download File
Also Published In
- Title
- Journal of Glaciology
- DOI
- https://doi.org/10.3189/2015JoG14J208
More About This Work
- Academic Units
- Earth and Environmental Sciences
- Lamont-Doherty Earth Observatory
- Marine Geology and Geophysics
- Published Here
- March 21, 2016