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Controls on jökulhlaup-transported buried ice melt-out at Skeiðarársandur, Iceland: Implications for the evolution of ice-marginal environments (2020)
Journal Article
Blauvelt, D. J., Russell, A. J., Large, A. R., Tweed, F. S., Hiemstra, J. F., Kulessa, B., …Waller, R. I. (2020). Controls on jökulhlaup-transported buried ice melt-out at Skeiðarársandur, Iceland: Implications for the evolution of ice-marginal environments. Geomorphology, 360, Article 107164. https://doi.org/10.1016/j.geomorph.2020.107164

High-magnitude jökulhlaups, glacier margin position and ice-thickness have been identified as key controls on sandur evolution. Existing models however have focused primarily on observations made during short windows of time and often do not account... Read More about Controls on jökulhlaup-transported buried ice melt-out at Skeiðarársandur, Iceland: Implications for the evolution of ice-marginal environments.

The empirical basis for modelling glacial erosion rates (2020)
Journal Article
Cook, S. J., Swift, D. A., Kirkbride, M. P., Knight, P. G., & Waller, R. I. (2020). The empirical basis for modelling glacial erosion rates. Nature communications, 11, Article 759. https://doi.org/10.1038/s41467-020-14583-8

Glaciers are highly effective agents of erosion that have profoundly shaped Earth’s surface, but there is uncertainty about how glacial erosion should be parameterised in landscape evolution models. Glacial erosion rate is usually modelled as a funct... Read More about The empirical basis for modelling glacial erosion rates.

The empirical basis for modelling glacial erosion rates. (2020)
Journal Article
Waller, & Knight. (2020). The empirical basis for modelling glacial erosion rates. Nature communications, https://doi.org/10.1038/s41467-020-14583-8

Glaciers are highly effective agents of erosion that have profoundly shaped Earth's surface, but there is uncertainty about how glacial erosion should be parameterised in landscape evolution models. Glacial erosion rate is usually modelled as a funct... Read More about The empirical basis for modelling glacial erosion rates..