Quantification of the ice-cored moraines' short-term dynamics in the high-Arctic glaciers Ebbabreen and Ragnarbreen, Petuniabukta, Svalbard

Abstract

Extensive ice-cored moraine complexes are common elements, marking the last advance of many Svalbard glaciers. Sediment gravity flows are among the most dynamic processes, transforming these landforms. The short-term (yearly and weekly) dynamics of mass-wasting processes were studied in a cm-scale using repetitive topographic scanning. We monitored several active sites on the forelands of two glaciers, Ebbabreen and Ragnarbreen, both of which are located near the Petuniabukta at the northern end of Billefjorden in Spitsbergen.The surveys indicate high dynamic rates of landforms' transformation. The mean annual volume loss of sediments and dead-ice for the most active parts of the moraines was up to 1.8 m a -1 . However, most of the transformation occurred during summer, with the short-term values of mean elevation changes as high as −104 mm day −1 . In comparison, the dynamics of the other (i.e. non-active) parts of the ice-cored moraines were much lower, namely, the mean annual lowering (attributed mainly to dead-ice downwasting) was up to 0.3 m a -1 , whereas lowering during summer was up to 8 mm day −1 . Our results indicate that in the case of the studied glaciers, backwasting was much more effective than downwasting in terms of landscape transformation in the glacier forelands. However, despite the high activity of localised mass movement processes, the overall short-term dynamics of ice-cored moraines for the studied glaciers were relatively low. We suggest that as long as debris cover is sufficiently thick (thicker than the permafrost's active layer depths), the mass movement activity would occur only under specific topographic conditions and/or due to occurrence of external meltwater sources and slope undercutting. In other areas, ice-cored moraines remain a stable landsystem component in a yearly to decadal time-scale. Graphical abstractPlease cite this article as: Ewertowski, Marek W., Tomczyk, Aleksandra M., Quantification of the ice-cored moraines' short-term dynamics in the high-Arctic glaciers Ebbabreen and Ragnarbreen, Petuniabukta, Svalbard, Geomorphology 234 (2015): 211-227,

Ice-cored moraine degradation mapped and quantified using an unmanned aerial vehicle: A case study from a polythermal glacier in Svalbard

“…ACCEPTED MANUSCRIPT (Ewertowski and Tomczyk, 2015). The evidence presented here indicates that such surface processes are less important with regard to the transformation of the lateral frontal moraine at Austre Lovénbreen.…”

“…An implication of this study is that the ice-cored moraines formed at Austre Lovénbreen, and potentially other valley glaciers in Svalbard (e.g. the recent results of Ewertowski and Tomczyk, 2015), may have higher preservation potential than previously recognised as insulating debris is not reworked and remains in situ.…”

“…It should be noted that the rate of change may not have remained consistent throughout the study period with moraines known to be subject to short-term changes over consecutive years (e.g. Ewertowski and Tomczyk, 2015). Even in areas with the highest levels of surface lowering (e.g.…”

“…Conversely, where debris cover is sufficiently thick, it has been reported that ice-cored moraine may stabilise, undergoing limited or negligible rates of transformation (Ewertowski, 2014;Ewertowski and Tomczyk, 2015).…”

“…However, the high-Arctic glacial environment in Svalbard is known for its highly unstable ice-cored moraine, and rapidly progressing mass wasting processes (Bennett et al, 2000;Schomacker, 2008;Irvine-Fynn et al, 2011;Ewertowski and Tomczyk, 2015). Schomacker (2008) …”