Geospatial investigation on transitional (quiescence to surge initiation) phase dynamics of Monacobreen tidewater glacier, Svalbard

The change in the phase, from quiescence to surge, may perturb the glacier's dynamical behavior. To understand these changes through geospatial technique, the fastest moving tidewater Monacobreen Glacier, Svalbard, was studied for the year 2016-2019. It was elucidated that the surge had initiated during 2017-2018 before it the glacier was in quiescence since 2001. Initially, the glacier radar zones, namely percolation refreeze, lower percolation, and clean ice, were identified using the multi-temporal SAR data. These zones were utilized to delineate the equilibrium line altitude, and it was found that it is continuously moving down during surging, unlike the quiescence phase. The accumulation area ratio was always more than 0.67 throughout the analysis. The seasonal change in glacier surface velocity for both the phases was estimated, adapting the most appropriate Offset Tracking approach using the SAR data. The mean velocity over the main trunk was found to vary from 0.5 to 4 m/day. Thereafter, Glen's flow law equation was used to estimate the ice-thickness and found that the glacier has an average thickness range of 216-326 m in quiescence and 136-244 m during the surging. The analysis depicted that the basal shear stresses are increasing with surging, and the viscosity is decreasing. It can be said that the transition of the glacier from quiescent to surging phase has entirely changed its dynamic behavior and characteristics. Further, in the absence of field observations, the geospatial technique may provide reasonable estimates of the glacier's physical and dynamical parameters. (c) 2021 COSPAR. Published by Elsevier B.V. All rights reserved.

Automated summary

The transition of a glacier from quiescence to surge phase can significantly affect its dynamics and characteristics. The study conducted on the Monacobreen Glacier in Svalbard from 2016 to 2019 revealed that the glacier had been inactive since 2001 before experiencing a surge from 2017 to 2018. Geospatial techniques were employed to identify different radar zones within the glacier and track changes in equilibrium line altitude and surface velocity. The analysis demonstrated that the glacier's dynamic behavior and characteristics were altered during the surge phase. Geospatial techniques can provide reasonable estimates of a glacier's physical and dynamical parameters in the absence of field observations.