Annual Greenland accumulation rates (2009–2012) from airborne snow radar The Cryosphere DOI 10.5194/tc-10-1739-2016 11 August 2016 Contemporary climate warming over the Arctic is accelerating mass loss from the Greenland Ice Sheet through increasing surface melt, emphasizing the need to closely monitor surface mass balance in order to improve sea-level rise predictions. Here, we quantify the net annual accumulation over the Greenland Ice Sheet, which comprises the largest component of surface mass balance, at a higher spatial resolution than currently available using high-resolution, airborne-radar data. Read more
Wave climate in the Arctic 1992–2014: seasonality and trends The Cryosphere DOI 10.5194/tc-10-1605-2016 26 July 2016 Satellite observations show the Arctic sea ice has decreased the last 30 years. From our wave model hindcast and satellite altimeter datasets we observe profound increasing wave heights, which are caused by the loss of sea ice and not the driving winds. If ice-free conditions persist later into fall, then regions like the Beaufort–Chukchi Sea will be prone to developing larger waves since the driving winds are strong this time of year. Read more
Which are the highest peaks in the US Arctic? Fodar settles the debate The Cryosphere DOI 10.5194/tc-10-1245-2016 23 June 2016 We measured the heights of the five tallest peaks in the US Arctic using fodar, a new airborne photogrammetric technique using structure-from-motion software. The highest peaks are Mt Isto (2735.6 m), Mt. Hubley (2717.6 m), Mt. Chamberlin (2712.3 m), Mt. Michelson (2698.1 m), and an unnamed peak (2694.9 m). We found fodar suitable for topographic change detection on the centimeter scale in steep mountain terrain, such as for measuring snow depths. Read more
Greenland Ice Sheet seasonal and spatial mass variability from model simulations and GRACE (2003–2012) The Cryosphere DOI 10.5194/tc-10-1259-2016 20 June 2016 We compared satellite-derived estimates of spatial and seasonal variations in Greenland Ice Sheet mass with a set of model simulations, revealing an agreement between models and satellite estimates for the ice-sheet-wide seasonal fluctuations in mass, but disagreement at finer spatial scales. The model simulations underestimate low-elevation mass loss. Improving the ability of models to capture variations and trends in Greenland Ice Sheet mass is important for estimating future sea level rise. GRACE (2003–2012)">Read more
Recent summer sea ice thickness surveys in Fram Strait and associated ice volume fluxes The Cryosphere DOI 10.5194/tc-10-523-2016 8 March 2016 We present an extensive data set of ground-based and airborne electromagnetic ice thickness measurements covering Fram Strait in summer between 2001 and 2012. An investigation of back trajectories of surveyed sea ice using satellite-based sea ice motion data allows us to examine the connection between thickness variability, ice age and source area. In addition, we determine across and along strait gradients in ice thickness and associated volume fluxes. Read more
Bulk meltwater flow and liquid water content of snowpacks mapped using the electrical self-potential (SP) method The Cryosphere DOI 10.5194/tc-10-433-2016 29 February 2016 We show that strong electrical self-potential fields are generated in melting in in situ snowpacks at Rhone Glacier and Jungfraujoch Glacier, Switzerland. We conclude that the electrical self-potential method is a promising snow and firn hydrology sensor, owing to its suitability for sensing lateral and vertical liquid water flows directly and minimally invasively, complementing established observational programs and monitoring autonomously at a low cost. Read more
Committed retreat of Smith, Pope, and Kohler Glaciers over the next 30 years inferred by transient model calibration The Cryosphere DOI 10.5194/tc-9-2429-2015 21 December 2015 We calibrate a time-dependent ice model through optimal fit to transient observations of surface elevation and velocity, a novel procedure in glaciology and in particular for an ice stream with a dynamic grounding line. We show this procedure gives a level of confidence in model projections that cannot be achieved through more commonly used glaciological data assimilation methods. We show that Smith Glacier is in a state of retreat regardless of climatic forcing for the next several decades. Read more
Reducing uncertainties in projections of Antarctic ice mass loss The Cryosphere DOI 10.5194/tc-9-2043-2015 9 November 2015 Projections of Antarctic dynamics and contribution to sea-level rise are evaluated in the light of intercomparison exercises dedicated to evaluate models’ ability of representing coastal changes. Uncertainties in projections can be substantially decreased if a selection of models is made and models that are unqualified for the representation of coastal dynamics are excluded. Read more
Retrieving the paleoclimatic signal from the deeper part of the EPICA Dome C ice core The Cryosphere DOI 10.5194/tc-9-1633-2015 20 August 2015 The oldest paleoclimatic information is buried within the lowermost layers of deep ice cores. It is therefore essential to judge how deep these records remain unaltered. We study the bottom 60 meters of the EPICA Dome C ice core from central Antarctica to show that the paleoclimatic signal is only affected at the small scale (decimeters) in terms of some of the global ice properties. However our data suggest that the time scale has been considerably distorted by mechanical stretching. EPICA Dome C ice core">Read more
Century-scale simulations of the response of the West Antarctic Ice Sheet to a warming climate The Cryosphere DOI 10.5194/tc-9-1579-2015 18 August 2015 We used a high resolution ice sheet model capable of resolving grouding line dynamics (BISICLES) to compute responses of the major West Antarctic ice streams to projections of ocean and atmospheric warming. This is computationally demanding, and although other groups have considered parts of West Antarctica, we think this is the first calculation for the whole region at the sub-kilometer resolution that we show is required. Read more
