Remote sensing of recent changes in permafrost-influenced wetlands

Changes in thermokarst lakes have been identified across many high-latitude ecosystems at different spatial and temporal scales. With the declassification of the Landsat archive in 2008, it is now possible to conduct a near-complete yearly time series of homogenous geospatial imagery to assess the trends seen in thermokarst lake surface area. By implementing an automated land- cover classification algorithm, this study examined the dynamics of lake surface area over different spatial and temporal scales in the Tuktoyaktuk Peninsula, Northwest Territories, Canada. Due to the presence of a statistically significant structural temporal break between the years 1997 and 1998, lake areal trends were estimated at two temporal scales, a longer term scale (1985 to 2011) and its component shorter scales (1985 to 1997 and 1998 to 2011). Large lakes saw the greatest changes both in lake areal increase and decreases at all temporal scales, and was suggested to drive the overall changes in surface area. In addition, regional differences were observed in the spatial distribution of individual lake area trends. On the broad scale, a latitudinal divide bifurcated the peninsula into two regions of approximately equal area, where the northern region exhibited general trends of lake areal decline, while the southern region exhibited general trends of lake areal increase. Within these regions, meso- and local hot and cold spots were identified, some that exhibited trends in concordance with local surroundings, while others represented local spatial heterogeneity in areal trends. The spatiotemporal trends in lake area were suggested to be influenced at varying scales by atmospheric and climate variables, and by ground characteristics such as coincident permafrost and surficial geology. As the Arctic continues to warm, a continued observation of thermokarst lake evolution over both broad landscapes and localised regions will be increasingly valuable to future studies that investigate the resulting transformation of the Arctic permafrost region

The Antarctic Flags project: a flagship outreach campaign for international cooperation

Antarctica does not have a flag. It is not a country, it has no indigenous population, and there is no government. Despite many countries laying claim to (often overlapping) parts of this frozen region, the continent was ultimately designated as a scientific preserve through the Antarctic Treaty. Military activity is explicitly banned by the Treaty, as are any activities that ‘shall constitute a basis for asserting, supporting or denying a claim to territorial sovereignty in Antarctica or create any rights of sovereignty in Antarctica’ (Article IV, Clause 2). The resulting tenet of scientific cooperation and collaboration underpins all modern activity on the continent and, ultimately, embodies the ideals of Antarctica and notions of Antarcticness. So why, every year, are hundreds of flags designed for Antarctica and sent to the continent from all over the world, if the continent is only to be used for peaceful activities? Originally conceived by the Foundation for the Good Governance of International Spaces, or ‘Our Spaces’,1 the Antarctic Flags project aims to connect schoolchildren to Antarctica through taking their flag designs to be flown on the frozen continent. The project was designed to be a school- level activity that could be carried out in celebration of Antarctica Day, which was established after the Antarctic Treaty Summit in 2009 to carry on the legacy of the Antarctic Treaty.2 The project, devised by Julie Hambrook Berkman, and expanded by the Association of Polar Early Career Scientists (APECS), the International Polar Foundation (IPF) and Polar Educators International (PEI), is now coordinated by early career scientists from the UK Polar Network (UKPN) and has involved participants from every non-Antarctic continent. Teachers are sent lesson suggestions, so that their students gain a true understanding of Antarctica’s unique position among the Earth’s continents before they create their designs. Flags from each school are then sent on to those travelling to Antarctica for scientific purposes to display (Figures 11.1–11.3). Here, we reflect on the impact of bringing Antarctica and Antarcticness into the classroom, discuss the evolution of the project with previous participants, and deliberate on perceptions of Antarctica, a continent which the majority of people will never visit, but still have a deep interest in

High-resolution distributed vertical strain and velocity from repeat borehole logging by optical televiewer:Derwael Ice Rise, Antarctica

Abstract Direct measurements of spatially distributed vertical strain within ice masses are scientifically valuable but challenging to acquire. We use manual marker tracking and automatic cross correlation between two repeat optical televiewer (OPTV) images of an ~100 m-long borehole at Derwael Ice Rise (DIR), Antarctica, to reconstruct discretised, vertical strain rate and velocity at millimetre resolution. The resulting profiles decay with depth, from −0.07 a −1 at the surface to ~−0.002 a −1 towards the base in strain and from −1.3 m a −1 at the surface to ~−0.5 m a −1 towards the base in velocity. Both profiles also show substantial local variability. Three coffee-can markers installed at different depths into adjacent boreholes record consistent strain rates and velocities, although averaged over longer depth ranges and subject to greater uncertainty. Measured strain-rate profiles generally compare closely with output from a 2-D ice-flow model, while the former additionally reveal substantial high-resolution variability. We conclude that repeat OPTV borehole logging represents an effective means of measuring distributed vertical strain at millimetre scale, revealing high-resolution variability along the uppermost ~100 m of DIR, Antarctica.info:eu-repo/semantics/publishe

Rapid basal melting of the Greenland Ice Sheet from surface meltwater drainage

Subglacial hydrologic systems regulate ice sheet flow, causing acceleration or deceleration, depending on hydraulic efficiency and the rate at which surface meltwater is delivered to the bed. Because these systems are rarely observed, ice sheet basal drainage represents a poorly integrated and uncertain component of models used to predict sea level changes. Here, we report radar-derived basal melt rates and unexpectedly warm subglacial conditions beneath a large Greenlandic outlet glacier. The basal melt rates averaged 14 mm ⋅d−1 over 4 months, peaking at 57 mm ⋅d−1 when basal water temperature reached +0.88 ∘C in a nearby borehole. We attribute both observations to the conversion of potential energy of surface water to heat in the basal drainage system, which peaked during a period of rainfall and intense surface melting. Our findings reveal limitations in the theory of channel formation, and we show that viscous dissipation far surpasses other basal heat sources, even in a distributed, high-pressure system

Resolving the internal and basal geometry of ice masses using imaging phase-sensitive radar

The phase-sensitive radio-echo sounder (pRES) is a powerful new instrument that can measure the depth of internal layers and the glacier bed to millimetre accuracy. We use a stationary 16-antenna pRES array on Store Glacier in West Greenland to measure the three-dimensional orientation of dipping internal reflectors, extending the capabilities of pRES beyond conventional depth sounding. This novel technique portrays the effectiveness of pRES in deriving the orientation of dipping internal layers that may complement profiles obtained through other geophysical surveying methods. Deriving ice vertical strain rates from changes in layer depth as measured by a sequence of pRES observations assumes that the internal reflections come from vertically beneath the antenna. By revealing the orientation of internal reflectors and the potential deviation from nadir of their associated reflections, the use of an antenna array can correct this assumption. While the array configuration was able to resolve the geometry of englacial layers, the same configuration could not be used to accurately image the glacier bed. Here, we use simulations of the performance of different array geometries to identify configurations that can be tailored to study different types of basal geometry for future deployments

Thermodynamics of a fast-moving Greenlandic outlet glacier revealed by fiber-optic distributed temperature sensing

Funding: This research was funded by the European Research Council as part of the RESPONDER project under the European Union’s Horizon 2020 research and innovation program (grant 683043). R.L. and T.R.C. were supported by Natural Environment Research Council Doctoral Training Partnership studentships (grant NE/ L002507/1). B.H. was supported by a HEFCW/Aberystwyth University Capital Equipment Grant.Measurements of ice temperature provide crucial constraints on ice viscosity and the thermodynamic processes occurring within a glacier. However, such measurements are presently limited by a small number of relatively coarse-spatial-resolution borehole records, especially for ice sheets. Here, we advance our understanding of glacier thermodynamics with an exceptionally high-vertical-resolution (~0.65 m), distributed-fiber-optic temperature-sensing profile from a 1043-m borehole drilled to the base of Sermeq Kujalleq (Store Glacier), Greenland. We report substantial but isolated strain heating within interglacial-phase ice at 208 to 242 m depth together with strongly heterogeneous ice deformation in glacial-phase ice below 889 m. We also observe a high-strain interface between glacial- and interglacial-phase ice and a 73-m-thick temperate basal layer, interpreted as locally formed and important for the glacier's fast motion. These findings demonstrate notable spatial heterogeneity, both vertically and at the catchment scale, in the conditions facilitating the fast motion of marine-terminating glaciers in Greenland.Publisher PDFPeer reviewe

Post-intervention Status in Patients With Refractory Myasthenia Gravis Treated With Eculizumab During REGAIN and Its Open-Label Extension

OBJECTIVE: To evaluate whether eculizumab helps patients with anti-acetylcholine receptor-positive (AChR+) refractory generalized myasthenia gravis (gMG) achieve the Myasthenia Gravis Foundation of America (MGFA) post-intervention status of minimal manifestations (MM), we assessed patients' status throughout REGAIN (Safety and Efficacy of Eculizumab in AChR+ Refractory Generalized Myasthenia Gravis) and its open-label extension. METHODS: Patients who completed the REGAIN randomized controlled trial and continued into the open-label extension were included in this tertiary endpoint analysis. Patients were assessed for the MGFA post-intervention status of improved, unchanged, worse, MM, and pharmacologic remission at defined time points during REGAIN and through week 130 of the open-label study. RESULTS: A total of 117 patients completed REGAIN and continued into the open-label study (eculizumab/eculizumab: 56; placebo/eculizumab: 61). At week 26 of REGAIN, more eculizumab-treated patients than placebo-treated patients achieved a status of improved (60.7% vs 41.7%) or MM (25.0% vs 13.3%; common OR: 2.3; 95% CI: 1.1-4.5). After 130 weeks of eculizumab treatment, 88.0% of patients achieved improved status and 57.3% of patients achieved MM status. The safety profile of eculizumab was consistent with its known profile and no new safety signals were detected. CONCLUSION: Eculizumab led to rapid and sustained achievement of MM in patients with AChR+ refractory gMG. These findings support the use of eculizumab in this previously difficult-to-treat patient population. CLINICALTRIALSGOV IDENTIFIER: REGAIN, NCT01997229; REGAIN open-label extension, NCT02301624. CLASSIFICATION OF EVIDENCE: This study provides Class II evidence that, after 26 weeks of eculizumab treatment, 25.0% of adults with AChR+ refractory gMG achieved MM, compared with 13.3% who received placebo