Observed snow depth trends in the European Alps: 1971 to 2019 The Cryosphere DOI 10.5194/tc-15-1343-2021 9 April 2021 Here, we present an Alpine-wide analysis of snow depth from six Alpine countries – Austria, France, Germany, Italy, Slovenia, and Switzerland – including altogether more than 2000 stations of which more than 800 were used for the trend assessment. Linear trends of monthly mean snow depth between1971 and 2019 showed decreases in snow depth for most stations from November to May. Read more
The case of a southern European glacier which survived Roman and medieval warm periods but is disappearing under recent warming The Cryosphere DOI 10.5194/tc-15-1157-2021 22 March 2021 We present here the first chronological study of a glacier located in the Central Pyrenees (NE Spain), Monte Perdido Glacier (MPG),carried out by different radiochronological techniques and a comparison with geochemical proxies from neighbouring palaeoclimate records. The chronological model evidences that the glacier persisted during the Roman period and the Medieval Climate Anomaly. The apparent absence of ice in the past∼ 600 years suggests that any ice accumulated during the Little Ice Age has since ablated. Read more
Diverging responses of high-latitude CO2 and CH4 emissions in idealized climate change scenarios The Cryosphere DOI 10.5194/tc-15-1097-2021 19 March 2021 The present study investigates the response of the high-latitude carbon cycle to changes in atmospheric greenhouse gas (GHG) concentrations in idealized climate change scenarios. We find that at a global mean temperature of roughly 1.75 K (±0.5 K) above pre-industrial levels the high-latitude ecosystem turns from a CO2 sink into a source of atmospheric carbon, with the net fluxes into the atmosphere increasing substantially with rising atmospheric GHG concentrations. This is very different from scenario simulations with the standard version of the MPI-ESM, in which the region continues to take up atmospheric CO2 throughout the entire 21st century. Read more
Mapping avalanches with satellites – evaluation of performance andcompleteness The Cryosphere DOI 10.5194/tc-15-983-2021 16 March 2021 The spatial distribution and size of avalanches are essential parameters for avalanche warning, avalanche documentation, mitigation measure design and hazard zonation. Despite its importance, this information is incomplete today and only available for limited areas and limited time periods. Read more
Macroscopic water vapor diffusion is not enhanced in snow The Cryosphere DOI 10.5194/tc-15-389-2021 12 February 2021 Here we show using theory and numerical simulations of idealized and measured snow microstructures that, although sublimation and deposition of water vapor onto snow crystal surfaces do enhance microscopic diffusion in the pore space, this effect is more than countered by the restriction of diffusion space due to ice. Read more
Review article: Earth’s ice imbalance The Cryosphere DOI 10.5194/tc-15-233-2021 9 February 2021 We combine satellite observations and numerical models to show that Earth lost 28 trillion tonnes of ice between 1994 and 2017. Read more
Brief communication: Heterogenous thinning and subglacial lake activity on Thwaites Glacier, West Antarctica The Cryosphere DOI 10.5194/tc-14-4603-2020 18 January 2021 The West Antarctic Ice Sheet has long been considered geometrically prone to collapse, and Thwaites Glacier, the largest glacier in the Amundsen Sea, is likely in the early stages of disintegration. Using observations of Thwaites Glacier velocity and elevation change, we show that the transport of ~2 km 3 of water beneath Thwaites Glacier has only a small and transient effect on glacier speed relative to ongoing thinning driven by ocean melt. Read more
The Antarctic sea ice cover from ICESat-2 and CryoSat-2: freeboard, snow depth, and ice thickness The Cryosphere DOI 10.5194/tc-14-4453-2020 31 December 2020 Our current understanding of Antarctic ice cover is largely informed by ice extent measurements from passive microwave sensors. These records, while useful, provide a limited picture of how the ice is responding to climate change. In this paper, we combine measurements from ICESat-2 and CryoSat-2 missions to assess snow depth and ice thickness of the Antarctic ice cover over an 8-month period (April through November 2019). The potential impact of salinity in the snow layer is discussed. ICESat-2 and CryoSat-2: freeboard, snow depth, and ice thickness">Read more
The catastrophic thermokarst lake drainage events of 2018 in northwesternAlaska: fast-forward into the future The Cryosphere DOI 10.5194/tc-14-4279-2020 30 December 2020 In summer 2018, northwestern Alaska was affected by widespread lake drainage which strongly exceeded previous observations. We analyzed the spatial and temporal patterns with remote sensing observations, weather data and lake-ice simulations. The preceding fall and winter season was the second warmest and wettest on record, causing the destabilization of permafrost and elevated water levels which likely led to widespread and rapid lake drainage during or right after ice breaku Read more
Distinguishing the impacts of ozone and ozone-depleting substanceson the recent increase in Antarctic surface mass balance The Cryosphere DOI 10.5194/tc-14-4135-2020 18 December 2020 The increase in Antarctic surface mass balance (SMB, precipitation vs. evaporation/sublimation) is projected to mitigate sea-level rise. Here we show that nearly half of this increase over the 20th century is attributed to stratospheric ozone depletion and ozone-depleting substance (ODS) emissions. Our results suggest that the phaseout of ODS by the Montreal Protocol, and the recovery of stratospheric ozone, will act to decrease the SMB over the 21st century and the mitigation of sea-level rise. Read more
