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            <title>TC - recent papers</title>
            <link>https://tc.copernicus.org/articles/</link>
            <description>Combined list of the recent articles of the journal The Cryosphere and the recent discussion forum The Cryosphere Discussions</description>
        <language>en</language>
            <item>
                <title>Sensitivity of the Bootstrap sea ice concentration algorithm to surface parameters in the Antarctic marginal ice zone using passive microwave retrievals</title>
                <link>https://doi.org/10.5194/tc-20-4465-2026</link>
                <guid>https://doi.org/10.5194/tc-20-4465-2026</guid>
                <description>
                    &lt;b&gt;Sensitivity of the Bootstrap sea ice concentration algorithm to surface parameters in the Antarctic marginal ice zone using passive microwave retrievals&lt;/b&gt;&lt;br&gt;
                    Marta Stentella, Ghislain Picard, Petra Heil, Jacqueline Boutin, Emmanuel Dinnat, and Stuart Corney&lt;br&gt;
                        The Cryosphere, 20, 4465&#8211;4489, https://doi.org/10.5194/tc-20-4465-2026, 2026&lt;br&gt;
                        Passive microwave radiometers are the primary tool for monitoring Antarctic sea ice, but their reliability decreases in the marginal ice zone between the pack ice and the open ocean. We simulate satellite observations to assess the impact of varying physical parameters on sea ice concentration retrievals. The largest errors are due to flooded/wet snow, thin ice, and roughened ocean surfaces. These findings can improve our interpretation of satellite observations and forecast sea ice changes.

                </description>

                <pubDate>Mon, 17 Aug 2026 12:29:47 +0200</pubDate>
            </item>
            <item>
                <title>Data-driven equation discovery of a sea ice albedo parametrisation</title>
                <link>https://doi.org/10.5194/tc-20-4437-2026</link>
                <guid>https://doi.org/10.5194/tc-20-4437-2026</guid>
                <description>
                    &lt;b&gt;Data-driven equation discovery of a sea ice albedo parametrisation&lt;/b&gt;&lt;br&gt;
                    Diajeng W. Atmojo, Katja Weigel, Arthur Grundner, Marika M. Holland, Dmitry Sidorenko, and Veronika Eyring&lt;br&gt;
                        The Cryosphere, 20, 4437&#8211;4464, https://doi.org/10.5194/tc-20-4437-2026, 2026&lt;br&gt;
                        This study presents an observation-driven sea ice albedo parametrisation by discovering an equation using symbolic regression, an interpretable machine learning method. Leveraging satellite and reanalyses data, our discovered equation identifies high sensitivity to thin snow and the weighted temperature difference between sea ice surface and 2 m air as critical to determine sea ice albedo. Our findings contribute to improving Arctic climate projections and understanding.

                </description>

                <pubDate>Fri, 14 Aug 2026 12:29:47 +0200</pubDate>
            </item>
            <item>
                <title>Anatomy and impact of a high Arctic atmospheric river driving extreme winter rain and snowfall</title>
                <link>https://doi.org/10.5194/tc-20-4421-2026</link>
                <guid>https://doi.org/10.5194/tc-20-4421-2026</guid>
                <description>
                    &lt;b&gt;Anatomy and impact of a high Arctic atmospheric river driving extreme winter rain and snowfall&lt;/b&gt;&lt;br&gt;
                    Hannah Bailey, Jason E. Box, Ben G. Kopec, Valtteri Hyöky, Hannu Marttila, Jeffrey M. Welker, Jack Kohler, Dmitry V. Divine, and Alun Hubbard&lt;br&gt;
                        The Cryosphere, 20, 4421&#8211;4436, https://doi.org/10.5194/tc-20-4421-2026, 2026&lt;br&gt;
                        Atmospheric rivers (ARs) are narrow corridors of intense heat and moisture that can deliver extreme weather to the Arctic. We investigate a record March 2022 event in Svalbard using measurements of air and precipitation to track its origin and evolution. While the AR brought unusual winter rain and snow melt, it also delivered substantial snowfall that partially offset glacier mass loss. These findings show that the impacts of ARs on Arctic glaciers are more complex than typically reported.

                </description>

                <pubDate>Fri, 14 Aug 2026 12:29:47 +0200</pubDate>
            </item>
            <item>
                <title>Experimental investigation of the direct shear strength parameters of compacted snow</title>
                <link>https://doi.org/10.5194/tc-20-4401-2026</link>
                <guid>https://doi.org/10.5194/tc-20-4401-2026</guid>
                <description>
                    &lt;b&gt;Experimental investigation of the direct shear strength parameters of compacted snow&lt;/b&gt;&lt;br&gt;
                    Haifeng Huo, Hui Xu, Jixiu Wu, Tao Li, Jingjin Liu, Enzhao Xiao, and Xueyuan Tang&lt;br&gt;
                        The Cryosphere, 20, 4401&#8211;4419, https://doi.org/10.5194/tc-20-4401-2026, 2026&lt;br&gt;
                        Through a series of direct shear tests, this study analyzes the variation of shear strength parameters (cohesion and internal friction angle) in compacted snow under different conditions of density, sintering time, and temperature. A Genetic Algorithm-Back Propagation neural network model was subsequently developed to establish systematic benchmark values for these parameters. This work provides essential data and a predictive framework for the reliable design of snow structures in cold regions.

                </description>

                <pubDate>Thu, 13 Aug 2026 12:29:47 +0200</pubDate>
            </item>
            <item>
                <title>Mapping snow on northern winter roads: a dual-frequency polarimetric radar approach for snow characterization over land, lake and sea ice</title>
                <link>https://doi.org/10.5194/tc-20-4367-2026</link>
                <guid>https://doi.org/10.5194/tc-20-4367-2026</guid>
                <description>
                    &lt;b&gt;Mapping snow on northern winter roads: a dual-frequency polarimetric radar approach for snow characterization over land, lake and sea ice&lt;/b&gt;&lt;br&gt;
                    Julienne Stroeve, Rosemary Willatt, Madeleine Downie, Monojit Saha, Carmen Nab, Alicia Fallows, Clement Soriot, Robbie Mallett, Anton Komarov, Vishnu Nandan, Thomas Newman, Jennifer Lukovich, and John Yackel&lt;br&gt;
                        The Cryosphere, 20, 4367&#8211;4399, https://doi.org/10.5194/tc-20-4367-2026, 2026&lt;br&gt;
                        We evaluate polarimetry for snow depth retrieval on Arctic winter transport routes. Over landfast ice and tundra, traditional dual-frequency (Ku/Ka) methods often fail. We demonstrate that cross-polarization (VH) provides a more reliable marker for snow/ice and snow/ground interfaces. For lakes, we successfully resolve air, snow, and ice interfaces to retrieve snow and ice thickness simultaneously. These results establish a baseline for future polarimetric satellite missions.

                </description>

                <pubDate>Wed, 12 Aug 2026 12:29:47 +0200</pubDate>
            </item>
            <item>
                <title>Assessing spatial heterogeneity of active layer thickness over Arctic-foothills tundra, North Slope Alaska</title>
                <link>https://doi.org/10.5194/tc-20-4277-2026</link>
                <guid>https://doi.org/10.5194/tc-20-4277-2026</guid>
                <description>
                    &lt;b&gt;Assessing spatial heterogeneity of active layer thickness over Arctic-foothills tundra, North Slope Alaska&lt;/b&gt;&lt;br&gt;
                    Jinyang Du, K. Arthur Endsley, Kazem Bakian Dogaheh, John S. Kimball, Mahta Moghaddam, Thomas A. Douglas, Asem Melebari, Sepehr Eskandari, Jinhyuk E. Kim, Jane Whitcomb, Yuhuan Zhao, and Sophia Henze&lt;br&gt;
                        The Cryosphere, 20, 4277&#8211;4291, https://doi.org/10.5194/tc-20-4277-2026, 2026&lt;br&gt;
                        Active layer thickness (ALT) is a sensitive indicator of the thawing Alaskan frozen soil, which may lead to increased greenhouse gas emissions, vegetation changes, and infrastructure damage. This study represents a multi-scale assessment of ALT spatial variations using observations including intensive field sampling, and drone, airborne and satellite remote sensing. Our study allows for improved interpretation of remote sensing and process-based ALT simulations for the changing Arctic.

                </description>

                <pubDate>Fri, 07 Aug 2026 12:29:47 +0200</pubDate>
            </item>
            <item>
                <title>A State-Space Model for Monitoring Greenland Ice Sheet Surface Elevation Change from CryoSat-2</title>
                <link>https://doi.org/10.5194/tc-20-4327-2026</link>
                <guid>https://doi.org/10.5194/tc-20-4327-2026</guid>
                <description>
                    &lt;b&gt;A State-Space Model for Monitoring Greenland Ice Sheet Surface Elevation Change from CryoSat-2&lt;/b&gt;&lt;br&gt;
                    Natalia H. Andersen, Sebastian B. Simonsen, Karina Nielsen, Mai Winstrup, Baptiste Vandecrux, Hui Gao, Beata Csatho, Anton Schenk, and Louise Sandberg Sørensen&lt;br&gt;
                        The Cryosphere, 20, 4327&#8211;4344, https://doi.org/10.5194/tc-20-4327-2026, 2026&lt;br&gt;
                        We developed a new statistical approach to track monthly changes in the surface height of the Greenland Ice Sheet using radar data from the CryoSat-2 satellite (2011–2025). The method lets seasonal and long-term variations emerge directly from the data, creating a consistent record of elevation change that helps reveal how Greenland responds to ongoing climate change.

                </description>

                <pubDate>Fri, 07 Aug 2026 12:29:47 +0200</pubDate>
            </item>
            <item>
                <title>A nine-year record of slush on the Greenland Ice Sheet</title>
                <link>https://doi.org/10.5194/tc-20-4345-2026</link>
                <guid>https://doi.org/10.5194/tc-20-4345-2026</guid>
                <description>
                    &lt;b&gt;A nine-year record of slush on the Greenland Ice Sheet&lt;/b&gt;&lt;br&gt;
                    Emily Glen, Alison F. Banwell, Katie E. Miles, Amber A. Leeson, Rebecca L. Dell, Malcolm McMillan, and Jennifer Maddalena&lt;br&gt;
                        The Cryosphere, 20, 4345&#8211;4365, https://doi.org/10.5194/tc-20-4345-2026, 2026&lt;br&gt;
                        Using satellite imagery and machine learning, we created the first Greenland-wide dataset of slush (waterlogged snow) from 2016 to 2024. Slush was widespread and varied strongly between years and across Greenland, becoming most extensive during high melt seasons. It was most common where melting was greater and snow had less capacity to store water. These findings show that slush should be included in models of future melting and sea-level rise.

                </description>

                <pubDate>Fri, 07 Aug 2026 12:29:47 +0200</pubDate>
            </item>
            <item>
                <title>Climatology and Interannual Variations in Arctic Winter Sea Ice Leads in the ICESat-2 Era</title>
                <link>https://doi.org/10.5194/tc-20-4313-2026</link>
                <guid>https://doi.org/10.5194/tc-20-4313-2026</guid>
                <description>
                    &lt;b&gt;Climatology and Interannual Variations in Arctic Winter Sea Ice Leads in the ICESat-2 Era&lt;/b&gt;&lt;br&gt;
                    Mengnan Zhao, Christopher Little, Nathan Kurtz, Rachel Tilling, and Jesse Wimert&lt;br&gt;
                        The Cryosphere, 20, 4313&#8211;4326, https://doi.org/10.5194/tc-20-4313-2026, 2026&lt;br&gt;
                        We take advantage of ICESat-2 satellite, which measures surface heights with nominal resolution of meters to tens of meters, to characterize a near pan-Arctic winter sea ice leads, meter-scale elongated cracks in ice, from 2018 to 2024. We find that lead fractions are higher near the ice edge and sizes follow a power-law distribution. Four distinct features in the temporal evolution of lead fraction are also identified, with fraction increase associated with larger leads.

                </description>

                <pubDate>Fri, 07 Aug 2026 12:29:47 +0200</pubDate>
            </item>
            <item>
                <title>Glacier surges on James Ross Island, Antarctica, and their relationship with climate</title>
                <link>https://doi.org/10.5194/tc-20-4293-2026</link>
                <guid>https://doi.org/10.5194/tc-20-4293-2026</guid>
                <description>
                    &lt;b&gt;Glacier surges on James Ross Island, Antarctica, and their relationship with climate&lt;/b&gt;&lt;br&gt;
                    Benjamin J. Davison, Andrew J. Sole, Gregoire Guillet, Douglas I. Benn, Jonathan Kingslake, Jeremy C. Ely, Stephen J. Livingstone, Christopher D. Stringer, Jonathan L. Carrivick, and Anna E. Hogg&lt;br&gt;
                        The Cryosphere, 20, 4293&#8211;4311, https://doi.org/10.5194/tc-20-4293-2026, 2026&lt;br&gt;
                        Some glaciers flow slowly for many years before dramatically accelerating. This is usually a sign of a surge. Theory and observations suggest that surges occur in certain climates. The Antarctic Peninsula has such a climate yet only one surge has been observed there. We present detailed observations of three glaciers that surged recently. We explore how climate change over the past hundred years, and projected climate change up to 2150, has and will affect surging behaviour on the Peninsula.

                </description>

                <pubDate>Fri, 07 Aug 2026 12:29:47 +0200</pubDate>
            </item>
            <item>
                <title>Current morphodynamics and subsurface structure of thrust moraines and rock glaciers connected to three Little Ice Age glacier forefields in the Swiss Alps</title>
                <link>https://doi.org/10.5194/tc-20-4255-2026</link>
                <guid>https://doi.org/10.5194/tc-20-4255-2026</guid>
                <description>
                    &lt;b&gt;Current morphodynamics and subsurface structure of thrust moraines and rock glaciers connected to three Little Ice Age glacier forefields in the Swiss Alps&lt;/b&gt;&lt;br&gt;
                    Julius Kunz, Sebastian Buchelt, Tim Wiegand, Tobias Ullmann, and Christof Kneisel&lt;br&gt;
                        The Cryosphere, 20, 4255&#8211;4275, https://doi.org/10.5194/tc-20-4255-2026, 2026&lt;br&gt;
                        Glacier-permafrost interactions in Alpine environments influence geomorphological processes, making it essential to understand the relationship between subsurface structures and surface morphodynamics for predicting landscape evolution under climate change. This study uses applied geophysics and remote sensing methods to investigate this relationship and to reveal the distribution of different ground ice types, as well as the related surface morphodynamics in three alpine glacier forefields.

                </description>

                <pubDate>Thu, 06 Aug 2026 12:29:47 +0200</pubDate>
            </item>
            <item>
                <title>Sensitivity of Andean Glaciers to ice-flow parameters in the Parallel Ice Sheet Model</title>
                <link>https://doi.org/10.5194/tc-20-4209-2026</link>
                <guid>https://doi.org/10.5194/tc-20-4209-2026</guid>
                <description>
                    &lt;b&gt;Sensitivity of Andean Glaciers to ice-flow parameters in the Parallel Ice Sheet Model&lt;/b&gt;&lt;br&gt;
                    Ethan Lee, Jeremy C. Ely, Sarah L. Bradley, Tamsin L. Edwards, and Bethan J. Davies&lt;br&gt;
                        The Cryosphere, 20, 4209&#8211;4233, https://doi.org/10.5194/tc-20-4209-2026, 2026&lt;br&gt;
                        South American Andean glaciers are the least well known in their futures. We can use numerical models to estimate the change of these glaciers to future climate change. However, options within the numerical model which effect the results are unknown. We vary these selected important options to understand their effect on the numerical model output across the South American Andes. We find that how the model approximates sediment friction, and sliding, to be important on model output.

                </description>

                <pubDate>Thu, 30 Jul 2026 12:29:47 +0200</pubDate>
            </item>
            <item>
                <title>The Modèle Atmosphérique Régional – Intelligence Artificielle (MAR-IA): surface meltwater over Greenland</title>
                <link>https://doi.org/10.5194/tc-20-4235-2026</link>
                <guid>https://doi.org/10.5194/tc-20-4235-2026</guid>
                <description>
                    &lt;b&gt;The Modèle Atmosphérique Régional – Intelligence Artificielle (MAR-IA): surface meltwater over Greenland&lt;/b&gt;&lt;br&gt;
                    Marco Tedesco, Racheet Matai, and Xavier Fettweis&lt;br&gt;
                        The Cryosphere, 20, 4235&#8211;4253, https://doi.org/10.5194/tc-20-4235-2026, 2026&lt;br&gt;
                        We developed a machine learning emulator of a climate model simulating melting over Greenland that performs as well as the original model but it is much faster. We show that this emulator can be used as powerful tools to complement regional climate models by enabling computationally efficient ensemble simulations and physically interpretable attribution of past and future Greenland surface melt. Development of regional climate models should go hand in hand with ML-based tools.

                </description>

                <pubDate>Thu, 30 Jul 2026 12:29:47 +0200</pubDate>
            </item>
            <item>
                <title>Svalbard glacier calving front changes from the 1930s to the 1970s from archived satellite and aerial images</title>
                <link>https://doi.org/10.5194/tc-20-4133-2026</link>
                <guid>https://doi.org/10.5194/tc-20-4133-2026</guid>
                <description>
                    &lt;b&gt;Svalbard glacier calving front changes from the 1930s to the 1970s from archived satellite and aerial images&lt;/b&gt;&lt;br&gt;
                    Loris Danjou, Eero Rinne, and Erik Schytt Mannerfelt&lt;br&gt;
                        The Cryosphere, 20, 4133&#8211;4155, https://doi.org/10.5194/tc-20-4133-2026, 2026&lt;br&gt;
                        We retrieved front locations for 171 Svalbard tidewater glaciers in the 1960s and 1970s, from Landsat images and – for the first time in this region – declassified intelligence satellite photographs. We compared our results to aerial photographs from the 1930s and calculated that these glaciers retreated by about 1 km between 1936 and 1978. We also discovered one undocumented glacier surge (a rapid front advance), precised the time frames of two others, and documented two other glacier advances.

                </description>

                <pubDate>Tue, 28 Jul 2026 12:29:47 +0200</pubDate>
            </item>
            <item>
                <title>Evaluation of representation of seasonally frozen ground characteristics in Land Surface Models: JSBACH and CLM</title>
                <link>https://doi.org/10.5194/tc-20-4157-2026</link>
                <guid>https://doi.org/10.5194/tc-20-4157-2026</guid>
                <description>
                    &lt;b&gt;Evaluation of representation of seasonally frozen ground characteristics in Land Surface Models: JSBACH and CLM&lt;/b&gt;&lt;br&gt;
                    Mittal Parmar, Kristina Fröhlich, Antonella Sanna, Tobias Stacke, Marianna Benassi, Zhicheng Luo, Daniele Peano, and Bodo Ahrens&lt;br&gt;
                        The Cryosphere, 20, 4157&#8211;4184, https://doi.org/10.5194/tc-20-4157-2026, 2026&lt;br&gt;
                        Seasonally frozen ground strongly influences land–atmosphere interactions, yet its simulation remains uncertain in land surface models. This study evaluates 2 standalone LSM simulations forced by reanalysis data (1986-2022) and validates results against reference observations at 26 Russian sites. Results show contrasting biases linked to snow insulation and freeze–thaw processes, highlighting the need for improved snow and soil parameterizations.

                </description>

                <pubDate>Tue, 28 Jul 2026 12:29:47 +0200</pubDate>
            </item>
            <item>
                <title>Comparing high spatial and temporal resolution snow depth measurements and modelling results in an avalanche release area</title>
                <link>https://doi.org/10.5194/tc-20-4185-2026</link>
                <guid>https://doi.org/10.5194/tc-20-4185-2026</guid>
                <description>
                    &lt;b&gt;Comparing high spatial and temporal resolution snow depth measurements and modelling results in an avalanche release area&lt;/b&gt;&lt;br&gt;
                    Pia Ruttner, Nora Helbig, Annelies Voordendag, Andreas Wieser, and Yves Bühler&lt;br&gt;
                        The Cryosphere, 20, 4185&#8211;4208, https://doi.org/10.5194/tc-20-4185-2026, 2026&lt;br&gt;
                        The spatial variability of snow depth distribution in avalanche release areas is key for avalanche forecasting but is strongly influenced by the interaction of wind with the terrain. We generate maps of high resolution snow depth changes during three snowfall events by using low-cost terrestrial laser scanner measurements and compare them to the results of selected snow depth distribution models. We show that basic terrain derivations have the highest correlations to our measurement results.

                </description>

                <pubDate>Tue, 28 Jul 2026 12:29:47 +0200</pubDate>
            </item>
            <item>
                <title>Evolution of Maud Rise Polynya during the last 250 years – a multiproxy ice core reconstruction from coastal Dronning Maud Land, Antarctica</title>
                <link>https://doi.org/10.5194/tc-20-4117-2026</link>
                <guid>https://doi.org/10.5194/tc-20-4117-2026</guid>
                <description>
                    &lt;b&gt;Evolution of Maud Rise Polynya during the last 250 years – a multiproxy ice core reconstruction from coastal Dronning Maud Land, Antarctica&lt;/b&gt;&lt;br&gt;
                    Rahul Dey, Chavarukonam M. Laluraj, Kenichi Matsuoka, Ashish Paiguinkar, Bhikaji L. Redkar, and Meloth Thamban&lt;br&gt;
                        The Cryosphere, 20, 4117&#8211;4131, https://doi.org/10.5194/tc-20-4117-2026, 2026&lt;br&gt;
                        We present a 250-year reconstruction of the Maud Rise Polynya opening, using an ice core collected from coastal Antarctica. This polynya is considered a rare phenomenon in the Weddell Sea, with only two well-documented openings since the 1970s. However, our 250-year record reveals numerous past polynya events, including occurrences possibly comparable in scale to the Great Weddell Polynya of 1974–1976, suggesting that these openings are a part of the Southern Ocean's natural variability.

                </description>

                <pubDate>Mon, 27 Jul 2026 12:29:47 +0200</pubDate>
            </item>
            <item>
                <title>Evolution of the Antarctic Ice Sheet from 2000–2300 and beyond: model sensitivity and uncertainty analysis using MPAS-Albany Land Ice</title>
                <link>https://doi.org/10.5194/tc-20-4061-2026</link>
                <guid>https://doi.org/10.5194/tc-20-4061-2026</guid>
                <description>
                    &lt;b&gt;Evolution of the Antarctic Ice Sheet from 2000–2300 and beyond: model sensitivity and uncertainty analysis using MPAS-Albany Land Ice&lt;/b&gt;&lt;br&gt;
                    Trevor R. Hillebrand, Matthew J. Hoffman, Holly K. Han, Mauro Perego, Alexander O. Hager, Andrew Nolan, Xylar Asay-Davis, Stephen F. Price, Jerry Watkins, and Max Carlson&lt;br&gt;
                        The Cryosphere, 20, 4061&#8211;4098, https://doi.org/10.5194/tc-20-4061-2026, 2026&lt;br&gt;
                        We present new simulations that complement our contribution to the ISMIP6-Antarctica-2300 ensemble. We find significant mass loss after 2300 under both low-emissions and present-day forcing. Thermal evolution is extremely important, with fixed temperature yielding up to almost twice as much mass loss as simulations with evolving temperature. External forcing uncertainty, rather than parameter uncertainty, dominates the ensemble spread after 2050.

                </description>

                <pubDate>Fri, 24 Jul 2026 12:29:47 +0200</pubDate>
            </item>
            <item>
                <title>Assessing the effect of land cover on ISBA snow water equivalent and land surface temperature simulations over Europe</title>
                <link>https://doi.org/10.5194/tc-20-4099-2026</link>
                <guid>https://doi.org/10.5194/tc-20-4099-2026</guid>
                <description>
                    &lt;b&gt;Assessing the effect of land cover on ISBA snow water equivalent and land surface temperature simulations over Europe&lt;/b&gt;&lt;br&gt;
                    Oscar Rojas-Munoz, Constantin Ardilouze, Bertrand Bonan, Diane Tzanos, Darren Ghent, Céline Lamarche, Thomas Nagler, and Jean-Christophe Calvet&lt;br&gt;
                        The Cryosphere, 20, 4099&#8211;4115, https://doi.org/10.5194/tc-20-4099-2026, 2026&lt;br&gt;
                        This study evaluated how updating land cover maps, such as forests, grasslands, and croplands, affects simulations of snow and land surface temperatures across Europe from 2010 to 2022. Results using older, less detailed maps were compared with those from newer, high-resolution data. The updated maps improved the accuracy of snow predictions, particularly in areas where grasslands transitioned to forests. However, the improvements were less noticeable for temperature simulations. 

                </description>

                <pubDate>Fri, 24 Jul 2026 12:29:47 +0200</pubDate>
            </item>
            <item>
                <title>Brief communication: Two-year MRR observations at Great Wall Station, Antarctic Peninsula region</title>
                <link>https://doi.org/10.5194/tc-20-4049-2026</link>
                <guid>https://doi.org/10.5194/tc-20-4049-2026</guid>
                <description>
                    &lt;b&gt;Brief communication: Two-year MRR observations at Great Wall Station, Antarctic Peninsula region&lt;/b&gt;&lt;br&gt;
                    Jiayi Sun, Junmei Lv, Haoran Li, Wenqian Zhang, Biao Tian, and Minghu Ding&lt;br&gt;
                        The Cryosphere, 20, 4049&#8211;4059, https://doi.org/10.5194/tc-20-4049-2026, 2026&lt;br&gt;
                        This study reports two years of Micro Rain Radar observations from Great Wall Station, from March 2024 to February 2026. Near-surface precipitation and snowfall occurred during 32 % and 21 % of the time. The signal changed little with height, suggesting frequent shallow snowfall. Weak winds had little effect, while stronger winds likely affected radar observations below 0.7 km. A radar-based snowfall estimate shows that the ERA5 reanalysis product underestimates cumulative snowfall.

                </description>

                <pubDate>Thu, 23 Jul 2026 12:29:47 +0200</pubDate>
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