Articles | Volume 10, issue 6
https://doi.org/10.5194/bg-10-4297-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Special issue:
https://doi.org/10.5194/bg-10-4297-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
27 Jun 2013
Research article |
| 27 Jun 2013
Short- and long-term thermo-erosion of ice-rich permafrost coasts in the Laptev Sea region
F. Günther
Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research, Potsdam, Germany
P. P. Overduin
Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research, Potsdam, Germany
A. V. Sandakov
Melnikov Permafrost Institute, Russian Academy of Sciences, Siberian Branch, Yakutsk, Russia
G. Grosse
Geophysical Institute, University of Alaska Fairbanks, Alaska, Fairbanks, USA
M. N. Grigoriev
Melnikov Permafrost Institute, Russian Academy of Sciences, Siberian Branch, Yakutsk, Russia
Related authors
Thomas Opel, Julian B. Murton, Sebastian Wetterich, Hanno Meyer, Kseniia Ashastina, Frank Günther, Hendrik Grotheer, Gesine Mollenhauer, Petr P. Danilov, Vasily Boeskorov, Grigoriy N. Savvinov, and Lutz Schirrmeister
Clim. Past, 15, 1443–1461, https://doi.org/10.5194/cp-15-1443-2019, https://doi.org/10.5194/cp-15-1443-2019, 2019
Short summary
Short summary
To reconstruct past winter climate, we studied ice wedges at two sites in the Yana Highlands, interior Yakutia (Russia), the most continental region of the Northern Hemisphere. Our ice wedges of the upper ice complex unit of the Batagay megaslump and a river terrace show much more depleted stable-isotope compositions than other study sites in coastal and central Yakutia, reflecting lower winter temperatures and a higher continentality of the study region during Marine Isotope Stages 3 and 1.
Matthias Fuchs, Guido Grosse, Jens Strauss, Frank Günther, Mikhail Grigoriev, Georgy M. Maximov, and Gustaf Hugelius
Biogeosciences, 15, 953–971, https://doi.org/10.5194/bg-15-953-2018, https://doi.org/10.5194/bg-15-953-2018, 2018
Short summary
Short summary
Our paper investigates soil organic carbon and nitrogen in permafrost soils on Sobo-Sise Island and Bykovsky Peninsula in the north of eastern Siberia. We collected and analysed permafrost soil cores and upscaled carbon and nitrogen stocks to landscape level. We found large amounts of carbon and nitrogen stored in these frozen soils, reconstructed sedimentation rates and estimated the potential increase in organic carbon availability if permafrost continues to thaw and active layer deepens.
Simon Zwieback, Steven V. Kokelj, Frank Günther, Julia Boike, Guido Grosse, and Irena Hajnsek
The Cryosphere, 12, 549–564, https://doi.org/10.5194/tc-12-549-2018, https://doi.org/10.5194/tc-12-549-2018, 2018
Short summary
Short summary
We analyse elevation losses at thaw slumps, at which icy sediments are exposed. As ice requires a large amount of energy to melt, one would expect that mass wasting is governed by the available energy. However, we observe very little mass wasting in June, despite the ample energy supply. Also, in summer, mass wasting is not always energy limited. This highlights the importance of other processes, such as the formation of a protective veneer, in shaping mass wasting at sub-seasonal scales.
Sina Muster, Kurt Roth, Moritz Langer, Stephan Lange, Fabio Cresto Aleina, Annett Bartsch, Anne Morgenstern, Guido Grosse, Benjamin Jones, A. Britta K. Sannel, Ylva Sjöberg, Frank Günther, Christian Andresen, Alexandra Veremeeva, Prajna R. Lindgren, Frédéric Bouchard, Mark J. Lara, Daniel Fortier, Simon Charbonneau, Tarmo A. Virtanen, Gustaf Hugelius, Juri Palmtag, Matthias B. Siewert, William J. Riley, Charles D. Koven, and Julia Boike
Earth Syst. Sci. Data, 9, 317–348, https://doi.org/10.5194/essd-9-317-2017, https://doi.org/10.5194/essd-9-317-2017, 2017
Short summary
Short summary
Waterbodies are abundant in Arctic permafrost lowlands. Most waterbodies are ponds with a surface area smaller than 100 x 100 m. The Permafrost Region Pond and Lake Database (PeRL) for the first time maps ponds as small as 10 x 10 m. PeRL maps can be used to document changes both by comparing them to historical and future imagery. The distribution of waterbodies in the Arctic is important to know in order to manage resources in the Arctic and to improve climate predictions in the Arctic.
Pier Paul Overduin, Sebastian Wetterich, Frank Günther, Mikhail N. Grigoriev, Guido Grosse, Lutz Schirrmeister, Hans-Wolfgang Hubberten, and Aleksandr Makarov
The Cryosphere, 10, 1449–1462, https://doi.org/10.5194/tc-10-1449-2016, https://doi.org/10.5194/tc-10-1449-2016, 2016
Short summary
Short summary
How fast does permafrost warm up and thaw after it is covered by the sea? Ice-rich permafrost in the Laptev Sea, Siberia, is rapidly eroded by warm air and waves. We used a floating electrical technique to measure the depth of permafrost thaw below the sea, and compared it to 60 years of coastline retreat and permafrost depths from drilling 30 years ago. Thaw is rapid right after flooding of the land and slows over time. The depth of permafrost is related to how fast the coast retreats.
F. Günther, P. P. Overduin, I. A. Yakshina, T. Opel, A. V. Baranskaya, and M. N. Grigoriev
The Cryosphere, 9, 151–178, https://doi.org/10.5194/tc-9-151-2015, https://doi.org/10.5194/tc-9-151-2015, 2015
Short summary
Short summary
Coastal erosion rates at Muostakh Island (eastern Siberian Arctic) have doubled, based on remotely sensed observations of land loss, and therefore the island will disappear prematurely. Based on analyses of seasonal variability of permafrost thaw, thermo-erosion increases by 1.2m per year when summer temperatures rise by 1°C. Due to rapid permafrost thaw, the land surface is subsiding up to 11cm per year, based on comparison of elevation changes and active layer thaw depth.
B. Heim, E. Abramova, R. Doerffer, F. Günther, J. Hölemann, A. Kraberg, H. Lantuit, A. Loginova, F. Martynov, P. P. Overduin, and C. Wegner
Biogeosciences, 11, 4191–4210, https://doi.org/10.5194/bg-11-4191-2014, https://doi.org/10.5194/bg-11-4191-2014, 2014
Lydia Stolpmann, Ingmar Nitze, Ingeborg Bussmann, Benjamin M. Jones, Josefine Lenz, Hanno Meyer, Juliane Wolter, and Guido Grosse
EGUsphere, https://doi.org/10.5194/egusphere-2024-2822, https://doi.org/10.5194/egusphere-2024-2822, 2024
Short summary
Short summary
We combine hydrochemical and lake change data to show consequences of permafrost thaw induced lake changes on hydrochemistry, which are relevant for the global carbon cycle. We found higher methane concentrations in lakes that do not freeze to the ground and show that lagoons have lower methane concentrations than lakes. Our detailed lake sampling approach show higher concentrations in Dissolved Organic Carbon in areas of higher erosion rates, that might increase under the climate warming.
Nina Nesterova, Marina Leibman, Alexander Kizyakov, Hugues Lantuit, Ilya Tarasevich, Ingmar Nitze, Alexandra Veremeeva, and Guido Grosse
The Cryosphere, 18, 4787–4810, https://doi.org/10.5194/tc-18-4787-2024, https://doi.org/10.5194/tc-18-4787-2024, 2024
Short summary
Short summary
Retrogressive thaw slumps (RTSs) are widespread in the Arctic permafrost landforms. RTSs present a big interest for researchers because of their expansion due to climate change. There are currently different scientific schools and terminology used in the literature on this topic. We have critically reviewed existing concepts and terminology and provided clarifications to present a useful base for experts in the field and ease the introduction to the topic for scientists who are new to it.
Maren Jenrich, Juliane Wolter, Susanne Liebner, Christian Knoblauch, Guido Grosse, Fiona Giebeler, Dustin Whalen, and Jens Strauss
EGUsphere, https://doi.org/10.5194/egusphere-2024-2891, https://doi.org/10.5194/egusphere-2024-2891, 2024
Short summary
Short summary
Climate warming in the Arctic is causing the erosion of permafrost coasts and the transformation of permafrost lakes into lagoons. To understand how this affects greenhouse gas (GHG) emissions, we studied carbon dioxide (CO₂) and methane (CH₄) production in lagoons with varying sea connections. Younger lagoons produce more CH₄, while CO₂ increases in more marine conditions. Flooding of permafrost lowlands due to rising sea levels may lead to higher GHG emissions from Arctic coasts in the future.
Soraya Kaiser, Julia Boike, Guido Grosse, and Moritz Langer
Earth Syst. Sci. Data, 16, 3719–3753, https://doi.org/10.5194/essd-16-3719-2024, https://doi.org/10.5194/essd-16-3719-2024, 2024
Short summary
Short summary
Arctic warming, leading to permafrost degradation, poses primary threats to infrastructure and secondary ecological hazards from possible infrastructure failure. Our study created a comprehensive Alaska inventory combining various data sources with which we improved infrastructure classification and data on contaminated sites. This resource is presented as a GeoPackage allowing planning of infrastructure damage and possible implications for Arctic communities facing permafrost challenges.
Bennet Juhls, Anne Morgenstern, Jens Hölemann, Antje Eulenburg, Birgit Heim, Frederieke Miesner, Hendrik Grotheer, Gesine Mollenhauer, Hanno Meyer, Ephraim Erkens, Felica Yara Gehde, Sofia Antonova, Sergey Chalov, Maria Tereshina, Oxana Erina, Evgeniya Fingert, Ekaterina Abramova, Tina Sanders, Liudmila Lebedeva, Nikolai Torgovkin, Georgii Maksimov, Vasily Povazhnyi, Rafael Gonçalves-Araujo, Urban Wünsch, Antonina Chetverova, Sophie Opfergelt, and Pier Paul Overduin
Earth Syst. Sci. Data Discuss., https://doi.org/10.5194/essd-2024-290, https://doi.org/10.5194/essd-2024-290, 2024
Revised manuscript accepted for ESSD
Short summary
Short summary
The Siberian Arctic is warming fast: permafrost is thawing, river chemistry is changing, and coastal ecosystems are affected. We want to understand changes to the Lena River, a major Arctic river flowing to the Arctic Ocean, by collecting 4.5 years of detailed water data, including temperature and carbon and nutrient contents. This dataset records current conditions and helps us to detect future changes. Explore it at https://doi.org/10.1594/PANGAEA.913197 and https://lena-monitoring.awi.de/.
Frederieke Miesner, William Lambert Cable, Pier Paul Overduin, and Julia Boike
The Cryosphere, 18, 2603–2611, https://doi.org/10.5194/tc-18-2603-2024, https://doi.org/10.5194/tc-18-2603-2024, 2024
Short summary
Short summary
The temperature in the sediment below Arctic lakes determines the stability of the permafrost and microbial activity. However, measurements are scarce because of the remoteness. We present a robust and portable device to fill this gap. Test campaigns have demonstrated its utility in a range of environments during winter and summer. The measured temperatures show a great variability within and across locations. The data can be used to validate models and estimate potential emissions.
Ephraim Erkens, Michael Angelopoulos, Jens Tronicke, Scott R. Dallimore, Dustin Whalen, Julia Boike, and Pier Paul Overduin
EGUsphere, https://doi.org/10.5194/egusphere-2024-1044, https://doi.org/10.5194/egusphere-2024-1044, 2024
Short summary
Short summary
We investigate the depth of subsea permafrost formed by inundation of terrestrial permafrost due to marine transgression around the rapidly disappearing, permafrost-cored Tuktoyaktuk Island (Beaufort Sea, NWT, Canada). We use geoelectrical surveys with floating electrodes to identify the boundary between unfrozen and frozen sediment. Our findings indicate that permafrost thaw depths beneath the seabed can be explained by coastal erosion rates and landscape features before inundation.
Tabea Rettelbach, Ingmar Nitze, Inge Grünberg, Jennika Hammar, Simon Schäffler, Daniel Hein, Matthias Gessner, Tilman Bucher, Jörg Brauchle, Jörg Hartmann, Torsten Sachs, Julia Boike, and Guido Grosse
Earth Syst. Sci. Data Discuss., https://doi.org/10.5194/essd-2023-193, https://doi.org/10.5194/essd-2023-193, 2023
Revised manuscript accepted for ESSD
Short summary
Short summary
Permafrost landscapes in the Arctic are rapidly changing due to climate warming. We here publish aerial images and elevation models with very high spatial detail that help study these landscapes in northwestern Canada and Alaska. The images were collected using the Modular Aerial Camera System (MACS). This dataset has significant implications for understanding permafrost landscape dynamics in response to climate change. It is publicly available for further research.
Sebastian Westermann, Thomas Ingeman-Nielsen, Johanna Scheer, Kristoffer Aalstad, Juditha Aga, Nitin Chaudhary, Bernd Etzelmüller, Simon Filhol, Andreas Kääb, Cas Renette, Louise Steffensen Schmidt, Thomas Vikhamar Schuler, Robin B. Zweigel, Léo Martin, Sarah Morard, Matan Ben-Asher, Michael Angelopoulos, Julia Boike, Brian Groenke, Frederieke Miesner, Jan Nitzbon, Paul Overduin, Simone M. Stuenzi, and Moritz Langer
Geosci. Model Dev., 16, 2607–2647, https://doi.org/10.5194/gmd-16-2607-2023, https://doi.org/10.5194/gmd-16-2607-2023, 2023
Short summary
Short summary
The CryoGrid community model is a new tool for simulating ground temperatures and the water and ice balance in cold regions. It is a modular design, which makes it possible to test different schemes to simulate, for example, permafrost ground in an efficient way. The model contains tools to simulate frozen and unfrozen ground, snow, glaciers, and other massive ice bodies, as well as water bodies.
Martine Lizotte, Bennet Juhls, Atsushi Matsuoka, Philippe Massicotte, Gaëlle Mével, David Obie James Anikina, Sofia Antonova, Guislain Bécu, Marine Béguin, Simon Bélanger, Thomas Bossé-Demers, Lisa Bröder, Flavienne Bruyant, Gwénaëlle Chaillou, Jérôme Comte, Raoul-Marie Couture, Emmanuel Devred, Gabrièle Deslongchamps, Thibaud Dezutter, Miles Dillon, David Doxaran, Aude Flamand, Frank Fell, Joannie Ferland, Marie-Hélène Forget, Michael Fritz, Thomas J. Gordon, Caroline Guilmette, Andrea Hilborn, Rachel Hussherr, Charlotte Irish, Fabien Joux, Lauren Kipp, Audrey Laberge-Carignan, Hugues Lantuit, Edouard Leymarie, Antonio Mannino, Juliette Maury, Paul Overduin, Laurent Oziel, Colin Stedmon, Crystal Thomas, Lucas Tisserand, Jean-Éric Tremblay, Jorien Vonk, Dustin Whalen, and Marcel Babin
Earth Syst. Sci. Data, 15, 1617–1653, https://doi.org/10.5194/essd-15-1617-2023, https://doi.org/10.5194/essd-15-1617-2023, 2023
Short summary
Short summary
Permafrost thaw in the Mackenzie Delta region results in the release of organic matter into the coastal marine environment. What happens to this carbon-rich organic matter as it transits along the fresh to salty aquatic environments is still underdocumented. Four expeditions were conducted from April to September 2019 in the coastal area of the Beaufort Sea to study the fate of organic matter. This paper describes a rich set of data characterizing the composition and sources of organic matter.
Ngai-Ham Chan, Moritz Langer, Bennet Juhls, Tabea Rettelbach, Paul Overduin, Kimberly Huppert, and Jean Braun
Earth Surf. Dynam., 11, 259–285, https://doi.org/10.5194/esurf-11-259-2023, https://doi.org/10.5194/esurf-11-259-2023, 2023
Short summary
Short summary
Arctic river deltas influence how nutrients and soil organic carbon, carried by sediments from the Arctic landscape, are retained or released into the Arctic Ocean. Under climate change, the deltas themselves and their ecosystems are becoming more vulnerable. We build upon previous models to reproduce for the first time an important feature ubiquitous to Arctic deltas and simulate its future under climate warming. This can impact the future of Arctic deltas and the carbon release they moderate.
Simeon Lisovski, Alexandra Runge, Iuliia Shevtsova, Nele Landgraf, Anne Morgenstern, Ronald Reagan Okoth, Matthias Fuchs, Nikolay Lashchinskiy, Carl Stadie, Alison Beamish, Ulrike Herzschuh, Guido Grosse, and Birgit Heim
Earth Syst. Sci. Data Discuss., https://doi.org/10.5194/essd-2023-36, https://doi.org/10.5194/essd-2023-36, 2023
Preprint under review for ESSD
Short summary
Short summary
The Lena Delta is the largest river delta in the Arctic, and represents a biodiversity hotspot. Here, we describe multiple field datasets and a detailed habitat classification map for the Lena Delta. We present context and methods of these openly available datasets and show how they can improve our understanding of the rapidly changing Arctic tundra system.
Mauricio Arboleda-Zapata, Michael Angelopoulos, Pier Paul Overduin, Guido Grosse, Benjamin M. Jones, and Jens Tronicke
The Cryosphere, 16, 4423–4445, https://doi.org/10.5194/tc-16-4423-2022, https://doi.org/10.5194/tc-16-4423-2022, 2022
Short summary
Short summary
We demonstrate how we can reliably estimate the thawed–frozen permafrost interface with its associated uncertainties in subsea permafrost environments using 2D electrical resistivity tomography (ERT) data. In addition, we show how further analyses considering 1D inversion and sensitivity assessments can help quantify and better understand 2D ERT inversion results. Our results illustrate the capabilities of the ERT method to get insights into the development of the subsea permafrost.
Loeka L. Jongejans, Kai Mangelsdorf, Cornelia Karger, Thomas Opel, Sebastian Wetterich, Jérémy Courtin, Hanno Meyer, Alexander I. Kizyakov, Guido Grosse, Andrei G. Shepelev, Igor I. Syromyatnikov, Alexander N. Fedorov, and Jens Strauss
The Cryosphere, 16, 3601–3617, https://doi.org/10.5194/tc-16-3601-2022, https://doi.org/10.5194/tc-16-3601-2022, 2022
Short summary
Short summary
Large parts of Arctic Siberia are underlain by permafrost. Climate warming leads to permafrost thaw. At the Batagay megaslump, permafrost sediments up to ~ 650 kyr old are exposed. We took sediment samples and analysed the organic matter (e.g. plant remains). We found distinct differences in the biomarker distributions between the glacial and interglacial deposits with generally stronger microbial activity during interglacial periods. Further permafrost thaw enhances greenhouse gas emissions.
Jan Nitzbon, Damir Gadylyaev, Steffen Schlüter, John Maximilian Köhne, Guido Grosse, and Julia Boike
The Cryosphere, 16, 3507–3515, https://doi.org/10.5194/tc-16-3507-2022, https://doi.org/10.5194/tc-16-3507-2022, 2022
Short summary
Short summary
The microstructure of permafrost soils contains clues to its formation and its preconditioning to future change. We used X-ray computed tomography (CT) to measure the composition of a permafrost drill core from Siberia. By combining CT with laboratory measurements, we determined the the proportions of pore ice, excess ice, minerals, organic matter, and gas contained in the core at an unprecedented resolution. Our work demonstrates the potential of CT to study permafrost properties and processes.
Matthias Fuchs, Juri Palmtag, Bennet Juhls, Pier Paul Overduin, Guido Grosse, Ahmed Abdelwahab, Michael Bedington, Tina Sanders, Olga Ogneva, Irina V. Fedorova, Nikita S. Zimov, Paul J. Mann, and Jens Strauss
Earth Syst. Sci. Data, 14, 2279–2301, https://doi.org/10.5194/essd-14-2279-2022, https://doi.org/10.5194/essd-14-2279-2022, 2022
Short summary
Short summary
We created digital, high-resolution bathymetry data sets for the Lena Delta and Kolyma Gulf regions in northeastern Siberia. Based on nautical charts, we digitized depth points and isobath lines, which serve as an input for a 50 m bathymetry model. The benefit of this data set is the accurate mapping of near-shore areas as well as the offshore continuation of the main deep river channels. This will improve the estimation of river outflow and the nutrient flux output into the coastal zone.
Charlotte Haugk, Loeka L. Jongejans, Kai Mangelsdorf, Matthias Fuchs, Olga Ogneva, Juri Palmtag, Gesine Mollenhauer, Paul J. Mann, P. Paul Overduin, Guido Grosse, Tina Sanders, Robyn E. Tuerena, Lutz Schirrmeister, Sebastian Wetterich, Alexander Kizyakov, Cornelia Karger, and Jens Strauss
Biogeosciences, 19, 2079–2094, https://doi.org/10.5194/bg-19-2079-2022, https://doi.org/10.5194/bg-19-2079-2022, 2022
Short summary
Short summary
Buried animal and plant remains (carbon) from the last ice age were freeze-locked in permafrost. At an extremely fast eroding permafrost cliff in the Lena Delta (Siberia), we found this formerly frozen carbon well preserved. Our results show that ongoing degradation releases substantial amounts of this carbon, making it available for future carbon emissions. This mobilisation at the studied cliff and also similarly eroding sites bear the potential to affect rivers and oceans negatively.
Stiig Wilkenskjeld, Frederieke Miesner, Paul P. Overduin, Matteo Puglini, and Victor Brovkin
The Cryosphere, 16, 1057–1069, https://doi.org/10.5194/tc-16-1057-2022, https://doi.org/10.5194/tc-16-1057-2022, 2022
Short summary
Short summary
Thawing permafrost releases carbon to the atmosphere, enhancing global warming. Part of the permafrost soils have been flooded by rising sea levels since the last ice age, becoming subsea permafrost (SSPF). The SSPF is less studied than the part on land. In this study we use a global model to obtain rates of thawing of SSPF under different future climate scenarios until the year 3000. After the year 2100 the scenarios strongly diverge, closely connected to the eventual disappearance of sea ice.
David Olefeldt, Mikael Hovemyr, McKenzie A. Kuhn, David Bastviken, Theodore J. Bohn, John Connolly, Patrick Crill, Eugénie S. Euskirchen, Sarah A. Finkelstein, Hélène Genet, Guido Grosse, Lorna I. Harris, Liam Heffernan, Manuel Helbig, Gustaf Hugelius, Ryan Hutchins, Sari Juutinen, Mark J. Lara, Avni Malhotra, Kristen Manies, A. David McGuire, Susan M. Natali, Jonathan A. O'Donnell, Frans-Jan W. Parmentier, Aleksi Räsänen, Christina Schädel, Oliver Sonnentag, Maria Strack, Suzanne E. Tank, Claire Treat, Ruth K. Varner, Tarmo Virtanen, Rebecca K. Warren, and Jennifer D. Watts
Earth Syst. Sci. Data, 13, 5127–5149, https://doi.org/10.5194/essd-13-5127-2021, https://doi.org/10.5194/essd-13-5127-2021, 2021
Short summary
Short summary
Wetlands, lakes, and rivers are important sources of the greenhouse gas methane to the atmosphere. To understand current and future methane emissions from northern regions, we need maps that show the extent and distribution of specific types of wetlands, lakes, and rivers. The Boreal–Arctic Wetland and Lake Dataset (BAWLD) provides maps of five wetland types, seven lake types, and three river types for northern regions and will improve our ability to predict future methane emissions.
Torben Windirsch, Guido Grosse, Mathias Ulrich, Bruce C. Forbes, Mathias Göckede, Juliane Wolter, Marc Macias-Fauria, Johan Olofsson, Nikita Zimov, and Jens Strauss
Biogeosciences Discuss., https://doi.org/10.5194/bg-2021-227, https://doi.org/10.5194/bg-2021-227, 2021
Revised manuscript not accepted
Short summary
Short summary
With global warming, permafrost thaw and associated carbon release are of increasing importance. We examined how large herbivorous animals affect Arctic landscapes and how they might contribute to reduction of these emissions. We show that over a short timespan of roughly 25 years, these animals have already changed the vegetation and landscape. On pastures in a permafrost area in Siberia we found smaller thaw depth and higher carbon content than in surrounding non-pasture areas.
Lydia Stolpmann, Caroline Coch, Anne Morgenstern, Julia Boike, Michael Fritz, Ulrike Herzschuh, Kathleen Stoof-Leichsenring, Yury Dvornikov, Birgit Heim, Josefine Lenz, Amy Larsen, Katey Walter Anthony, Benjamin Jones, Karen Frey, and Guido Grosse
Biogeosciences, 18, 3917–3936, https://doi.org/10.5194/bg-18-3917-2021, https://doi.org/10.5194/bg-18-3917-2021, 2021
Short summary
Short summary
Our new database summarizes DOC concentrations of 2167 water samples from 1833 lakes in permafrost regions across the Arctic to provide insights into linkages between DOC and environment. We found increasing lake DOC concentration with decreasing permafrost extent and higher DOC concentrations in boreal permafrost sites compared to tundra sites. Our study shows that DOC concentration depends on the environmental properties of a lake, especially permafrost extent, ecoregion, and vegetation.
Ines Spangenberg, Pier Paul Overduin, Ellen Damm, Ingeborg Bussmann, Hanno Meyer, Susanne Liebner, Michael Angelopoulos, Boris K. Biskaborn, Mikhail N. Grigoriev, and Guido Grosse
The Cryosphere, 15, 1607–1625, https://doi.org/10.5194/tc-15-1607-2021, https://doi.org/10.5194/tc-15-1607-2021, 2021
Short summary
Short summary
Thermokarst lakes are common on ice-rich permafrost. Many studies have shown that they are sources of methane to the atmosphere. Although they are usually covered by ice, little is known about what happens to methane in winter. We studied how much methane is contained in the ice of a thermokarst lake, a thermokarst lagoon and offshore. Methane concentrations differed strongly, depending on water body type. Microbes can also oxidize methane in ice and lower the concentrations during winter.
Rebecca Rolph, Pier Paul Overduin, Thomas Ravens, Hugues Lantuit, and Moritz Langer
Geosci. Model Dev. Discuss., https://doi.org/10.5194/gmd-2021-28, https://doi.org/10.5194/gmd-2021-28, 2021
Revised manuscript not accepted
Short summary
Short summary
Declining sea ice, larger waves, and increasing air temperatures are contributing to a rapidly eroding Arctic coastline. We simulate water levels using wind speed and direction, which are used with wave height, wave period, and sea surface temperature to drive an erosion model of a partially frozen cliff and beach. This provides a first step to include Arctic erosion in larger-scale earth system models. Simulated cumulative retreat rates agree within the same order of magnitude as observations.
Ingeborg Bussmann, Irina Fedorova, Bennet Juhls, Pier Paul Overduin, and Matthias Winkel
Biogeosciences, 18, 2047–2061, https://doi.org/10.5194/bg-18-2047-2021, https://doi.org/10.5194/bg-18-2047-2021, 2021
Short summary
Short summary
Arctic rivers, lakes, and bays are affected by a warming climate. We measured the amount and consumption of methane in waters from Siberia under ice cover and in open water. In the lake, methane concentrations under ice cover were much higher than in summer, and methane consumption was highest. The ice cover leads to higher methane concentration under ice. In a warmer Arctic, there will be more time with open water when methane is consumed by bacteria, and less methane will escape into the air.
Arthur Monhonval, Sophie Opfergelt, Elisabeth Mauclet, Benoît Pereira, Aubry Vandeuren, Guido Grosse, Lutz Schirrmeister, Matthias Fuchs, Peter Kuhry, and Jens Strauss
Earth Syst. Sci. Data Discuss., https://doi.org/10.5194/essd-2020-359, https://doi.org/10.5194/essd-2020-359, 2020
Preprint withdrawn
Short summary
Short summary
With global warming, ice-rich permafrost soils expose organic carbon to microbial degradation and unlock mineral elements as well. Interactions between mineral elements and organic carbon may enhance or mitigate microbial degradation. Here, we provide a large scale ice-rich permafrost mineral concentrations assessment and estimates of mineral element stocks in those deposits. Si is the most abundant mineral element and Fe and Al are present in the same order of magnitude as organic carbon.
Ingmar Nitze, Sarah W. Cooley, Claude R. Duguay, Benjamin M. Jones, and Guido Grosse
The Cryosphere, 14, 4279–4297, https://doi.org/10.5194/tc-14-4279-2020, https://doi.org/10.5194/tc-14-4279-2020, 2020
Short summary
Short summary
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 breakup.
Torben Windirsch, Guido Grosse, Mathias Ulrich, Lutz Schirrmeister, Alexander N. Fedorov, Pavel Y. Konstantinov, Matthias Fuchs, Loeka L. Jongejans, Juliane Wolter, Thomas Opel, and Jens Strauss
Biogeosciences, 17, 3797–3814, https://doi.org/10.5194/bg-17-3797-2020, https://doi.org/10.5194/bg-17-3797-2020, 2020
Short summary
Short summary
To extend the knowledge on circumpolar deep permafrost carbon storage, we examined two deep permafrost deposit types (Yedoma and alas) in central Yakutia. We found little but partially undecomposed organic carbon as a result of largely changing sedimentation processes. The carbon stock of the examined Yedoma deposits is about 50 % lower than the general Yedoma domain mean, implying a very hetererogeneous Yedoma composition, while the alas is approximately 80 % below the thermokarst deposit mean.
Lutz Schirrmeister, Elisabeth Dietze, Heidrun Matthes, Guido Grosse, Jens Strauss, Sebastian Laboor, Mathias Ulrich, Frank Kienast, and Sebastian Wetterich
E&G Quaternary Sci. J., 69, 33–53, https://doi.org/10.5194/egqsj-69-33-2020, https://doi.org/10.5194/egqsj-69-33-2020, 2020
Short summary
Short summary
Late Pleistocene Yedoma deposits of Siberia and Alaska are prone to degradation with warming temperatures.
Multimodal grain-size distributions of >700 samples indicate varieties of sediment production, transport, and deposition.
These processes were disentangled using robust endmember modeling analysis.
Nine robust grain-size endmembers characterize these deposits.
The data set was finally classified using cluster analysis.
The polygenetic Yedoma origin is proved.
Julia Mitzscherling, Fabian Horn, Maria Winterfeld, Linda Mahler, Jens Kallmeyer, Pier P. Overduin, Lutz Schirrmeister, Matthias Winkel, Mikhail N. Grigoriev, Dirk Wagner, and Susanne Liebner
Biogeosciences, 16, 3941–3958, https://doi.org/10.5194/bg-16-3941-2019, https://doi.org/10.5194/bg-16-3941-2019, 2019
Short summary
Short summary
Permafrost temperatures increased substantially at a global scale, potentially altering microbial assemblages involved in carbon mobilization before permafrost thaws. We used Arctic Shelf submarine permafrost as a natural laboratory to investigate the microbial response to long-term permafrost warming. Our work shows that millennia after permafrost warming by > 10 °C, microbial community composition and population size reflect the paleoenvironment rather than a direct effect through warming.
Thomas Opel, Julian B. Murton, Sebastian Wetterich, Hanno Meyer, Kseniia Ashastina, Frank Günther, Hendrik Grotheer, Gesine Mollenhauer, Petr P. Danilov, Vasily Boeskorov, Grigoriy N. Savvinov, and Lutz Schirrmeister
Clim. Past, 15, 1443–1461, https://doi.org/10.5194/cp-15-1443-2019, https://doi.org/10.5194/cp-15-1443-2019, 2019
Short summary
Short summary
To reconstruct past winter climate, we studied ice wedges at two sites in the Yana Highlands, interior Yakutia (Russia), the most continental region of the Northern Hemisphere. Our ice wedges of the upper ice complex unit of the Batagay megaslump and a river terrace show much more depleted stable-isotope compositions than other study sites in coastal and central Yakutia, reflecting lower winter temperatures and a higher continentality of the study region during Marine Isotope Stages 3 and 1.
Bennet Juhls, Pier Paul Overduin, Jens Hölemann, Martin Hieronymi, Atsushi Matsuoka, Birgit Heim, and Jürgen Fischer
Biogeosciences, 16, 2693–2713, https://doi.org/10.5194/bg-16-2693-2019, https://doi.org/10.5194/bg-16-2693-2019, 2019
Short summary
Short summary
In this article, we present the variability and characteristics of dissolved organic matter at the fluvial–marine transition in the Laptev Sea from a unique dataset collected during 11 Arctic expeditions. We develop a new relationship between dissolved organic carbon (DOC) and coloured dissolved organic matter absorption, which is used to estimate surface water DOC concentration from space. We believe that our findings help current efforts to monitor ongoing changes in the Arctic carbon cycle.
Julia Boike, Jan Nitzbon, Katharina Anders, Mikhail Grigoriev, Dmitry Bolshiyanov, Moritz Langer, Stephan Lange, Niko Bornemann, Anne Morgenstern, Peter Schreiber, Christian Wille, Sarah Chadburn, Isabelle Gouttevin, Eleanor Burke, and Lars Kutzbach
Earth Syst. Sci. Data, 11, 261–299, https://doi.org/10.5194/essd-11-261-2019, https://doi.org/10.5194/essd-11-261-2019, 2019
Short summary
Short summary
Long-term observational data are available from the Samoylov research site in northern Siberia, where meteorological parameters, energy balance, and subsurface observations have been recorded since 1998. This paper presents the temporal data set produced between 2002 and 2017, explaining the instrumentation, calibration, processing, and data quality control. Furthermore, we present a merged dataset of the parameters, which were measured from 1998 onwards.
David Holl, Christian Wille, Torsten Sachs, Peter Schreiber, Benjamin R. K. Runkle, Lutz Beckebanze, Moritz Langer, Julia Boike, Eva-Maria Pfeiffer, Irina Fedorova, Dimitry Y. Bolshianov, Mikhail N. Grigoriev, and Lars Kutzbach
Earth Syst. Sci. Data, 11, 221–240, https://doi.org/10.5194/essd-11-221-2019, https://doi.org/10.5194/essd-11-221-2019, 2019
Short summary
Short summary
We present a multi-annual time series of land–atmosphere carbon dioxide fluxes measured in situ with the eddy covariance technique in the Siberian Arctic. In arctic permafrost regions, climate–carbon feedbacks are amplified. Therefore, increased efforts to better represent these regions in global climate models have been made in recent years. Up to now, the available database of in situ measurements from the Arctic was biased towards Alaska and records from the Eurasian Arctic were scarce.
Loeka L. Jongejans, Jens Strauss, Josefine Lenz, Francien Peterse, Kai Mangelsdorf, Matthias Fuchs, and Guido Grosse
Biogeosciences, 15, 6033–6048, https://doi.org/10.5194/bg-15-6033-2018, https://doi.org/10.5194/bg-15-6033-2018, 2018
Short summary
Short summary
Arctic warming mobilizes belowground organic matter in northern high latitudes. This study focused on the size of organic carbon pools and organic matter quality in ice-rich permafrost on the Baldwin Peninsula, West Alaska. We analyzed biogeochemistry and found that three-quarters of the carbon is stored in degraded permafrost deposits. Nonetheless, using biomarker analyses, we showed that the organic matter in undisturbed yedoma permafrost has a higher potential for decomposition.
Julia Boike, Inge Juszak, Stephan Lange, Sarah Chadburn, Eleanor Burke, Pier Paul Overduin, Kurt Roth, Olaf Ippisch, Niko Bornemann, Lielle Stern, Isabelle Gouttevin, Ernst Hauber, and Sebastian Westermann
Earth Syst. Sci. Data, 10, 355–390, https://doi.org/10.5194/essd-10-355-2018, https://doi.org/10.5194/essd-10-355-2018, 2018
Short summary
Short summary
A 20-year data record from the Bayelva site at Ny-Ålesund, Svalbard, is presented on meteorology, energy balance components, surface and subsurface observations. This paper presents the data set, instrumentation, calibration, processing and data quality control. The data show that mean annual, summer and winter soil temperature data from shallow to deeper depths have been warming over the period of record, indicating the degradation and loss of permafrost at this site.
Matthias Fuchs, Guido Grosse, Jens Strauss, Frank Günther, Mikhail Grigoriev, Georgy M. Maximov, and Gustaf Hugelius
Biogeosciences, 15, 953–971, https://doi.org/10.5194/bg-15-953-2018, https://doi.org/10.5194/bg-15-953-2018, 2018
Short summary
Short summary
Our paper investigates soil organic carbon and nitrogen in permafrost soils on Sobo-Sise Island and Bykovsky Peninsula in the north of eastern Siberia. We collected and analysed permafrost soil cores and upscaled carbon and nitrogen stocks to landscape level. We found large amounts of carbon and nitrogen stored in these frozen soils, reconstructed sedimentation rates and estimated the potential increase in organic carbon availability if permafrost continues to thaw and active layer deepens.
Simon Zwieback, Steven V. Kokelj, Frank Günther, Julia Boike, Guido Grosse, and Irena Hajnsek
The Cryosphere, 12, 549–564, https://doi.org/10.5194/tc-12-549-2018, https://doi.org/10.5194/tc-12-549-2018, 2018
Short summary
Short summary
We analyse elevation losses at thaw slumps, at which icy sediments are exposed. As ice requires a large amount of energy to melt, one would expect that mass wasting is governed by the available energy. However, we observe very little mass wasting in June, despite the ample energy supply. Also, in summer, mass wasting is not always energy limited. This highlights the importance of other processes, such as the formation of a protective veneer, in shaping mass wasting at sub-seasonal scales.
Sina Muster, Kurt Roth, Moritz Langer, Stephan Lange, Fabio Cresto Aleina, Annett Bartsch, Anne Morgenstern, Guido Grosse, Benjamin Jones, A. Britta K. Sannel, Ylva Sjöberg, Frank Günther, Christian Andresen, Alexandra Veremeeva, Prajna R. Lindgren, Frédéric Bouchard, Mark J. Lara, Daniel Fortier, Simon Charbonneau, Tarmo A. Virtanen, Gustaf Hugelius, Juri Palmtag, Matthias B. Siewert, William J. Riley, Charles D. Koven, and Julia Boike
Earth Syst. Sci. Data, 9, 317–348, https://doi.org/10.5194/essd-9-317-2017, https://doi.org/10.5194/essd-9-317-2017, 2017
Short summary
Short summary
Waterbodies are abundant in Arctic permafrost lowlands. Most waterbodies are ponds with a surface area smaller than 100 x 100 m. The Permafrost Region Pond and Lake Database (PeRL) for the first time maps ponds as small as 10 x 10 m. PeRL maps can be used to document changes both by comparing them to historical and future imagery. The distribution of waterbodies in the Arctic is important to know in order to manage resources in the Arctic and to improve climate predictions in the Arctic.
Lutz Schirrmeister, Georg Schwamborn, Pier Paul Overduin, Jens Strauss, Margret C. Fuchs, Mikhail Grigoriev, Irina Yakshina, Janet Rethemeyer, Elisabeth Dietze, and Sebastian Wetterich
Biogeosciences, 14, 1261–1283, https://doi.org/10.5194/bg-14-1261-2017, https://doi.org/10.5194/bg-14-1261-2017, 2017
Short summary
Short summary
We investigate late Pleistocene permafrost at the Buor Khaya Peninsula (Laptev Sea, Siberia) for cryolithological, geochemical, and geochronological parameters. The sequences were composed of ice-oversaturated silts and fine-grained sands with 0.2 to 24 wt% of organic matter. The deposition was between 54.1 and 9.7 kyr BP. Due to coastal erosion, the biogeochemical signature of the deposits represents the terrestrial end-member, and is related to organic matter deposited in the marine realm.
Heike Hildegard Zimmermann, Elena Raschke, Laura Saskia Epp, Kathleen Rosmarie Stoof-Leichsenring, Georg Schwamborn, Lutz Schirrmeister, Pier Paul Overduin, and Ulrike Herzschuh
Biogeosciences, 14, 575–596, https://doi.org/10.5194/bg-14-575-2017, https://doi.org/10.5194/bg-14-575-2017, 2017
Short summary
Short summary
Organic matter stored in permafrost will start decomposing due to climate warming. To better understand its composition in ice-rich Yedoma, we analyzed ancient sedimentary DNA, pollen and non-pollen palynomorphs throughout an 18.9 m long permafrost core. The combination of both proxies allow an interpretation both of regional floristic changes and of the local environmental conditions at the time of deposition.
Benjamin M. Jones, Carson A. Baughman, Vladimir E. Romanovsky, Andrew D. Parsekian, Esther L. Babcock, Eva Stephani, Miriam C. Jones, Guido Grosse, and Edward E. Berg
The Cryosphere, 10, 2673–2692, https://doi.org/10.5194/tc-10-2673-2016, https://doi.org/10.5194/tc-10-2673-2016, 2016
Short summary
Short summary
We combined field data collection with remote sensing data to document the presence and rapid degradation of permafrost in south-central Alaska during 1950–present. Ground temperature measurements confirmed permafrost presence in the region, but remotely sensed images showed that permafrost plateau extent decreased by 60 % since 1950. Better understanding these vulnerable permafrost deposits is important for predicting future permafrost extent across all permafrost regions that are warming.
Pier Paul Overduin, Sebastian Wetterich, Frank Günther, Mikhail N. Grigoriev, Guido Grosse, Lutz Schirrmeister, Hans-Wolfgang Hubberten, and Aleksandr Makarov
The Cryosphere, 10, 1449–1462, https://doi.org/10.5194/tc-10-1449-2016, https://doi.org/10.5194/tc-10-1449-2016, 2016
Short summary
Short summary
How fast does permafrost warm up and thaw after it is covered by the sea? Ice-rich permafrost in the Laptev Sea, Siberia, is rapidly eroded by warm air and waves. We used a floating electrical technique to measure the depth of permafrost thaw below the sea, and compared it to 60 years of coastline retreat and permafrost depths from drilling 30 years ago. Thaw is rapid right after flooding of the land and slows over time. The depth of permafrost is related to how fast the coast retreats.
P. R. Lindgren, G. Grosse, K. M. Walter Anthony, and F. J. Meyer
Biogeosciences, 13, 27–44, https://doi.org/10.5194/bg-13-27-2016, https://doi.org/10.5194/bg-13-27-2016, 2016
Short summary
Short summary
We mapped and characterized methane ebullition bubbles trapped in lake ice, and estimated whole-lake methane emission using high-resolution aerial images of a lake acquired following freeze-up. We identified the location and relative sizes of high- and low-flux seepage zones within the lake. A large number of seeps showed spatiotemporal stability over our study period. Our approach is applicable to other regions to improve the estimation of methane emission from lakes at the regional scale.
J. Boike, C. Georgi, G. Kirilin, S. Muster, K. Abramova, I. Fedorova, A. Chetverova, M. Grigoriev, N. Bornemann, and M. Langer
Biogeosciences, 12, 5941–5965, https://doi.org/10.5194/bg-12-5941-2015, https://doi.org/10.5194/bg-12-5941-2015, 2015
Short summary
Short summary
We show that lakes in northern Siberia are very efficient with respect to energy absorption and mixing using measurements as well as numerical modeling. We show that (i) the lakes receive substantial energy for warming from net short-wave radiation; (ii) convective mixing occurs beneath the ice cover, follow beneath the ice cover, following ice break-up, summer, and fall (iii) modeling suggests that the annual mean net heat flux across the bottom sediment boundary is approximately zero.
J. K. Heslop, K. M. Walter Anthony, A. Sepulveda-Jauregui, K. Martinez-Cruz, A. Bondurant, G. Grosse, and M. C. Jones
Biogeosciences, 12, 4317–4331, https://doi.org/10.5194/bg-12-4317-2015, https://doi.org/10.5194/bg-12-4317-2015, 2015
Short summary
Short summary
The relative magnitude of thermokarst lake CH4 production in surface sediments vs. deeper-thawed permafrost is not well understood. We assessed CH4 production potentials from a lake sediment core and adjacent permafrost tunnel in interior Alaska. CH4 production was highest in the organic-rich surface lake sediments and recently thawed permafrost at the bottom of the talik, implying CH4 production is highly variable and that both modern and ancient OM are important to lake CH4 production.
T. Schneider von Deimling, G. Grosse, J. Strauss, L. Schirrmeister, A. Morgenstern, S. Schaphoff, M. Meinshausen, and J. Boike
Biogeosciences, 12, 3469–3488, https://doi.org/10.5194/bg-12-3469-2015, https://doi.org/10.5194/bg-12-3469-2015, 2015
Short summary
Short summary
We have modelled the carbon release from thawing permafrost soils under various scenarios of future warming. Our results suggests that up to about 140Pg of carbon could be released under strong warming by end of the century. We have shown that abrupt thaw processes under thermokarst lakes can unlock large amounts of perennially frozen carbon stored in deep deposits (which extend many metres into the soil).
F. Günther, P. P. Overduin, I. A. Yakshina, T. Opel, A. V. Baranskaya, and M. N. Grigoriev
The Cryosphere, 9, 151–178, https://doi.org/10.5194/tc-9-151-2015, https://doi.org/10.5194/tc-9-151-2015, 2015
Short summary
Short summary
Coastal erosion rates at Muostakh Island (eastern Siberian Arctic) have doubled, based on remotely sensed observations of land loss, and therefore the island will disappear prematurely. Based on analyses of seasonal variability of permafrost thaw, thermo-erosion increases by 1.2m per year when summer temperatures rise by 1°C. Due to rapid permafrost thaw, the land surface is subsiding up to 11cm per year, based on comparison of elevation changes and active layer thaw depth.
I. Fedorova, A. Chetverova, D. Bolshiyanov, A. Makarov, J. Boike, B. Heim, A. Morgenstern, P. P. Overduin, C. Wegner, V. Kashina, A. Eulenburg, E. Dobrotina, and I. Sidorina
Biogeosciences, 12, 345–363, https://doi.org/10.5194/bg-12-345-2015, https://doi.org/10.5194/bg-12-345-2015, 2015
C. D. Arp, M. S. Whitman, B. M. Jones, G. Grosse, B. V. Gaglioti, and K. C. Heim
Biogeosciences, 12, 29–47, https://doi.org/10.5194/bg-12-29-2015, https://doi.org/10.5194/bg-12-29-2015, 2015
Short summary
Short summary
Beaded streams have deep elliptical pools connected by narrow runs that we show are common landforms in the continuous permafrost zone. These fluvial systems often initiate from lakes and occur predictably in headwater portions of moderately sloping watersheds. Snow capture along stream courses reduces ice thickness allowing thawed sediment to persist under most pools. Interpool thermal variability and hydrologic regimes provide important aquatic habitat and connectivity in Arctic landscapes.
G. Hugelius, J. Strauss, S. Zubrzycki, J. W. Harden, E. A. G. Schuur, C.-L. Ping, L. Schirrmeister, G. Grosse, G. J. Michaelson, C. D. Koven, J. A. O'Donnell, B. Elberling, U. Mishra, P. Camill, Z. Yu, J. Palmtag, and P. Kuhry
Biogeosciences, 11, 6573–6593, https://doi.org/10.5194/bg-11-6573-2014, https://doi.org/10.5194/bg-11-6573-2014, 2014
Short summary
Short summary
This study provides an updated estimate of organic carbon stored in the northern permafrost region. The study includes estimates for carbon in soils (0 to 3 m depth) and deeper sediments in river deltas and the Yedoma region. We find that field data is still scarce from many regions. Total estimated carbon storage is ~1300 Pg with an uncertainty range of between 1100 and 1500 Pg. Around 800 Pg carbon is perennially frozen, equivalent to all carbon dioxide currently in the Earth's atmosphere.
B. Heim, E. Abramova, R. Doerffer, F. Günther, J. Hölemann, A. Kraberg, H. Lantuit, A. Loginova, F. Martynov, P. P. Overduin, and C. Wegner
Biogeosciences, 11, 4191–4210, https://doi.org/10.5194/bg-11-4191-2014, https://doi.org/10.5194/bg-11-4191-2014, 2014
L. Liu, K. Schaefer, A. Gusmeroli, G. Grosse, B. M. Jones, T. Zhang, A. D. Parsekian, and H. A. Zebker
The Cryosphere, 8, 815–826, https://doi.org/10.5194/tc-8-815-2014, https://doi.org/10.5194/tc-8-815-2014, 2014
G. Hugelius, J. G. Bockheim, P. Camill, B. Elberling, G. Grosse, J. W. Harden, K. Johnson, T. Jorgenson, C. D. Koven, P. Kuhry, G. Michaelson, U. Mishra, J. Palmtag, C.-L. Ping, J. O'Donnell, L. Schirrmeister, E. A. G. Schuur, Y. Sheng, L. C. Smith, J. Strauss, and Z. Yu
Earth Syst. Sci. Data, 5, 393–402, https://doi.org/10.5194/essd-5-393-2013, https://doi.org/10.5194/essd-5-393-2013, 2013
M. Engram, K. W. Anthony, F. J. Meyer, and G. Grosse
The Cryosphere, 7, 1741–1752, https://doi.org/10.5194/tc-7-1741-2013, https://doi.org/10.5194/tc-7-1741-2013, 2013
S. Zubrzycki, L. Kutzbach, G. Grosse, A. Desyatkin, and E.-M. Pfeiffer
Biogeosciences, 10, 3507–3524, https://doi.org/10.5194/bg-10-3507-2013, https://doi.org/10.5194/bg-10-3507-2013, 2013
A. Gusmeroli and G. Grosse
The Cryosphere, 6, 1435–1443, https://doi.org/10.5194/tc-6-1435-2012, https://doi.org/10.5194/tc-6-1435-2012, 2012
Related subject area
Earth System Science/Response to Global Change: Evolution of System Earth
Technical note: Low meteorological influence found in 2019 Amazonia fires
Understanding tropical forest abiotic response to hurricanes using experimental manipulations, field observations, and satellite data
Towards a global understanding of vegetation–climate dynamics at multiple timescales
Evaluating and improving the Community Land Model's sensitivity to land cover
The extant shore platform stromatolite (SPS) facies association: a glimpse into the Archean?
Historic carbon burial spike in an Amazon floodplain lake linked to riparian deforestation near Santarém, Brazil
Nonlinear thermal and moisture response of ice-wedge polygons to permafrost disturbance increases heterogeneity of high Arctic wetland
Global assessment of Vegetation Index and Phenology Lab (VIP) and Global Inventory Modeling and Mapping Studies (GIMMS) version 3 products
Seasonal variation in grass water content estimated from proximal sensing and MODIS time series in a Mediterranean Fluxnet site
A red tide alga grown under ocean acidification upregulates its tolerance to lower pH by increasing its photophysiological functions
High-latitude cooling associated with landscape changes from North American boreal forest fires
Life-cycle evaluation of nitrogen-use in rice-farming systems: implications for economically-optimal nitrogen rates
Tephrostratigraphy and tephrochronology of lakes Ohrid and Prespa, Balkans
Douglas I. Kelley, Chantelle Burton, Chris Huntingford, Megan A. J. Brown, Rhys Whitley, and Ning Dong
Biogeosciences, 18, 787–804, https://doi.org/10.5194/bg-18-787-2021, https://doi.org/10.5194/bg-18-787-2021, 2021
Short summary
Short summary
Initial evidence suggests human ignitions or landscape changes caused most Amazon fires during August 2019. However, confirmation is needed that meteorological conditions did not have a substantial role. Assessing the influence of historical weather on burning in an uncertainty framework, we find that 2019 meteorological conditions alone should have resulted in much less fire than observed. We conclude socio-economic factors likely had a strong role in the high recorded 2019 fire activity.
Ashley E. Van Beusekom, Grizelle González, Sarah Stankavich, Jess K. Zimmerman, and Alonso Ramírez
Biogeosciences, 17, 3149–3163, https://doi.org/10.5194/bg-17-3149-2020, https://doi.org/10.5194/bg-17-3149-2020, 2020
Short summary
Short summary
This study looks at forest abiotic responses to canopy openness and debris deposition that follow a hurricane. We find that recovery to full canopy may take over half a decade and that recovery of humidity, soil moisture, and leaf saturation under the canopy is not monotonic and may temporarily look recovered before the response is over. Furthermore, we find that satellite data show a quicker recovery than field data, necessitating caution when looking at responses to hurricanes with satellites.
Nora Linscheid, Lina M. Estupinan-Suarez, Alexander Brenning, Nuno Carvalhais, Felix Cremer, Fabian Gans, Anja Rammig, Markus Reichstein, Carlos A. Sierra, and Miguel D. Mahecha
Biogeosciences, 17, 945–962, https://doi.org/10.5194/bg-17-945-2020, https://doi.org/10.5194/bg-17-945-2020, 2020
Short summary
Short summary
Vegetation typically responds to variation in temperature and rainfall within days. Yet seasonal changes in meteorological conditions, as well as decadal climate variability, additionally shape the state of ecosystems. It remains unclear how vegetation responds to climate variability on these different timescales. We find that the vegetation response to climate variability depends on the timescale considered. This scale dependency should be considered for modeling land–atmosphere interactions.
Ronny Meier, Edouard L. Davin, Quentin Lejeune, Mathias Hauser, Yan Li, Brecht Martens, Natalie M. Schultz, Shannon Sterling, and Wim Thiery
Biogeosciences, 15, 4731–4757, https://doi.org/10.5194/bg-15-4731-2018, https://doi.org/10.5194/bg-15-4731-2018, 2018
Short summary
Short summary
Deforestation not only releases carbon dioxide to the atmosphere but also affects local climatic conditions by altering energy fluxes at the land surface and thereby the local temperature. Here, we evaluate the local impact of deforestation in a widely used land surface model. We find that the model reproduces the daytime warming effect of deforestation well. On the other hand, the warmer temperatures observed during night in forests are not present in this model.
Alan Smith, Andrew Cooper, Saumitra Misra, Vishal Bharuth, Lisa Guastella, and Riaan Botes
Biogeosciences, 15, 2189–2203, https://doi.org/10.5194/bg-15-2189-2018, https://doi.org/10.5194/bg-15-2189-2018, 2018
Short summary
Short summary
Growing shore-platform stromatolites are increasingly found on modern rocky coasts. Stromatolites are very similar to Archean and Proterozoic stromatolites. A study of modern stromatolites may shed light on the conditions that existed on the early Earth and other planets and possibly provide information on how life began.
Luciana M. Sanders, Kathryn Taffs, Debra Stokes, Christian J. Sanders, Alex Enrich-Prast, Leonardo Amora-Nogueira, and Humberto Marotta
Biogeosciences, 15, 447–455, https://doi.org/10.5194/bg-15-447-2018, https://doi.org/10.5194/bg-15-447-2018, 2018
Short summary
Short summary
The Amazon rainforest produce large quantities of carbon, a portion of which is deposited in floodplain lakes. This research shows a potentially important spatial dependence of the carbon deposition in the Amazon lacustrine sediments in relation to deforestation rates in the catchment. The findings presented here highlight the effects of abrupt and temporary events in which some of the biomass released by the deforestation reach the depositional environments in the Amazon floodplains.
Etienne Godin, Daniel Fortier, and Esther Lévesque
Biogeosciences, 13, 1439–1452, https://doi.org/10.5194/bg-13-1439-2016, https://doi.org/10.5194/bg-13-1439-2016, 2016
Short summary
Short summary
Bowl-shaped ice-wedge polygons in permafrost regions can retain snowmelt water and moisture in their center. On Bylot Island (NU, CA), a rapidly developing thermal erosion gully eroded the polygons' ridges, impacting the polygon centers' ground moisture and temperature, plant cover and species. An intact polygon was homogeneous in its center for the aforementioned elements, whereas eroded polygons had a varying response following the breach, with heterogeneity as their new equilibrium state.
M. Marshall, E. Okuto, Y. Kang, E. Opiyo, and M. Ahmed
Biogeosciences, 13, 625–639, https://doi.org/10.5194/bg-13-625-2016, https://doi.org/10.5194/bg-13-625-2016, 2016
Short summary
Short summary
We compared two new Earth observation based long-term global vegetation index products used in global change research (Global Inventory Modeling and Mapping Studies and Vegetation Index and Phenology Lab- VIP version 3). The two products showed a high level of consistency throughout the primary growing season and were less consistent during green-up and brown-down that impacted trends in phenology. VIP was generally higher and more variable leading to poorer correlations with in situ data
G. Mendiguren, M. Pilar Martín, H. Nieto, J. Pacheco-Labrador, and S. Jurdao
Biogeosciences, 12, 5523–5535, https://doi.org/10.5194/bg-12-5523-2015, https://doi.org/10.5194/bg-12-5523-2015, 2015
S. Chen, J. Beardall, and K. Gao
Biogeosciences, 11, 4829–4837, https://doi.org/10.5194/bg-11-4829-2014, https://doi.org/10.5194/bg-11-4829-2014, 2014
B. M. Rogers, J. T. Randerson, and G. B. Bonan
Biogeosciences, 10, 699–718, https://doi.org/10.5194/bg-10-699-2013, https://doi.org/10.5194/bg-10-699-2013, 2013
Y. Xia and X. Yan
Biogeosciences, 8, 3159–3168, https://doi.org/10.5194/bg-8-3159-2011, https://doi.org/10.5194/bg-8-3159-2011, 2011
R. Sulpizio, G. Zanchetta, M. D'Orazio, H. Vogel, and B. Wagner
Biogeosciences, 7, 3273–3288, https://doi.org/10.5194/bg-7-3273-2010, https://doi.org/10.5194/bg-7-3273-2010, 2010
Cited articles
AMAP: Snow, Water, Ice and Permafrost in the Arctic (SWIPA): Climate Change and the Cryosphere, Arctic Monitoring and Assessment Programme (AMAP), Oslo, Norway, available at: www.amap.no, 2011.
Are, F. E.: The reworking of shorelines in the permafrost zone, in: Proceedings of the Second International Conference on Permafrost, Yakutsk, USSR, July 1973, USSR Contribution, US National Academy of Sciences, Washington, DC, 59–62, 1978.
Are, F. E.: Thermal abrasion of sea coasts (part 1), Polar Geogr. Geol., 12, 1–86, https://doi.org/10.1080/10889378809377343, from: Termoabraziya morskikh beregov, Moscow, Nauka, 1980, 158 pp., 1988a.
Are, F. E.: Thermal abrasion of sea coasts (part 2), Polar Geogr. Geol., 12, 87–157, https://doi.org/10.1080/10889378809377352, from: Termoabraziya morskikh beregov, Moscow, Nauka, 1980, 158 pp., 1988b.
Are, F. E.: The role of coastal retreat for sedimentation in the Laptev Sea, in: Land-Ocean Systems in the Siberian Arctic, edited by: Kassens, H., Bauch, H. A., Dmitrenko, I. A., Eicken, H., Hubberten, H.-W., Melles, M., Thiede, J., and Timokohov, L. A., Springer, Berlin Heidelberg, 287–295, 1999.
Are, F. E.: Razrushenie beregov arkticheskikh primorskikh nizmennostei (Coastal erosion of the Arctic lowlands), Academic publishing house "Geo", Novosibirsk, 2012.
Are, F. E., Grigoriev, M. N., Hubberten, H.-W., Rachold, V., Razumov, S. O., and Schneider, W.: Coastal erosion studies in the Laptev Sea, in: Russian-German Cooperation System Laptev Sea: The Expedition Lena 1999, edited by: Rachold, V., vol. 354, Reports on Polar and Marine Research, Alfred Wegener Institute, available at: http://hdl.handle.net/10013/epic.10357, chap. 4.3, 65–74, 2000.
Are, F., Grigoriev, M. N., Hubberten, H.-W., Rachold, V., Razumov, S. O., and Schneider, W.: Comparative shoreface evolution along the Laptev Sea coast, Polarforschung, 70, 135–150, available at: http://hdl.handle.net/10013/epic.29866, 2002.
Are, F. E., Grigoriev, M. N., Hubberten, H.-W., and Rachold, V.: Using thermoterrace dimensions to calculate the coastal erosion rate, Geo-Mar. Lett., 25, 121–126, https://doi.org/10.1007/s00367-004-0193-y, 2005.
Are, F. E., Reimnitz, E., Grigoriev, M. N., Hubberten, H.-W., and Rachold, V.: The influence of cryogenic processes on the erosional arctic shoreface, J. Coast. Res., 24, 110–121, https://doi.org/10.2112/05-0573.1, 2008.
Asplin, M. G., Galley, R., Barber, D. G., and Prinsenberg, S.: Fracture of summer perennial sea ice by ocean swell as a result of Arctic storms, J. Geophys. Res., 117, C06025, https://doi.org/10.1029/2011JC007221, 2012.
Benner, R., Benitez-Nelson, B., Kaiser, K., and Amon, R. M. W.: Export of young terrigenous dissolved organic carbon from rivers to the Arctic Ocean, Geophys. Res. Lett., 31, L05305, https://doi.org/10.1029/2003GL019251, 2004.
Boike, J., Kattenstroth, B., Abramova, K., Bornemann, N., Chetverova, A., Fedorova, I., Fröb, K., Grigoriev, M., Grüber, M., Kutzbach, L., Langer, M., Minke, M., Muster, S., Piel, K., Pfeiffer, E.-M., Stoof, G., Westermann, S., Wischnewski, K., Wille, C., and Hubberten, H.-W.: Baseline characteristics of climate, permafrost, and land cover from a new permafrost observatory in the Lena River Delta, Siberia (1998–2011), Biogeosciences, 10, 2105–2128, https://doi.org/10.5194/bg-10-2105-2013, 2012.
Brown, J., Jorgenson, M. T., Smith, O. P., and Lee, W.: Long-term rates of erosion and carbon input, Elson Lagoon, Barrow, Alaska, in: Permafrost: Proceedings of the 8th International Conference on Permafrost, edited by: Phillips, M., Springman, S. M., and Arenson, L. U., the Netherlands: AA Balkema Publishers, 101–106, 2003.
Charkin, A. N., Dudarev, O. V., Semiletov, I. P., Kruhmalev, A. V., Vonk, J. E., Sánchez-García, L., Karlsson, E., and Gustafsson, Ö.: Seasonal and interannual variability of sedimentation and organic matter distribution in the Buor-Khaya Gulf: the primary recipient of input from Lena River and coastal erosion in the southeast Laptev Sea, Biogeosciences, 8, 2581–2594, https://doi.org/10.5194/bg-8-2581-2011, 2011.
Comiso, J. C., Parkinson, C. L., Gersten, R., and Stock, L.: Accelerated decline in the Arctic sea ice cover, Geophys. Res. Lett., 35, L01703, https://doi.org/10.1029/2007GL031972, 2008.
Dmitrenko, I. A., Kirillov, S. A., Tremblay, L. B., Kassens, H., Anisimov, O. A., Lavrov, S. A., Razumov, S. O., and Grigoriev, M. N.: Recent changes in shelf hydrography in the Siberian Arctic: potential for subsea permafrost instability, J. Geophys. Res., 116, C10027, https://doi.org/10.1029/2011JC007218, 2011.
Drachev, S. S., Savostin, L. A., Groshev, V. G., and Bruni, I. E.: Structure and geology of the continental shelf of the Laptev Sea, Eastern Russian Arctic, Tectonophysics, 298, 357–393, https://doi.org/10.1016/S0040-1951(98)00159-0, 1998.
Dunaev, N. N. and Nikiforov, S. L.: Shelf i berega arkticheskikh morei (Shelf and coasts of arctic seas), in: Geoekologiya shelfa i beregov morei Rossii (Geoecology of Shelf and Coasts of Russian Seas), edited by: Aibulatov, N. A., Noosphera, Moscow, chap. 2, 27–242, 2001.
Dupeyrat, L., Costard, F., Randriamazaoro, R., Gailhardis, E., Gautier, E., and Fedorov, A.: Effects of ice content on the thermal erosion of permafrost: implications for coastal and fluvial erosion, Permafrost Periglac., 22, 179–187, https://doi.org/10.1002/ppp.722, 2011.
Ehlers, M., Klonus, S., Åstrand, P., and Rosso, P.: Multi-sensor image fusion for pansharpening in remote sensing, International J. Image Data Fus., 1, 25–45, https://doi.org/10.1080/19479830903561985, 2010.
Forbes, D. L.: State of the Arctic Coast 2010 – Scientific Review and Outlook, International Arctic Science Committee, Land-Ocean Interactions in the Coastal Zone, Arctic Monitoring and Assessment Programme, International Permafrost Association, Helmholtz-Zentrum, Geesthacht, Germany, available at: http://arcticcoasts.org, 2011.
Fraser, C. S. and Ravanbakhsh, M.: Georeferencing accuracy of GeoEye-1 imagery, Photogramm. Eng. Rem. S., 75, 634–638, 2009.
Fritz, M., Wetterich, S., Meyer, H., Schirrmeister, L., Lantuit, H., and Pollard, W. H.: Origin and characteristics of massive ground ice on Herschel Island (western Canadian Arctic) as revealed by stable water isotope and hydrochemical signatures, Permafrost Periglac., 22, 26–38, https://doi.org/10.1002/ppp.714, 2011.
Gavrilov, A. V., Romanovskii, N. N., and Hubberten, H.-W.: Paleogeograficheskii scenarii poslelednikovoi transgressii na shelfe Morya Laptevykh (Paleogeographic scenario of the postglacial transgression on the Laptev Sea shelf), Kriosfera Zemli (Earth's Cryosphere), 10, 39–50, available at: http://www.izdatgeo.ru/pdf/krio/2006-1/39.pdf, 2006.
Grigoriev, M. N.: Periglacial studies around Cape Mamontov Klyk – Studies of coastal dynamics and subsea permafrost, in: Russian–German Cooperation System Laptev Sea: The Expedition Lena–Anabar 2003, edited by: Schirrmeister, L., vol. 489, Reports on Polar and Marine Research, Alfred Wegener Institute, available at: http://hdl.handle.net/10013/epic.10494, chap. 4.7, 139–150, 2004.
Grigoriev, M. N.: Kriomorphogenez i litodinamika pribrezhno-shelfovoi zony morei Vostochnoi Sibiri (Cryomorhogenesis and lithodynamics of the East Siberian near-shore shelf zone), Habilitation thesis, SB RAS Permafrost Institute, Yakutsk, 2008.
Grigoriev, M. N. and Rachold, V.: The degradation of coastal permafrost and the organic carbon balance of the Laptev and East Siberian Seas, in: Permafrost: Proceedings of the 8th International Conference on Permafrost, edited by: Phillips, M. and Springman, S.M. and Arenson, L.U., the Netherlands: AA Balkema Publishers, 319–324, 2003.
Grigoriev, M. N., Are, F. E., Hubberten, H.-W., Rachold, V., Razumov, S. O., and Schneider, W.: Onshore coastal studies – coastal dynamics at key sites of the New Siberian Islands, Dmitry Laptev Strait, and Buor Khaya Bay, in: Russian–German Cooperation System Laptev Sea: The Expedition Lena 2002, edited by: Grigoriev, M. N., Rachold, V., Bolshiyanov, D. Y., Pfeiffer, E.-M., Schirrmeister, L., Wagner, D., and Hubberten, H.-W., vol. 466, Reports on Polar and Marine Research, Alfred Wegener Institute, available at: http://hdl.handle.net/10013/epic.10471, chap. 5.3.3, 326–329, 2003.
Grigoriev, M. N., Rachold, V., Schirrmeister, L., and Hubberten, H.-W.: Organic carbon input to the Arctic Seas through coastal erosion, in: The Organic Carbon Cycle in the Arctic Ocean: Present and Past, edited by: Stein, R. and Macdonald, R. W., Springer, Berlin, chap. 2.3, 37–65, 2004.
Grigoriev, M. N., Razumov, S. O., Kunitzky, V. V., and Spektor, V. B.: Dinamika Beregov Vostochnykh Arkticheskikh Morei Rossii: Osnovnye Faktory, Zakonomernosti i Tendencii (Dynamics of the Russian East Arctic Sea coast: major factors, regularities and tendencies), Kriosfera Zemli (Earth's Cryosphere), 10 (4), 74–94, available at: http://www.izdatgeo.ru/pdf/krio/2006-4/74.pdf, 2006.
Grigoriev, M. N., Kunitsky, V. V., Chzhan, R. V., and Shepelev, V. V.: On the variation in geocryological, landscape and hydrological conditions in the Arctic zone of East Siberia in connection with climate warming, Geogr. Natur. Resour., 30, 101–106, https://doi.org/10.1016/j.gnr.2009.06.002, 2009.
Grosse, G., Schirrmeister, L., Kunitsky, V. V., and Hubberten, H.-W.: The use of CORONA images in remote sensing of periglacial geomorphology: an illustration from the NE Siberian coast, Permafrost Periglac., 16, 163–172, https://doi.org/10.1002/ppp.509, 2005.
Grosse, G., Schirrmeister, L., and Malthus, T. J.: Application of Landsat-7 satellite data and a DEM for the quantification of thermokarst-affected terrain types in the periglacial Lena–Anabar coastal lowland, Polar Res., 25, 51–67, https://doi.org/10.1111/j.1751-8369.2006.tb00150.x, 2006.
Grosse, G., Romanovsky, V., Jorgenson, T., Walter Anthony, K. M., Brown, J., and Overduin, P. P.: Vulnerability and feedbacks of permafrost to climate change, Eos Trans. AGU, 92, 73–74, https://doi.org/10.1029/2011EO090001, 2011.
Günther, F., Ulrich, M., Morgenstern, A., and Schirrmeister, L.: Planimetric and volumetric thermokarst change detection on ice rich permafrost, using remote sensing and field data, in: Abstracts from the Third European Conference on Permafrost, edited by: Mertes, J. R., Christiansen, H. H., and Etzelmüller, B., The University Centre in Svalbard, available at: http://hdl.handle.net/10013/epic.35490, 2010.
Günther, F., Overduin, P. P., and Sandakov, A. V.: Topographical surveys for coastal dynamics studies, in: Russian–German Cooperation System Laptev Sea: The Expedition Eastern Laptev Sea – Buor Khaya Peninsula 2010, edited by: Wetterich, S., Overduin, P. P., and Grigoriev, M. N., vol. 629, Reports on Polar and Marine Research, Alfred-Wegener-Institute, chap. 4, 17–34, available at: http://hdl.handle.net/10013/epic.37743, 2011.
Günther, F., Overduin, P. P., Sandakov, A. V., Grosse, G., and Grigoriev, M. N.: Thermo-erosion along the Yedoma Coast of the Buor Khaya Peninsula, Laptev Sea, East Siberia, in: Proceedings of the Tenth International Conference on Permafrost, Salekhard, Yamal-Nenets Autonomous District, Russia, June 25–29, edited by: Hinkel, K. M., vol. 1, International Contributions, available at: http://epic.awi.de/30828/, 137–142, 2012.
Hellmann, L., Tegel, W., Eggertsson, Ó., Schweingruber, F. H., Blanchette, R., Kirdyanov, A., Gärtner, H., Büntgen, U.: Tracing the origin of Arctic driftwood, J. Geophys. Res.-Biogeosciences, 118, 68–76, https://doi.org/10.1002/jgrg.20022, 2013.
Hoque, M. A. and Pollard, W. H.: Arctic coastal retreat through block failure, Can. Geotechn. J., 46, 1103–1115, https://doi.org/10.1139/T09-058, 2009.
Imaeva, L. P., Kozmin, B. M., Sergeyenko, A. I., Belolyubskii, I. N., and Siegert, C.: Noveyshie struktury, stratigrafiya kvartera i sovremennaya geodinamika territorii Arkticheskogo sektora probrezhno-shelfovoi zony Severnogo Verkhoyana (Severo-vostok Yakutii) – (Modern structures, quaternary stratigraphy and recent geodynamics in the Arctic sector of the Northern Verkhoyan coastal shelf zone (North of East Yakutia)), Bulletin of the comission on studies of the quaternary period, 67, 6–19, 2007.
Jones, B. M., Arp, C. D., Jorgenson, M. T., Hinkel, K. M., Schmutz, J. A., and Flint, P. L.: Increase in the rate and uniformity of coastline erosion in Arctic Alaska, Geophys. Res. Lett., 36, L03503, https://doi.org/10.1029/2008GL036205, 2009a.
Jones, B. M., Arp, C. D., Beck, R. A., Grosse, G., Webster, J. M., and Urban, F.: Erosional history of Cape Halkett and contemporary monitoring of bluff retreat, Beaufort Sea coast, Alaska, Polar Geogr., 32, 129–142, https://doi.org/10.1080/10889370903486449, 2009b.
Jones, B. M., Grosse, G., Arp, C. D., Jones, M. C., Walter Anthony, K. M., and Romanovsky, V. E.: Modern thermokarst lake dynamics in the continuous permafrost zone, northern Seward Peninsula, Alaska, J. Geophys. Res., 116, G00M03, https://doi.org/10.1029/2011JG001666, 2011.
Kamiya, I.: Reduction of JPEG Noise from the ALOS PRISM Products, Bulletin of the Geographical Survey Institute, 55, 31–38, 2008.
Kaplina, T. N.: Nekotorye osobennosti razmyva beregov, slozhennykh mnogoletnemerzlymi gornymi porodami (Some features of coastal thermoerosion of frozen bluffs), Questions of sea coast research, Publishing House of the USSR Academy of Sciences, Moscow, 113–117, 1959.
Kaplina, T. N.: Drevnie alasnye kompleksy Severnoi Yakutii – soobshchenie 2 (Ancient alas complexes of Northern Yakutia – part 2), Kriosfera Zemli (Earth's Cryosphere), 15, 20–30, available at: http://www.izdatgeo.ru/pdf/krio/2011-3/20.pdf, 2011.
Kholodov, A., Gilichinsky, D., Ostroumov, V., Sorokovikov, V., Abramov, A., Davydov, S., and Romanovsky, V.: Regional and local variability of modern natural changes in permafrost temperature in the Yakutian coastal lowlands, Northeastern Siberia, in: Proceedings of the Tenth International Conference on Permafrost, Salekhard, Yamal-Nenets Autonomous District, Russia, 25–29 June, edited by: Hinkel, K., vol. 1, International Contributions, 203–207, 2012.
Kizyakov, A. I., Leibman, M. O., and Perednya, D. D.: Destruktivnye rel'efoobrazuyushie processy poberezhii arkticheckikh ravnin c plastovymi podzemnymi l'dami (Destructive relief-forming processes at the coasts of the arctic plains with tabular ground ice), Kriosfera Zemli (Earth's Cryosphere), 10, 79–89, available at: http://www.izdatgeo.ru/pdf/krio/2006-2/79.pdf, 2006.
Klyuev, Y. V.: Termicheskaya abraziya pribrezhnoi polosy polyarnykh morey (Thermal erosion of the coastal zone of polar seas), Izvestiya vsesoyuznogo geograficheskogo obshchestva, 102, 129–135, 1970.
Lantuit, H. and Pollard, W. H.: Temporal stereophotogrammetric analysis of retrogressive thaw slumps on Herschel Island, Yukon Territory, Nat. Hazards Earth Syst. Sci., 5, 413–423, https://doi.org/10.5194/nhess-5-413-2005, 2005.
Lantuit, H. and Pollard, W. H.: Fifty years of coastal erosion and retrogressive thaw slump activity on Herschel Island, southern Beaufort Sea, Yukon Territory, Canada, Geomorphology, 95, 84–102, https://doi.org/10.1016/j.geomorph.2006.07.040, 2008.
Lantuit, H., Rachold, V., Pollard, W. H., Steenhuisen, F., Ødegård, R., and Hubberten, H.-W.: Towards a calculation of organic carbon release from erosion of Arctic coasts using non-fractal coastline datasets, Mar. Geol., 257, 1–10, https://doi.org/10.1016/j.margeo.2008.10.004, 2009.
Lantuit, H., Atkinson, D., Overduin, P. P., Grigoriev, M. N., Rachold, V., Grosse, G., and Hubberten, H.-W.: Coastal erosion dynamics on the permafrost-dominated Bykovsky Peninsula, north Siberia, 1951–2006, Polar Res., 30, 7341, https://doi.org/10.3402/polar.v30i0.7341, 2011a.
Lantuit, H., Overduin, P. P., Couture, N., Wetterich, S., Are, F., Atkinson, D., Brown, J., Cherkashov, G., Drozdov, D., Forbes, D. L., Graves-Gaylord, A., Grigoriev, M. N., Hubberten, H.-W., Jordan, J., Jorgenson, T., Ødegård, R. S., Ogorodov, S., Pollard, W. H., Rachold, V., Sedenko, S., Solomon, S., Steenhuisen, F., Streletskaya, I., and Vasiliev, A.: The Arctic coastal dynamics database: a new classification scheme and statistics on arctic permafrost coastlines, Estuar. Coast., 35, 383–400, https://doi.org/10.1007/s12237-010-9362-6, 2011b.
Leibman, M., Gubarkov, A., Khomutov, A., Kizyakov, A., Vanshtein, B.: Coastal processes at the tabular-ground-ice-bearing area, Yugorsky Peninsula, Russia, in: Proceedings of the Ninth International Conference on Permafrost, University of Alaska Fairbanks, June 29–July 3, edited by: Kane, D. L. and Hinkel, K. M., vol. 1, 1037–1042, 2008.
Le Moigne, J., Cole-Rhodes, A. A., Eastman, R. D., Netanyahu, N. S., Stone, H. S., Zavorin, I., and Morisette, J. T.: Multitemporal and multisensor image registration, in: Image Registration for Remote Sensing, edited by: Le Moigne, J., Netanyahu, N. S., and Eastman, R. D., Cambridge University press, chap. 14, 293–338, 2011.
Markus, T., Stroeve, J. C., and Miller, J.: Recent changes in Arctic sea ice melt onset, freezeup, and melt season length, J. Geophys. Res.-Oceans, 114, C12024, https://doi.org/10.1029/2009JC005436, 2009.
Mars, J. C. and Houseknecht, D. W.: Quantitative remote sensing study indicates doubling of coastal erosion rate in past 50 yr along a segment of the Arctic coast of Alaska, Geology, 35, 583–586, https://doi.org/10.1130/G23672A.1, 2007.
Maslanik, J., Stroeve, J., Fowler, C., and Emery, W.: Distribution and trends in Arctic sea ice age through spring 2011, Geophys. Res. Lett., 38, L13502, https://doi.org/10.1029/2011GL047735, 2011.
Morgenstern, A., Grosse, G., Günther, F., Fedorova, I., and Schirrmeister, L.: Spatial analyses of thermokarst lakes and basins in Yedoma landscapes of the Lena Delta, The Cryosphere, 5, 849–867, https://doi.org/10.5194/tc-5-849-2011, 2011.
Opel, T., Dereviagin, A. Y., Meyer, H., Schirrmeister, L., and Wetterich, S.: Palaeoclimatic information from stable water isotopes of Holocene ice wedges on the Dmitrii Laptev Strait, Northeast Siberia, Russia, Permafrost Periglac., 22, 84–100, https://doi.org/10.1002/ppp.667, 2011.
Overduin, P. P., Hubberten, H.-W., Rachold, V., Romanovskii, N. N., Grigoriev, M. N., and Kasymskaya, M.: The evolution and degradation of coastal and offshore permafrost in the Laptev and East Siberian Seas during the last climatic cycle, in: Coastline Changes: Interrelation of Climate and Geological Processes, edited by: Harff, J., Hay, W., and Tetzlaff, D., The Geological Society of America Special Paper, 426, 97–111, https://doi.org/10.1130/2007.2426(07), 2007.
Overeem, I., Anderson, R. S., Wobus, C. W., Clow, G. D., Urban, F. E., and Matell, N.: Sea ice loss enhances wave action at the Arctic coast, Geophys. Res. Lett., 38, L17503, https://doi.org/10.1029/2011GL048681, 2011.
Peterson, B. J., Holmes, R. M., McClelland, J. W., Vorosmarty, C. J., Lammers, R. B., Shiklomanov, A. I., Shiklomanov, I. A., and Rahmstorf, S.: Increasing river discharge to the Arctic Ocean, Science, 298, 2171–2173, https://doi.org/10.1126/science.1077445, 2002.
Pieczonka, T., Bolch, T., and Buchroithner, M.: Generation and evaluation of multitemporal digital terrain models of the Mt. Everest area from different optical sensors, Int. Soc. Photogramme., 66, 927–940, https://doi.org/10.1016/j.isprsjprs.2011.07.003, 2011.
Ping, C.-L., Michaelson, G. J., Guo, L., Jorgenson, M. T., Kanevskiy, M., Shur, Y., Dou, F., and Liang, J.: Soil carbon and material fluxes across the eroding Alaska Beaufort Sea coastline, J. Geophys. Res., 116, G02004, https://doi.org/10.1029/2010JG001588, 2011.
Pipko, I. I., Semiletov, I. P., Pugach, S. P., Wåhlström, I., and Anderson, L. G.: Interannual variability of air-sea CO2 fluxes and carbon system in the East Siberian Sea, Biogeosciences, 8, 1987–2007, https://doi.org/10.5194/bg-8-1987-2011, 2011.
Pizhankova, E. I. and Dobrynina, M. S.: Dinamika poberezh'ya Lyakhovskikh Ostrovov – Rezultaty deshifrirovaniya aerokosmicheskikh snimkov (The dynamics of the Lyakhovsky Islands coastline – results of aerospace image interpretation), Kriosfera Zemli (Earth's Cryosphere), 14, 66–79, available at: http://www.izdatgeo.ru/pdf/krio/2010-4/66.pdf, 2010.
Popov, A. I.: Regionalnaya Kriolitologiya (Regional Cryolithology), Moscow State University Publishing House, 1989.
Rachold, V., Grigoriev, M. N., Are, F. E., Solomon, S., Reimnitz, E., Kassens, H., and Antonow, M.: Coastal erosion vs riverine sediment discharge in the Arctic Shelf seas, Int. J. Earth Sci., 89, 450–460, https://doi.org/10.1007/s005310000113, 2000a.
Rachold, V., Grigoriev, M. N., and Bauch, H.: An estimation of the sediment budget in the Laptev Sea during the last 5000 years, Polarforschung, 70, 151–157, available at: http://epic.awi.de/28493/, 2000b.
Rachold, V., Are, F. E., Atkinson, D. E., Cherkashov, G., and Solomon, S. M.: Arctic Coastal Dynamics (ACD): an introduction, Geo-Mar. Lett., 25, 63–68, https://doi.org/10.1007/s00367-004-0187-9, 2003.
Raymond, P. A., McClelland, J. W., Holmes, R. M., Zhulidov, A. V., Mull, K., Peterson, B. J., Striegl, R. G., Aiken, G. R., and Gurtovaya, T. Y.: Flux and age of dissolved organic carbon exported to the Arctic Ocean: A carbon isotopic study of the five largest arctic rivers, Global Biogeochem. Cy., 21, GB4011, https://doi.org/10.1029/2007GB002934, 2007.
Razumov, S. O.: Permafrost as a factor of the dynamics of the coastal zone of the Russian East Arctic Seas, Oceanology, 50, 262–267, https://doi.org/10.1134/S0001437010020116, 2010.
Razumov, S. O. and Grigoriev, M. N.: Coastal erosion as a destabilizing factor of carbonate balance in the East Siberian Arctic seas, Kriosfera Zemli (Earth's Cryosphere), 15, 65–68, available at: http://www.izdatgeo.ru/pdf/krio/2011-4/65_eng.pdf, 2011.
Romanovskii, N. N. and Tumskoy, V. E.: Retrospektivnyi podkhod k ocenke sovremennogo rasprostraneniya i stroeniya shelfovoi kriolitozony vostochnoi Arktiki (Retrospective approach to the estimation of the contemporary extension and structure of the shelf cryolithozone in East Arctic), Kriosfera Zemli (Earth's Cryosphere), 15, 3–14, available at: http://www.izdatgeo.ru/pdf/krio/2011-1/3.pdf, 2011.
Romanovskii, N., Hubberten, H.-W., Gavrilov, A., Tumskoy, V., Tipenko, G., Grigoriev, M., and Siegert, C.: Thermokarst and land-ocean interactions, Laptev Sea Region, Russia, Permafrost Periglac., 11, 137–152, https://doi.org/10.1002/1099-1530(200004/06)11:2<137::AID-PPP345>3.0.CO;2-L, 2000.
Romanovsky, V. E., Drozdov, D. S., Oberman, N. G., Malkova, G. V., Kholodov, A. L., Marchenko, S. S., Moskalenko, N. G., Sergeev, D. O., Ukraintseva, N. G., Abramov, A. A., Gilichinsky, D. A., and Vasiliev, A. A.: Thermal state of permafrost in Russia, Permafrost Periglac., 21, 136–155, https://doi.org/10.1002/ppp.683, 2010.
ROSHYDROMET and ArcticRIMS: Lena at Kusur, stream discharge station data, available at: http://rims.unh.edu/data/station/station.cgi?station=6342, 2009.
RSG: Remote Sensing Software Graz, software documentation, release 7.03, Institute for Digital Image Processing of Joanneum Research, Graz, Austria, 2011.
Santoro, M. and Strozzi, T.: Circumpolar digital elevation models > 55°N with links to geotiff images, ESA DUE Permafrost, DEM from Russian Topographic Maps, https://doi.org/10.1594/PANGAEA.779748, 2012.
Schirrmeister, L., Grosse, G., Kunitsky, V., Magens, D., Meyer, H., Dereviagin, A., Kuznetsova, T., Andreev, A., Babiy, O., Kienast, F., Grigoriev, M., Overduin, P. P., and Preusser, F.: Periglacial landscape evolution and environmental changes of Arctic lowland areas for the last 60 000 years (western Laptev Sea coast, Cape Mamontov Klyk), Polar Res., 27, 249–272, https://doi.org/10.1111/j.1751-8369.2008.00067.x, 2008.
Schirrmeister, L., Grosse, G., Wetterich, S., Overduin, P. P., Strauss, J., Schuur, E. A. G., and Hubberten, H.-W.: Fossil organic matter characteristics in permafrost deposits of the northeast Siberian Arctic, J. Geophys. Res., 116, G00M02, https://doi.org/10.1029/2011JG001647, 2011a.
Schirrmeister, L., Kunitsky, V., Grosse, G., Wetterich, S., Meyer, H., Schwamborn, G., Babiy, O., Derevyagin, A., and Siegert, C.: Sedimentary characteristics and origin of the Late Pleistocene Ice Complex on north-east Siberian Arctic coastal lowlands and islands – a review, Quaternary Int., 241, 3–25, https://doi.org/10.1016/j.quaint.2010.04.004, 2011b.
Sekretov, S. B.: Eurasian Basin – Laptev Sea geodynamic system: tectonic and structural evolution, Polarforschung, 69, 51–54, available at: http://epic.awi.de/28453/, 2001.
Semiletov, I. P., Pipko, I. I., Shakhova, N. E., Dudarev, O. V., Pugach, S. P., Charkin, A. N., McRoy, C. P., Kosmach, D., and Gustafsson, Ö.: Carbon transport by the Lena River from its headwaters to the Arctic Ocean, with emphasis on fluvial input of terrestrial particulate organic carbon vs. carbon transport by coastal erosion, Biogeosciences, 8, 2407–2426, https://doi.org/10.5194/bg-8-2407-2011, 2011.
Shiklomanov, N. I., Streletskiy, D. A., and Nelson, F. E.: Northern Hemisphere component of the Global Circumpolar Active Layer Monitoring (CALM) Program, in: Proceedings of the Tenth International Conference on Permafrost, Salekhard, Yamal-Nenets Autonomous District, Russia, 25–29 June 2012, edited by: Hinkel, K. M., vol. 1, International Contributions, 377–382, The Northern Publisher, Salekhard, 2012.
Shur, Y., Vasiliev, A., Kanevskiy, M., Maximov, V., Pokrovsky, S., and Zaikanov, V.: Shore Erosion in Russian Arctic, in: Cold regions Engineering – Cold Regions Impacts on Transportation and Infrastructure, edited by: Merrill, K., American Society of Civil Engineers, 736–747, 2002.
Sisko, R. K.: Termoabrazionnye berega arkticheskikh morei – na primere o. Novaya Sibir (Thermo-abrasional coasts of arctic seas – on the example of the island of New Siberia), Glaciologicheskie issledovaniya v polyarnykh stranakh (glaciological research in polar regions), AANII, Leningrad, 294, 183–194, 1970.
Sohn, H. G., Kim, G.-H., and Yom, J.-H.: Mathematical modelling of historical reconnaissance CORONA KH-4B imagery, Photogramm Rec, 19, 51–66, https://doi.org/10.1046/j.0031-868X.2003.00257.x, 2004.
Sovershaev, V. A.: Beregovaya zona arkticheskikh morei (Coastal zone of Arctic Seas), in: Geoekologiya Severa (Geoecology of the North), edited by: Solomatin, V. I., Moscow State University Publishing House, Moscow, chap. 2.5, 55–59, 1992.
Strauss, J. and Schirrmeister, L.: Permafrost sequences of Buor Khaya Peninsula, in: Russian–German Cooperation System Laptev Sea: The Expedition Eastern Laptev Sea – Buor Khaya Peninsula 2010, edited by: Wetterich, S., Overduin, P. P., and Grigoriev, M. N., vol. 629, Reports on Polar and Marine Research, Alfred-Wegener-Institute, chap. 5, 35–50, available at: http://epic.awi.de/29931/, 2011.
Strauss, J., Schirrmeister, L., Wetterich, S., Borchers, A., and Davydov, S. P.: Grain-size properties and organic-carbon stock of Yedoma Ice Complex permafrost from the Kolyma lowland, northeastern Siberia, Global Biogeochem. Cy., 26, GB3003, https://doi.org/10.1029/2011GB004104, 2012.
Streletskaya, I. D., Kanevskiy, M. Z., and Vasiliev, A. A.: Massive ground ice in dislocated quaternary sediments of Western Yamal, Kriosfera Zemli (Earth's Cryosphere), 10 (2), 68–78, available at: http://www.izdatgeo.ru/pdf/krio/2006-2/68.pdf, 2006.
Thieler, E. R., Himmelstoss, E. A., Zichichi, J. L., and Ergul, A.: Digital Shoreline Analysis System (DSAS) version 4.0 – an ArcGIS extension for calculating shoreline change, US Geological Survey Open-File Report 2008–1278, 2009.
Toutin, T.: Review article: geometric processing of remote sensing images: models, algorithms and methods, Int. J. Remote Sens., 25, 1893–1924, https://doi.org/10.1080/0143116031000101611, 2004.
Treshnikov, A. F.: Atlas Arktiki. (Atlas of the Arctic.), National Commission of Hydro-Meteorology and Environmental Protection, Major Dept. of Geodesy and Cartography, Moscow, 1985.
Ulrich, M., Morgenstern, A., Günther, F., Reiss, D., Bauch, K. E., Hauber, E., Rössler, S., and Schirrmeister, L.: Thermokarst in Siberian ice-rich permafrost: comparison to asymmetric scalloped depressions on Mars, J. Geophys. Res., 115, E10009, https://doi.org/10.1029/2010JE003640, 2010.
Van Huissteden, J., Berrittella, C., Parmentier, F. J. W., Mi, Y., Maximov, T. C., and Dolman, A. J.: Methane emissions from permafrost thaw lakes limited by lake drainage, Nat. Clim. Change, 1, 119–123, https://doi.org/10.1038/nclimate1101, 2011.
Vasiliev, A. A., Streletskaya, I. D., Shirokov, R. S., and Oblogov, G. E.: Coastal permafrost evolution of western Yamal in context of climate change, Kriosfera Zemli (Earth's Cryosphere), 15, 63–65, available at: http://www.izdatgeo.ru/pdf/krio/2011-4/63_eng.pdf, 2011.
Vonk, J. E., Sánchez-García, L., van Dongen, B. E., Alling, V., Kosmach, D., Charkin, A., Semiletov, I. P., Dudarev, O. V., Shakhova, N., Roos, P., Eglinton, T. I., Andersson, A., and Gustafsson, Ö.: Activation of old carbon by erosion of coastal and subsea permafrost in Arctic Siberia, Nature, advance online publication, 489, 137–140, https://doi.org/10.1038/nature11392, 2012.
Wassmann, P.: Arctic marine ecosystems in an era of rapid climate change, Prog. Oceanogr., 90, 1–17, https://doi.org/10.1016/j.pocean.2011.02.002, 2011.
Wetterich, S. and Schirrmeister, L.: Limnological studies in the Dmitrii Laptev Strait region, in: Russian–German Cooperation System Laptev Sea: The Expedition Lena – New Siberian Islands 2007 during the International Polar Year 2007/2008, edited by: Boike, J., Bolshiyanov, D. Y., Schirrmeister, L., and Wetterich, S., vol. 584, Reports on Polar and Marine Research, Alfred Wegener Institute, chap. 5.2, 155–163, available at: http://epic.awi.de/28775/, 2008.
Wetterich, S., Schirrmeister, L., Andreev, A. A., Pudenz, M., Plessen, B., Meyer, H., and Kunitsky, V. V.: Eemian and Late Glacial/Holocene palaeoenvironmental records from permafrost sequences at the Dmitry Laptev Strait (NE Siberia, Russia), Palaeogeogr. Palaeocl., 279, 73–95, https://doi.org/10.1016/j.palaeo.2009.05.002, 2009.
Wetterich, S., Overduin, P. P., and Grigoriev, M. N. (Eds.): Russian–German Cooperation System Laptev Sea: The Expedition Eastern Laptev Sea – Buor Khaya Peninsula 2010, vol. 629, Reports on Polar and Marine Research, Alfred Wegener Institute, available at: http://epic.awi.de/29931/, 2011.
Whitehouse, P. L., Allen, M. B., and Milne, G. A.: Glacial isostatic adjustment as a control on coastal processes: an example from the Siberian Arctic, Geology, 35, 747–750, https://doi.org/10.1130/G23437A.1, 2007.
Winterfeld, M., Schirrmeister, L., Grigoriev, M. N., Kunitsky, V. V., Andreev, A., Murray, A., and Overduin, P. P.: Coastal permafrost landscape development since the Late Pleistocene in the western Laptev Sea, Siberia, Boreas, 40, 697–713, https://doi.org/10.1111/j.1502-3885.2011.00203.x, 2011.
Altmetrics
Final-revised paper
Preprint