Article
Environmental Sciences
Ylva Sjoberg, Ahmad Jan, Scott L. Painter, Ethan T. Coon, Michael P. Carey, Jonathan A. O'Donnell, Joshua C. Koch
Summary: The presence of permafrost in Arctic landscapes affects the flow paths of water, potentially impacting stream discharge and thermal regimes. Simulations show that hillslopes with continuous permafrost have shallower flow paths and higher rates of evapotranspiration. Thawing permafrost alters groundwater flow paths, leading to decreases in summer stream temperatures and reductions in evapotranspiration.
WATER RESOURCES RESEARCH
(2021)
Article
Environmental Sciences
Hanna N. Kreplin, Carla Sofia Santos Ferreira, Georgia Destouni, Saskia D. Keesstra, Luca Salvati, Zahra Kalantari
Summary: Arctic wetlands are impacted by warming and hydrological changes, with key factors being permafrost thaw and concurrent hydrological changes leading to shrinkage and expansion of wetland areas. Various factors interact with warming, hydrological changes, and permafrost thaw in altering the Arctic wetland systems, ultimately affecting the global carbon cycle.
WILEY INTERDISCIPLINARY REVIEWS-WATER
(2021)
Article
Engineering, Civil
Shiqi Liu, Ping Wang, Jingjie Yu, Tianye Wang, Hongyan Cai, Qiwei Huang, Sergey P. Pozdniakov, Yichi Zhang, Ekaterina S. Kazak
Summary: The increasing winter streamflow of major Arctic rivers has been well documented. The study focused on four Arctic rivers with relatively few dam effects and analyzed their climate change-related responses in winter streamflow. The results showed that winter streamflow increased significantly from 1980 to 2019, with the highest increase observed in early winter. Late winter streamflow was particularly sensitive to air temperature changes, potentially due to permafrost degradation. The different change rates in winter streamflow among the four river basins were determined by permafrost degradation and related baseflow discharge processes.
JOURNAL OF HYDROLOGY
(2022)
Article
Geosciences, Multidisciplinary
H. T. Mithan, T. C. Hales, P. J. Cleall
Summary: An increase in Arctic shallow landsliding caused by climate warming is influenced by the topographic controls on ground ice distribution and hydrology, with high ground-ice concentrations near the potential failure plane acting as a stronger control than high average ice volumes or rapid thawing. The low average slopes and low concavity of Arctic hillslopes cannot generate landsliding solely based on pore-water pressures.
GEOPHYSICAL RESEARCH LETTERS
(2021)
Article
Geosciences, Multidisciplinary
David Olefeldt, Mikael Hovemyr, McKenzie A. Kuhn, David Bastviken, Theodore J. Bohn, John Connolly, Patrick Crill, Eugenie S. Euskirchen, Sarah A. Finkelstein, Helene Genet, Guido Grosse, Lorna 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 Raesaenen, Christina Schaedel, Oliver Sonnentag, Maria Strack, Suzanne E. Tank, Claire Treat, Ruth K. Varner, Tarmo Virtanen, Rebecca K. Warren, Jennifer D. Watts
Summary: The study introduces the BorealArctic Wetland and Lake Dataset (BAWLD) to estimate the distribution of wetlands and lakes in the Arctic region. Using expert assessments and random forest modeling, the dataset provides the distribution of various wetland and lake classes, helping to improve assessments of current and future methane emissions.
EARTH SYSTEM SCIENCE DATA
(2021)
Editorial Material
Environmental Sciences
Rebecca Finger-Higgens
Summary: Due to rising air temperatures and autumn rains, some Arctic lakes are drying, leading to permafrost thawing and water drainage.
NATURE CLIMATE CHANGE
(2022)
Article
Geography, Physical
Alexandra Hamm, Andrew Frampton
Summary: Modeling the physical state of permafrost landscapes is crucial in understanding the feedback mechanisms between permafrost and the atmosphere in a warming climate. This study suggests that lateral surface and subsurface processes have a significant impact on permafrost temperatures and active layer properties, with uphill areas on slopes generally warmer than downhill areas. The findings also indicate that temperature distributions in sloped terrain can vary considerably compared to flat terrain, which could impact the response of subsurface hydrothermal conditions to ongoing climate change.
Article
Multidisciplinary Sciences
Shawn M. Chartrand, A. Mark Jellinek, Antero Kukko, Anna Grau Galofre, Gordon R. Osinski, Shannon Hibbard
Summary: This research reconstructs and analyzes the landscape development and channelization in the Muskox Valley region over the past 60 years using multiple sources of data and physical models. The results demonstrate that the presence of polygon fields in permafrost-rich environments plays a crucial role in shaping the establishment and evolution of stream networks.
NATURE COMMUNICATIONS
(2023)
Article
Environmental Sciences
J. C. Koch, Y. Sjoberg, J. A. O'Donnell, M. P. Carey, P. F. Sullivan, A. Terskaia
Summary: This study empirically examined the impacts of changing vegetation cover and soil thaw on the hydrological characteristics of headwater catchments in northwestern Alaska. The results showed that as temperature increases and forests expand, evapotranspiration and infiltration become significant fluxes, while in colder tundra-dominated areas, precipitation is mainly discharged through streamflow. The study also found that even minor warming can lead to increased infiltration and subsurface flow.
ENVIRONMENTAL RESEARCH LETTERS
(2022)
News Item
Geosciences, Multidisciplinary
Michael M. Loranty
Summary: Shrubs in the tundra snowpack function as thermal bridges, facilitating heat loss from the ground during winter and heat gain in spring.
Article
Environmental Sciences
K. Castro-Morales, A. Canning, A. Koertzinger, M. Goeckede, K. Kuesel, W. A. Overholt, T. Wichard, S. Redlich, S. Arzberger, O. Kolle, N. Zimov
Summary: The release of organic matter from thawed permafrost will impact the sources and sinks of greenhouse gases in Arctic rivers. However, little is known about the temporal variation, environmental controls, and magnitude of greenhouse gases in these rivers. This study measured the concentrations of CO2, CH4, and O2 in the Ambolikha River in northeast Siberia, revealing the effects of temperature variation, flooding, and lateral exchange on greenhouse gas emissions.
JOURNAL OF GEOPHYSICAL RESEARCH-BIOGEOSCIENCES
(2022)
Editorial Material
Environmental Sciences
Christina Schaedel
Summary: Rising Arctic temperatures are accelerating coastal erosion, which not only threatens coastal communities and infrastructure, but also adds carbon to the atmosphere. Studies predict that Arctic coastal erosion will exceed historical variability and increase two to three times by the end of the century.
NATURE CLIMATE CHANGE
(2022)
Article
Plant Sciences
Emily P. Pedersen, Bo Elberling, Anders Michelsen
Summary: As arctic permafrost thaws, previously inaccessible nitrogen becomes available to arctic plants, which can take them up locally or transport them downslope. The retention, transport, and uptake of permafrost nitrogen may contribute to shaping arctic vegetation change.
JOURNAL OF ECOLOGY
(2022)
Editorial Material
Multidisciplinary Sciences
J. E. Vonk, N. J. Speetjens, A. E. Poste
Summary: Despite the fact that over 99% of coastal arctic rivers drain small catchments, future projections of land-ocean fluxes are derived from data of large rivers. We advocate for the inclusion and increased focus on smaller catchments to facilitate representative assessments of arctic ecosystem change.
NATURE COMMUNICATIONS
(2023)
Article
Geosciences, Multidisciplinary
Niek Jesse Speetjens, Gustaf Hugelius, Thomas Gumbricht, Hugues Lantuit, Wouter R. Berghuijs, Philip A. Pika, Amanda Poste, Jorien E. Vonk
Summary: ARCADE is an integrated database of over 40,000 catchments that drain into the Arctic Ocean, ranging in size from 1 to 3.1 x 106 km2. It includes numerous small catchments experiencing significant climatic warming and storing large amounts of soil carbon. ARCADE is a key tool for monitoring the pan-Arctic across scales.
EARTH SYSTEM SCIENCE DATA
(2023)