Results 11 to 20 of about 277 (174)

Pathways of ice-wedge degradation in polygonal tundra under different hydrological conditions [PDF]

open access: yesThe Cryosphere, 2019
Ice-wedge polygons are common features of lowland tundra in the continuous permafrost zone and prone to rapid degradation through melting of ground ice.
J. Nitzbon   +9 more
doaj   +8 more sources

Late Holocene ice-wedge polygon dynamics in northeastern Siberian coastal lowlands [PDF]

open access: yesArctic, Antarctic, and Alpine Research, 2018
Ice-wedge polygons are common features of northeastern Siberian lowland periglacial tundra landscapes. To deduce the formation and alternation of ice-wedge polygons in the Kolyma Delta and in the Indigirka Lowland, we studied shallow cores, up to 1.3 m ...
Lutz Schirrmeister   +6 more
doaj   +5 more sources

A Quantitative Graph-Based Approach to Monitoring Ice-Wedge Trough Dynamics in Polygonal Permafrost Landscapes [PDF]

open access: yesRemote Sensing, 2021
In response to increasing Arctic temperatures, ice-rich permafrost landscapes are undergoing rapid changes. In permafrost lowlands, polygonal ice wedges are especially prone to degradation.
Tabea Rettelbach   +6 more
doaj   +3 more sources

The importance of freeze–thaw cycles for lateral tracer transport in ice-wedge polygons [PDF]

open access: yesThe Cryosphere, 2022
A significant portion of the Arctic coastal plain is classified as polygonal tundra and plays a vital role in soil carbon cycling. Recent research suggests that lateral transport of dissolved carbon could exceed vertical carbon releases to the atmosphere.
E. E. Jafarov   +6 more
doaj   +3 more sources

Monitoring Arctic permafrost – examining the contribution of volunteered geographic information to mapping ice-wedge polygons [PDF]

open access: yesThe Cryosphere
This study evaluates the potential of Volunteered Geographic Information (VGI) for mapping and monitoring ice-wedge polygons in Arctic permafrost regions through two case studies in Alaska and Canada.
P. Walz   +11 more
doaj   +8 more sources

Formation of Low-Centered Ice-Wedge Polygons and Their Orthogonal Systems: A Review

open access: yesGeosciences
Ice wedges, which are ubiquitous in permafrost areas, play a significant role in the evolution of permafrost landscapes, influencing the topography and hydrology of these regions. In this paper, we combine a detailed multi-generational, interdisciplinary,
Yuri Shur   +8 more
doaj   +2 more sources

Thermokarst Development Detected from High-Definition Topographic Data in Central Yakutia [PDF]

open access: yesRemote Sensing, 2018
Eastern Siberia is characterized by widespread permafrost thawing and subsequent thermokarst development. Estimation of the impacts of the predicted rise in precipitation and air temperatures under climate change requires quantitative knowledge about the
Hitoshi Saito   +4 more
doaj   +9 more sources

Degradation of ice-wedge polygons leads to increased fluxes of water and DOC

open access: yesScience of The Total Environment, 2023
Ice-wedge polygon landscapes make up a substantial part of high-latitude permafrost landscapes. The hydrological conditions shape how these landscapes store and release organic carbon. However, their coupled water‑carbon dynamics are poorly understood as field measurements are sparse in smaller catchments and coupled hydrology-dissolved organic carbon (
Speetjens, Niek Jesse   +3 more
openaire   +3 more sources

Effects of multi-scale heterogeneity on the simulated evolution of ice-rich permafrost lowlands under a warming climate [PDF]

open access: yesThe Cryosphere, 2021
In continuous permafrost lowlands, thawing of ice-rich deposits and melting of massive ground ice lead to abrupt landscape changes called thermokarst, which have widespread consequences on the thermal, hydrological, and biogeochemical state of the ...
J. Nitzbon   +10 more
doaj   +1 more source

Understanding the relative importance of vertical and horizontal flow in ice-wedge polygons [PDF]

open access: yesHydrology and Earth System Sciences, 2020
Ice-wedge polygons are common Arctic landforms. The future of these landforms in a warming climate depends on the bidirectional feedback between the rate of ice-wedge degradation and changes in hydrological characteristics.
N. A. Wales   +9 more
doaj   +1 more source

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