Results 111 to 120 of about 12,423 (209)

DARTS: Multi-year database of AI-detected retrogressive thaw slumps in the circum-arctic permafrost region

open access: yesScientific Data
Retrogressive Thaw Slumps (RTS) are widespread mass-wasting hillslope failures triggered by thawing permafrost. While regional studies have provided insights into the spatial distribution and dynamics of RTS, a consistent and unbiased quantification and ...
Ingmar Nitze   +9 more
doaj   +1 more source

Natural Fracture Ventilation Altering the Ground Thermal Regime in Unstable Rock Slopes—A Case Study From Western Norway

open access: yesJournal of Geophysical Research: Earth Surface, Volume 131, Issue 11, November 2026.
Abstract Open bedrock fractures are common features in unstable rock slopes and alter subsurface thermal conditions of fractured rock masses through convective air ventilation and atmospheric exchange. These processes are particularly relevant in cold mountain environments, where variations in ground temperature affect rock mass stability and may allow
T. Scheiber   +4 more
wiley   +1 more source

Study of hydrothermal processes in ice-layers subgrade under constant temperature and dynamic loading

open access: yesScientific Reports
The presence of ice-layers in the subgrade soils makes the hydrothermal state of road subgrade built in island permafrost regions more susceptible to external environmental influences.
Jinbang Zhai   +3 more
doaj   +1 more source

Petagram‐Scale Dissolved Organic Carbon Stocks in Alaskan Permafrost Soils

open access: yesGeophysical Research Letters, Volume 53, Issue 20, 28 October 2026.
Abstract The pan‐Arctic permafrost region hosts vast amounts of soil organic carbon, a pool increasingly susceptible to climate‐driven changes. Dissolved organic carbon (DOC) is a key component of this carbon pool. However, its stocks and fluxes remain poorly understood due to limited measurements and challenges of tracking subsurface fluxes across ...
Yongni He   +5 more
wiley   +1 more source

Net Carbon Transfer From Ocean to Land During the Last Deglaciation Synchronous With Sea Level Rise and Lagging Atmospheric CO2 by Several Millennia

open access: yesGeophysical Research Letters, Volume 53, Issue 20, 28 October 2026.
Abstract The sequence of events in the global carbon cycle during deglaciations is not entirely understood. Here, we analyze mean ocean δ13 ${\delta }^{13}$C and δ18 ${\delta }^{18}$O in an updated compilation of foraminiferal stable isotope data comprising 902 time series from 381 sediment cores, with individual records covering intervals within the ...
Peter Köhler, Stefan Mulitza
wiley   +1 more source

Constraining Fault Kinematics and India‐Tarim Convergence Partitioning in Southwestern Tibet With Geodetic Block Modeling

open access: yesGeophysical Research Letters, Volume 53, Issue 20, 28 October 2026.
Abstract How the convergent strain between the India Plate and the Tarim basin is partitioned by active faults and off‐fault deformation in southwestern Tibet is poorly understood due to limited knowledge of strain localisation and fault kinematics. In this study, we derive high‐resolution velocity fields for the southwestern Tibetan Plateau using both
Dehua Wang   +4 more
wiley   +1 more source

Permafrost

open access: yes, 1972
The upsurge of public interest in northern regions in recent years has brought the name `permafrost' into the market place. The proposed construction of pipelines for gas and oil from the Arctic Coast to southern Canada is now generally known to be complicated by the existence of permafrost along considerable parts of the routes that may be followed ...
openaire   +1 more source

Sandy Turbidity Current Acts as a Rusty Carbon Pump at the Shelf Edge

open access: yesGeophysical Research Letters, Volume 53, Issue 20, 28 October 2026.
Abstract Sandy turbidity currents (STCs) efficiently sequester organic carbon (OC) through rapid burial. Yet our understanding of OC preservation within STC deposits remains far less constrained, especially considering STC deposits as an inferred major sink for iron‐bound OC (Fe‐OC), a long‐term stabilized form of OC.
Zhuoyue Zhang   +7 more
wiley   +1 more source

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