Results 231 to 240 of about 341,120 (304)
Internal Structure, Kinematics, and Prehistory of Frozen Debris Lobe‐A (FDL‐A), Brooks Range, Alaska
ABSTRACT Frozen Debris Lobe‐A (FDL‐A)—one of hundreds of FDLs in the Brooks Range of northern Alaska—is a slow‐moving landslide in permafrost that has been the subject of research since 2008 due to its close proximity to the Dalton Highway. Here, we synthesize more than a decade's worth of climate and surface measurements of monitored FDLs, and the ...
Margaret M. Darrow +2 more
wiley +1 more source
Camera-Trap Evidence of <i>Myricaria</i> sp. Consumption and Head-Rubbing by a Wild Snow Leopard (<i>Panthera uncia</i>) in an Alpine Ecosystem. [PDF]
Kinoshita K +7 more
europepmc +1 more source
ABSTRACT Permafrost in northern peatlands occurs within individual palsas or extensive peat plateaus and controls local carbon storage. These permafrost landforms are complex, and their internal structure remains poorly understood. We used quasi‐3D electrical resistivity tomography (ERT) measurements, supported by UAV‐LiDAR topography, frost probing ...
Cas Renette +5 more
wiley +1 more source
Atmospheric Microbial Transport to Antarctica and Its Ecological Implications: A Systematic Review. [PDF]
Goldenberg-Barbosa R +5 more
europepmc +1 more source
ABSTRACT The McMurdo Dry Valleys, the largest ice‐free region in Antarctica, are home to a cold‐desert hydrologic system of glaciers, snowbanks, streams, and lakes. Freshwater is also stored as dead glacial ice, which is poorly constrained in terms of ion concentrations and interactions with both in situ and overlying sediments.
Matthew C. Witscheber, Kate M. Swanger
wiley +1 more source
Soil microbial communities and carbon and nitrogen forms across snow-driven vegetation types in alpine tundra. [PDF]
Benech A +7 more
europepmc +1 more source
ABSTRACT Pingos are large mounds with cores formed of intrusive ice that form in periglacial landscapes. These ice structures can form in regions of discontinuous permafrost, commonly as hydraulic or open‐system pingos, or in locations of continuous permafrost, commonly as hydrostatic or closed‐system pingos.
Venezia M. Follingstad +12 more
wiley +1 more source
Epidemiology of Alpine Skiing and Snowboarding Injuries: A Systematic Review and Meta-Analysis. [PDF]
Laaksonen J +5 more
europepmc +1 more source
ABSTRACT Freeze–thaw processes cause periglacial creep (otherwise known as solifluction) which forms solifluction lobes. These are lobate features characterized by a steep riser (front) and a smooth tread (body). Despite the widespread occurrence of these lobes, the controls on their morphometry remain poorly understood. Research into solifluction lobe
Jil S. van Etten +2 more
wiley +1 more source
Sexual differences of temporal marking and communication behaviours of common leopards (Panthera pardus) in Luolong County, Tibet. [PDF]
Guo K +15 more
europepmc +1 more source

