Results 41 to 50 of about 284,030 (141)
Permafrost and Periglacial Processes, Volume 37, Issue 4, Page 725-752, October/December 2026.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
Permafrost and Periglacial Processes, Volume 37, Issue 4, Page 765-777, October/December 2026.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
Snow College Convocation, circa 1990
, 1990 Photo of the print program for Leonard H.
Snow College
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Experimental Simulation of Wet-Snow Shedding from Sagged Cables [PDF]
The process of wet-snow shedding from overhead cables was simulated in cold-chamber experiments under different ambient conditions. The main objective of the study was to examine how cable sag influences the snow-shedding process. However, the effects of
Kollar, László E. +3 more
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The Anatomy of a Dust Emitting Hot Spot: The White Sands Playa‐Aeolian System, New Mexico, USA
Journal of Geophysical Research: Earth Surface, Volume 131, Issue 10, October 2026.Abstract The White Sands aeolian system is a hot spot of dust emissions and has likely been a persistent dust source since the early to mid‐Holocene, when arid conditions promoted the desiccation and erosion of Pleistocene Lake Otero and the formation of the dune field.
M. R. Sweeney +7 more
wiley +1 more source
Living Snow Fences; TR-460, 2006 [PDF]
, 2006 Blowing snow can cause significant problems for mobility and safety during winter weather in three distinct ways. It may drift onto the road, thus requiring almost continuous plowing while the wind is blowing (which may occur when a given winter storm is
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Evaluation of snow cover and depth simulated by a land-surface model using detailed regional snow observations from Austria [PDF]
, 2010 An evaluation is undertaken of the accuracy with which the Joint UK Land Environment Simulator (JULES) can simulate snow cover and depth when driven using data from the Hadley Centre Regional Climate Model.
Thomas Lafon +8 more
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On the Adversarial Robustness of Hydrological Models
Water Resources Research, Volume 62, Issue 10, October 2026.Abstract The evaluation of hydrological models is essential for both model selection and reliability assessment. However, comparing predictions with observations alone is insufficient to fully characterize model behavior. This limitation is particularly relevant to deep learning (DL) models because of their complex internal structures.
Yang Yang +3 more
wiley +1 more source
STRUCTURAL TRANSFORMATION OF THE METAMORPHOSIS GROUP : TOWARDS A METAECONOMIC THEORY OF METAMORPHOSIS [PDF]
As a case study of metaeconomic analysis we discuss Marx.s economic thinking on .metamorphosis.. Our aim is to extend the coverage of the concept beyond the ordinary sphere of economic analysis.
KAMITAKE, YOSHIRO
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Implications of spatial distributions of snow mass and melt rate for snow-cover depletion: observations in a subarctic mountain catchment [PDF]
, 2004 Spatial statistics of snow water equivalent (SWE) and melt rate were measured using spatially distributed, sequential ground surveys of depth and density in forested, shrub and alpine tundra environments over several seasons within a 185 km(2) mountain ...
Pomeroy, J +2 more
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