Results 61 to 70 of about 423 (178)
Debris properties and mass-balance impacts on adjacent debris-covered glaciers, Mount Rainier, USA
The north and east slopes of Mount Rainier, Washington, are host to three of the largest glaciers in the contiguous United States: Carbon Glacier, Winthrop Glacier, and Emmons Glacier. Each has an extensive blanket of supraglacial debris on its terminus,
Peter L. Moore +2 more
doaj +1 more source
Refined energy-balance modelling of a supraglacial pond, Langtang Khola, Nepal
Supraglacial ponds on debris-covered glaciers present a mechanism of atmosphere/glacier energy transfer that is poorly studied, and only conceptually included in mass-balance studies of debris-covered glaciers.
Evan S. Miles +5 more
doaj +1 more source
Controls on Ice Cliff Distribution and Characteristics on Debris‐Covered Glaciers
Ice cliff distribution plays a major role in determining the melt of debris‐covered glaciers but its controls are largely unknown. We assembled a data set of 37,537 ice cliffs and determined their characteristics across 86 debris‐covered glaciers within ...
Marin Kneib +13 more
doaj +1 more source
Winter Baseflow Calibration's Critical Role in Hydrological Modeling for the Pamir Region
Abstract The Pamir Mountains, a critical water source for Central Asia, require accurate quantification of runoff components for water resource management under climate change. Uncertainties in precipitation data are known to greatly affect hydrological model accuracy, leading to the widespread use of multi‐data calibration methods to avoid internal ...
J. Huang +4 more
wiley +1 more source
Supraglacial debris-transport variability over time: examples from Switzerland and Iceland [PDF]
The volume of debris in the left-lateral, Little Ice Age (LIA: AD 1550–1850) moraine of the Feegletscher, Valais, Switzerland was compared with the actual volume being transported currently by the glacier. The latter is smaller by a factor of about two.
W.B. Whalley +3 more
openaire +1 more source
AbstractThe origin of supraglacial debris covers is often conceptualised as the formation of a surface lag by melt‐out of englacial debris from slow‐moving ice, where complexity arises from feedback between debris thickness and sub‐debris ice melt. Here, we examine the origin of a debris cover from the perspective of debris provenance and changing ...
Martin P. Kirkbride +7 more
openaire +6 more sources
Dynamic Changes of a Thick Debris-Covered Glacier in the Southeastern Tibetan Plateau
Debris-covered glaciers have contrasting melting mechanisms and climate response patterns if compared with debris-free glaciers and thus show a unique influence on the hydrological process.
Zhen He +5 more
doaj +1 more source
Repeat laser scanning and change detection revealed that large but infrequent rockfall events dominated summer debris supply from subaerial rock slopes bordering Miage Glacier, Italy. Rockfall source locations reflect the legacy of recent deglaciation and possibly longer‐term glacial trimlines, highlighting climate‐driven controls on sediment fluxes in
Rebecca Stewart +4 more
wiley +1 more source
Representing moisture fluxes and phase changes in glacier debris cover using a reservoir approach [PDF]
Due to the complexity of treating moisture in supraglacial debris, surface energy balance models to date have neglected moisture infiltration and phase changes in the debris layer.
E. Collier +5 more
doaj +1 more source
NSF GAGE/SAGE Community Science Workshop: Advancing Geophysical Research Through Collaboration
Abstract The 2025 NSF GAGE/SAGE Community Science Workshop, hosted by the EarthScope Consortium from May 18–21 in Bloomington, Minnesota, convened 188 participants from 109 institutions for four days of scientific exchange and community engagement. The workshop featured plenary sessions, poster presentations, special interest groups, and networking ...
Gillian Haberli +4 more
wiley +1 more source

