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Coupled glacio-hydrological models have recently become a valuable method for predicting the hydrological response of catchments in mountainous regions under a changing climate.
María Herminia Pesci +3 more
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AbstractA mixture of approximately one part of water to two parts of kaolin (china clay) has proved suitable for making model glaciers on scales between 1 : 1000 and 1 : 10,000. The kaolin “glaciers” crevasse and flow realistically, and slide on their beds.
W. V. Lewis, Maynard M. Miller
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The representation of iceberg calving in numerical models is a key source of uncertainty in century-scale sea-level rise projections. Parameters central to model representations of calving, including the tensile strength of glacier ice, remain poorly ...
Lizz Ultee, Colin Meyer, Brent Minchew
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Ensemble Kalman Filtering for Glacier Modeling
Working with a two-stage ice sheet model, we explore how statistical data assimilation methods can be used to improve predictions of glacier melt and relatedly, sea level rise. We find that the EnKF improves model runs initialized using incorrect initial conditions or parameters, providing us with better models of future glacier melt.
Corcoran, Emily +4 more
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Analysis of the Image of Global Glacier Tourism Destinations from the Perspective of Tourists
Glaciers are attracting increasing attention in the context of climate change, and glacier tourism has also become a popular tourist product. However, few studies have been conducted concerning the image of glacier tourism destinations.
Fan Tang +3 more
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What Can We Learn from Comparing Glacio-Hydrological Models?
Glacio-hydrological models combine both glacier and catchment hydrology modeling and are used to assess the hydrological response of high-mountain glacierized catchments to climate change. To capture the uncertainties from these model combinations, it is
Elena Stoll +6 more
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Simulation of Historic Glacier Variations with a Simple Climate-Glacier Model [PDF]
AbstractGlacier variations during the last few centuries have shown a marked coherence over the globe. Characteristic features are the maximum stand somewhere in the middle of the nineteenth century, and the steady retreat afterwards (with some minor interruptions depending on the particular region).
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Rock glaciers on the run – understanding rock glacier landform evolution and recent changes from numerical flow modeling [PDF]
Rock glaciers are landforms that form as a result of creeping mountain permafrost which have received considerable attention concerning their dynamical and thermal changes.
J. Müller, A. Vieli, I. Gärtner-Roer
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A unified model for transient subglacial water pressure and basal sliding
Changes in water pressure at the beds of glaciers greatly modify their sliding rate, affecting rates of ice mass loss and sea level change. However, there is still no agreement about the physics of subglacial sliding or how water affects it.
Victor C. Tsai +3 more
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A new global dataset of mountain glacier centerlines and lengths [PDF]
The length of a glacier is a key determinant of its geometry and is an important parameter in glacier inventories and modeling; glacier centerlines are the lines along which the main flow of glaciers takes place and, thus, are crucial inputs for many ...
D. Zhang +9 more
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