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Wolverines use spatial memory to plan efficient routes through rugged terrain. [PDF]
Glass TW+4 more
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Ecological indicators predict functional diversity dynamics following glacier retreat
Losapio G+7 more
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This essay views glaciers as networks of non/human things that constantly, and slowly, collaborate. Early modern Arctic travel narratives challenge ontological separations between the human and the icescape, demonstrating how glaciers compose bodies and passages, fears and desires, stories and dreams – and how they continue to do so today, even if we ...
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Journal of Fluid Mechanics, 1982
This paper is an attempt at a mathematical synopsis of the theory of wave motions on glaciers. These comprise surface waves (analogous to water waves) and seasonal waves (more like compression waves). Surface waves have been often treated and are well understood, but seasonal waves, while observed, do not seem to have attracted any theoretical ...
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This paper is an attempt at a mathematical synopsis of the theory of wave motions on glaciers. These comprise surface waves (analogous to water waves) and seasonal waves (more like compression waves). Surface waves have been often treated and are well understood, but seasonal waves, while observed, do not seem to have attracted any theoretical ...
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Glacier Fluctuations and Simple Glacier Models
2020This chapter details the formulation and analysis of simple mathematical models that describe the response of glaciers to mass balance changes. The primary focus is on glacier length fluctuations. Key aspects studied include the response time and sensitivity of different glaciers to changes in climate, and the use of models to reconstruct past ...
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Glacier Studies of the McCall Glacier, Alaska
ARCTIC, 1959Describes in detail this glacier in the Romanzof Mts., Brooks Range, northern Alaska, studied during the McCall Glacier Project, 1957-58. The crescent-shaped body of ice, approx. 8 km long, 640 m wide and 1,450 m high, has three cirques and a well defined drainage basin.
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Glacier Runoff Observations at Sholes Glacier
2015Glacier runoff is a major source of streamflow during the summer low-flow season and mitigates both low flow and high water temperatures. Measurement of ablation and discharge immediately below Sholes Glacier quantifies the volume of glacier runoff to the North Fork Nooksack River, which provided more than 40 % of total river runoff on 21 days in ...
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2011
A glacier in equilibrium with the climate is characterized by a given geometry. This geometry results from a balance between snow accumulation, ablation (mainly by melting), and the flow that redistributes the mass accumulated at high elevations toward the lower parts of the glacier. If external forcings (climate) or internal forcings (ice flow) change,
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A glacier in equilibrium with the climate is characterized by a given geometry. This geometry results from a balance between snow accumulation, ablation (mainly by melting), and the flow that redistributes the mass accumulated at high elevations toward the lower parts of the glacier. If external forcings (climate) or internal forcings (ice flow) change,
openaire +2 more sources