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Poor performance of a common crevasse model at marine-terminating glaciers
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Sharp Contrasts in Observed and Modeled Crevasse Patterns at Greenland’s Marine...
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Observed mechanism for sustained glacier retreat and acceleration in response to...
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Observed mechanism for sustained glacier retreat and acceleration in response to...
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Observed mechanism for sustained glacier retreat and acceleration in response to...
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Revisiting the role of vertical shear in analytic ice shelf models
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Rolling stones gather moss: movement and longevity of moss balls on an Alaskan g...
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Brief communication: Is vertical shear in an ice shelf (still) negligible?
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Revisiting the role of vertical shear in analytic ice shelf models
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Brief communication: Is vertical shear in an ice shelf (still) negligible?
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Evaluation of Iceberg Calving Models Against Observations from Greenland Outlet...
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Steep Glacier Bed Knickpoints Mitigate Inland Thinning in Greenland
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Steep Glacier Bed Knickpoints Mitigate Inland Thinning in Greenland.
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Dynamic Changes at Yahtse Glacier, the Most Rapidly Advancing Tidewater Glacier...
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Dynamic Changes at Yahtse Glacier, the Most Rapidly Advancing Tidewater Glacier...
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Steep Glacier Bed Knickpoints Mitigate Inland Thinning in Greenland.
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Steep Glacier Bed Knickpoints Mitigate Inland Thinning in Greenland
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Steep Glacier Bed Knickpoints Mitigate Inland Thinning in Greenland
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Subseasonal changes observed in subglacial channel pressure, size, and sediment...
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Subseasonal changes observed in subglacial channel pressure, size, and sediment...
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[SDU.STU]Sciences of the Universe [physics]/Earth Sciences
[SDU]Sciences of the Universe [physics]
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