We develop numerical solutions of a theoretical model which has been proposed to explain the formation of subglacial bedforms. The model has been shown to have the capability of producing bedforms in two dimensions, when they may be interpreted as ribbed moraine. However, these investigations have left unanswered the question of whether the theory is capable of producing fully three‐dimensional bedforms such as drumlins. We show that, while the three‐dimensional calculations show realistic quasi‐three‐dimensional features such as dislocations in the ribbing pattern, they do not produce genuine three‐dimensional drumlins. We suggest that this inadequacy is due to the treatment of subglacial drainage in the theory as a passive variable, and t...
The origin of ribbed moraines (Rogen moraine) is a long-discussed topic in the field of geomorpholog...
Subglacial bed forms (drumlins, ribbed moraines, and megascale glacial lineations) are enigmatic rep...
Despite their importance in understanding glaciological processes and constraining large-scale flow ...
We develop numerical solutions of a theoretical model which has been proposed to explain the formati...
peer-reviewedWe summarize the present form of the instability theory for drumlin formation, which de...
Ribbed moraines are large (up to 16 km long) ridges of sediment produced transverse to ice flow dire...
Ribbed (Rogen) moraines are large subglacially formed transverse ridges that cover extensive areas ...
We summarize the present form of the instability theory for drumlin formation, which describes the c...
peer-reviewedSubglacial bedforms,which include drumlins,ribbed moraine,and mega scale glacial lineat...
The instability theory of drumlin formation has been very successful in predicting the existence of ...
Subglacial bedforms are a range of landforms (10 – 105 m in length) shaped mostly in glacial sedimen...
Acknowledgments We thank the editors of PLOS ONE and three anonymous reviewers for their detailed an...
Sediments beneath modern ice sheets exert a key control on their flow, but are largely inaccessible ...
Sediments beneath modern ice sheets exert a key control on their flow, but are largely inaccessible ...
Understanding the evolution of the ice-bed interface is fundamentally important for gaining insight ...
The origin of ribbed moraines (Rogen moraine) is a long-discussed topic in the field of geomorpholog...
Subglacial bed forms (drumlins, ribbed moraines, and megascale glacial lineations) are enigmatic rep...
Despite their importance in understanding glaciological processes and constraining large-scale flow ...
We develop numerical solutions of a theoretical model which has been proposed to explain the formati...
peer-reviewedWe summarize the present form of the instability theory for drumlin formation, which de...
Ribbed moraines are large (up to 16 km long) ridges of sediment produced transverse to ice flow dire...
Ribbed (Rogen) moraines are large subglacially formed transverse ridges that cover extensive areas ...
We summarize the present form of the instability theory for drumlin formation, which describes the c...
peer-reviewedSubglacial bedforms,which include drumlins,ribbed moraine,and mega scale glacial lineat...
The instability theory of drumlin formation has been very successful in predicting the existence of ...
Subglacial bedforms are a range of landforms (10 – 105 m in length) shaped mostly in glacial sedimen...
Acknowledgments We thank the editors of PLOS ONE and three anonymous reviewers for their detailed an...
Sediments beneath modern ice sheets exert a key control on their flow, but are largely inaccessible ...
Sediments beneath modern ice sheets exert a key control on their flow, but are largely inaccessible ...
Understanding the evolution of the ice-bed interface is fundamentally important for gaining insight ...
The origin of ribbed moraines (Rogen moraine) is a long-discussed topic in the field of geomorpholog...
Subglacial bed forms (drumlins, ribbed moraines, and megascale glacial lineations) are enigmatic rep...
Despite their importance in understanding glaciological processes and constraining large-scale flow ...