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Aeolian and subaqueous bedforms in shear flows
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Zeitschriftentitel: | Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences |
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Personen und Körperschaften: | , |
In: | Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences, 371, 2013, 2004, S. 20120364 |
Format: | E-Article |
Sprache: | Englisch |
veröffentlicht: |
The Royal Society
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Schlagwörter: |
author_facet |
Andreotti, Bruno Claudin, Philippe Andreotti, Bruno Claudin, Philippe |
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author |
Andreotti, Bruno Claudin, Philippe |
spellingShingle |
Andreotti, Bruno Claudin, Philippe Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences Aeolian and subaqueous bedforms in shear flows General Physics and Astronomy General Engineering General Mathematics |
author_sort |
andreotti, bruno |
spelling |
Andreotti, Bruno Claudin, Philippe 1364-503X 1471-2962 The Royal Society General Physics and Astronomy General Engineering General Mathematics http://dx.doi.org/10.1098/rsta.2012.0364 <jats:p>A sediment bed sheared by an unbounded flow is unconditionally unstable towards the growth of bedforms called ripples under water and dunes in the aeolian case. We review here the dynamical mechanisms controlling this linear instability, putting the emphasis on testing models against field and laboratory measurements. We then discuss the role of nonlinearities and the influence of finite size effects, namely the depth of the atmospheric boundary layer in the aeolian case and the water depth in the case of rivers.</jats:p> Aeolian and subaqueous bedforms in shear flows Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences |
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10.1098/rsta.2012.0364 |
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The Royal Society, 2013 |
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The Royal Society, 2013 |
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1364-503X 1471-2962 |
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2013 |
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The Royal Society |
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Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences |
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title |
Aeolian and subaqueous bedforms in shear flows |
title_unstemmed |
Aeolian and subaqueous bedforms in shear flows |
title_full |
Aeolian and subaqueous bedforms in shear flows |
title_fullStr |
Aeolian and subaqueous bedforms in shear flows |
title_full_unstemmed |
Aeolian and subaqueous bedforms in shear flows |
title_short |
Aeolian and subaqueous bedforms in shear flows |
title_sort |
aeolian and subaqueous bedforms in shear flows |
topic |
General Physics and Astronomy General Engineering General Mathematics |
url |
http://dx.doi.org/10.1098/rsta.2012.0364 |
publishDate |
2013 |
physical |
20120364 |
description |
<jats:p>A sediment bed sheared by an unbounded flow is unconditionally unstable towards the growth of bedforms called ripples under water and dunes in the aeolian case. We review here the dynamical mechanisms controlling this linear instability, putting the emphasis on testing models against field and laboratory measurements. We then discuss the role of nonlinearities and the influence of finite size effects, namely the depth of the atmospheric boundary layer in the aeolian case and the water depth in the case of rivers.</jats:p> |
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author | Andreotti, Bruno, Claudin, Philippe |
author_facet | Andreotti, Bruno, Claudin, Philippe, Andreotti, Bruno, Claudin, Philippe |
author_sort | andreotti, bruno |
container_issue | 2004 |
container_start_page | 0 |
container_title | Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences |
container_volume | 371 |
description | <jats:p>A sediment bed sheared by an unbounded flow is unconditionally unstable towards the growth of bedforms called ripples under water and dunes in the aeolian case. We review here the dynamical mechanisms controlling this linear instability, putting the emphasis on testing models against field and laboratory measurements. We then discuss the role of nonlinearities and the influence of finite size effects, namely the depth of the atmospheric boundary layer in the aeolian case and the water depth in the case of rivers.</jats:p> |
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imprint_str_mv | The Royal Society, 2013 |
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physical | 20120364 |
publishDate | 2013 |
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series | Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences |
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spelling | Andreotti, Bruno Claudin, Philippe 1364-503X 1471-2962 The Royal Society General Physics and Astronomy General Engineering General Mathematics http://dx.doi.org/10.1098/rsta.2012.0364 <jats:p>A sediment bed sheared by an unbounded flow is unconditionally unstable towards the growth of bedforms called ripples under water and dunes in the aeolian case. We review here the dynamical mechanisms controlling this linear instability, putting the emphasis on testing models against field and laboratory measurements. We then discuss the role of nonlinearities and the influence of finite size effects, namely the depth of the atmospheric boundary layer in the aeolian case and the water depth in the case of rivers.</jats:p> Aeolian and subaqueous bedforms in shear flows Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences |
spellingShingle | Andreotti, Bruno, Claudin, Philippe, Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences, Aeolian and subaqueous bedforms in shear flows, General Physics and Astronomy, General Engineering, General Mathematics |
title | Aeolian and subaqueous bedforms in shear flows |
title_full | Aeolian and subaqueous bedforms in shear flows |
title_fullStr | Aeolian and subaqueous bedforms in shear flows |
title_full_unstemmed | Aeolian and subaqueous bedforms in shear flows |
title_short | Aeolian and subaqueous bedforms in shear flows |
title_sort | aeolian and subaqueous bedforms in shear flows |
title_unstemmed | Aeolian and subaqueous bedforms in shear flows |
topic | General Physics and Astronomy, General Engineering, General Mathematics |
url | http://dx.doi.org/10.1098/rsta.2012.0364 |