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Title: A tribute to Michael R. Raupach for contributions to aeolian fluid dynamics

Author
item SHAO, YAPING - University Of Cologne
item NICKLING, WILLIAM - University Of Guelph
item BERGAMETTI, GILLES - University Of Paris
item BUTLER, HARRY - University Of Southern Queensland
item CHAPPELL, ADRAIN - Commonwealth Scientific And Industrial Research Organisation (CSIRO)
item FINDLATER, PAUL - University Of Western Australia
item GILLIES, JOHN - Desert Research Institute
item ISHIZUKA, MASAHIDE - Kagawa University
item KLOSE, MARTINA - University Of Cologne
item KOK, JASPER - University Of California
item LEYS, JOHN - Nsw Department Of Primary Industries
item LU, HUA - University Of Cambridge
item MARTICORENA, BEATRICE - University Of Paris
item MCTAINSH, GRANT - Griffiths University
item NEUMAN, CHERYL - Trent University
item OKIN, GREGORY - University Of California
item STRONG, CRAIG - Canberra
item WEBB, NICHOLAS - New Mexico State University

Submitted to: Aeolian Research
Publication Type: Peer Reviewed Journal
Publication Acceptance Date: 9/7/2015
Publication Date: 11/1/2015
Publication URL: http://handle.nal.usda.gov/10113/61727
Citation: Shao, Y., Nickling, W., Bergametti, G., Butler, H., Chappell, A., Findlater, P., Gillies, J., Ishizuka, M., Klose, M., Kok, J., Leys, J., Lu, H., Marticorena, B., Mctainsh, G., Neuman, C.M., Okin, G., Strong, C., Webb, N. 2015. A tribute to Michael R. Raupach for contributions to aeolian fluid dynamics. Aeolian Research. 19:37-54.

Interpretive Summary: Since the early work of Ralph Bagnold in the 1940s, aeolian research has grown to become a major integral part of earth-system studies. Many individuals have contributed to this development, and Dr. Michael R. Raupach (MR2, 1950 – 2015) was one of the most outstanding. MR2 worked for about a decade (1985 – 1995) intensively on wind erosion problems, but he did so brilliantly by relating aeolian problems to his deep knowledge of turbulence, and made profound contributions to the field with far-reaching influences and a lasting legacy. The beauty of MR2s work is crystal clear conceptual thinking, reducing problems to their essentials and expressing that essence with elegance yet simplicity. The results of his work are robust and practically applicable. In this review we reflect on MR2’s contribution to a number of important aeolian research themes, summarize the developments since his inspirational work and place MR2’s effort in the context of aeolian science. We also demonstrate how MR2’s work provided the foundations for many of the new developments in aeolian new research. In this tribute, we concentrate on MR2’s work in five areas: (1) drag partition theory; (2) saltation roughness length; (3) saltation bombardment; (4) threshold friction velocity; and (5) carbon cycle.

Technical Abstract: Since the early work of Bagnold in the 1940s, aeolian research has grown to become a major integral part of earth-system studies. Many individuals have contributed to this development, and Dr. Michael R. Raupach (MR2, 1950 – 2015) was one of the most outstanding. MR2 worked for about a decade (1985 – 1995) intensively on wind erosion problems, but he did so brilliantly by relating aeolian problems to his deep knowledge of turbulence, and made profound contributions to the field with far-reaching influences and a lasting legacy. The beauty of MR2s work is crystal clear conceptual thinking, reducing problems to their essentials and expressing that essence with elegance yet simplicity. The results of his work are robust and practically applicable. In this review we reflect on MR2’s contribution to a number of important aeolian research themes, summarize the developments since his inspirational work and place MR2’s effort in the context of aeolian science. We also demonstrate how MR2’s work provided the foundations for many of the new developments in aeolian new research. In this tribute, we concentrate on MR2’s work in five areas: (1) drag partition theory; (2) saltation roughness length; (3) saltation bombardment; (4) threshold friction velocity; and (5) carbon cycle.