Orencio Duran Vinent Texas A&M University Department of Ocean Engineering
|
|
|
- Brooke Pamela Cain
- 6 years ago
- Views:
Transcription
1 Orencio Duran Vinent Texas A&M University Department of Ocean Engineering EDUCATION Ph.D MS BS University of Stuttgart, Institute for Computational Physics, Germany Applied Physics, 2007 University of Havana, Department of Theoretical Physics, Cuba Applied Physics, 2003 University of Havana, Cuba Physics, 2000 EMPLOYMENT Research Assistant Professor, Department of Ocean Engineering 2017 Texas A&M University Postdoctoral Research Associate, Department of Physical Sciences Virginia Institute of Marine Sciences Postdoctoral Scholar, MARUM Center for Marine Environmental Sciences University of Bremen, Germany Postdoctoral Scholar, Department of Geological Sciences University of North Carolina Chapel Hill Postdoctoral Scholar, Physique et Mécanique des Milieux Hétérogènes ESPCI ParisTech, France Postdoctoral Scholar, Department of Mechanical Engineering University of Twente, The Netherlands Graduate Student Researcher, Institute for Computational Physics University of Stuttgart, Germany Assistant Professor, Department of Physics Latin American School of Medicine, Cuba PUBLICATIONS Refereed Journal Articles 32. Goldstein EB, Moore LJ & Duran Vinent O (2017) Lateral vegetation growth rates exert control on coastal foredune hummockiness and coalescing time. Earth Surface Dynamics, 5 (3), Pähtz T & Duran O (2017) Fluid forces or impacts: What governs the entrainment of soil particles in sediment transport mediated by a Newtonian fluid? Phys. Rev. Fluids., 2, Moore LJ, Duran Vinent O & Ruggiero P (2016) Vegetation control allows autocyclic formation of multiple dunes on prograding coasts. Geology, 44 (7), Duran Vinent O & Moore LJ (2016) Reply to Bistability and the future of barrier islands. Nature Clim. Change, 6 (1), 6.
2 Orencio Duran Vinent Curriculum Vitae Page! 2 of! Duran Vinent O & Moore LJ (2015) Bistability of barrier islands induced by biophysical interactions. Nature Clim. Change, 5, Pähtz T, Duran O, Ho T-D, Valance A & Kok J (2015) The fluctuation energy balance in nonsuspended fluid-mediated particle transport. Phys. of Fluids, 27 (1), Duran O, Claudin P & Andreotti B (2014) Direct simulations of aeolian sand ripples. Proc. Natl. Acad. Sci. USA, 111 (44), Walters D, Moore LJ, Duran Vinent O, Fagherazzi S & Mariotti G (2014) Interactions between barrier islands and backbarrier marshes affect island system response to sea level rise: Insights from a coupled model. J. Geophys. Res. - Earth Surf., 119, Duran O, Andreotti B & Claudin P (2014) Turbulent and viscous sediment transport a numerical study. Adv. Geosci., 37, Parteli EJR, Duran O, Bourke MC, Tsoar H, Pöschel T & Herrmann HJ (2014) Origins of barchan dune asymmetry: Insights from numerical simulations. Aeolian Res., 12, Duran O & Moore LJ (2013) Vegetation controls on the maximum size of coastal dunes. Proc. Natl. Acad. Sci. USA, 110 (43), Duran O, Andreotti B & Claudin P (2012) Numerical simulations of turbulent sediment transport, from bed load to saltation. Phys. Fluids, 24, Andreotti B, Claudin P, Devauchelle O, Duran O & Fourriere A (2012) Bedforms in a turbulent stream: ripples, chevrons and antidunes. J. Fluid Mech., 690, Duran O, Claudin P & Andreotti B (2011) On aeolian transport: grain-scale interactions, dynamical mechanisms and scaling laws. Aeolian Res., 3, Duran O, Schwämmle V, Lind PG & Herrmann HJ (2011) Size distribution and structure of barchan dune fields. Nonlin. Processes Geophys., 18, Luna MCM, Parteli EJR, Duran O & Herrmann HJ (2011) Model for the genesis of coastal dune fields with vegetation. Geomorphology, 129, Göncü F, Duran O & Luding S (2010) Constitutive relations for the isotropic deformation of frictionless packings of polydisperse spheres. Comptes Rendu Mecanique, 338(10-11), Duran O, Parteli EJR & Herrmann HJ (2010) A continuous model for sand dunes: Review, new developments and application to barchan dunes. Earth Surf. Proc. Land., 35, Duran O, Kruyt N & Luding S (2010) Micro-mechanical analysis of deformation characteristics of three-dimensional granular materials. Int. J Solids Struct., 47, Duran O, Kruyt N & Luding S (2010) Analysis of three-dimensional micro-mechanical strain formulations for granular materials: evaluation of accuracy. Int. J Solids Struct., 47, Parteli EJR, Duran O, Tsoar H, Schwämmle V & Herrmann HJ (2009) Dune formation under bimodal winds. Proc. Natl. Acad. Sci. USA, 106, Duran O, Schwämmle V, Lind PG & Herrmann HJ (2009) The dune size distribution and scaling relations of barchan dune fields. Granular Matter, 11, Parteli EJR, Almeida MP, Duran O, Andrade JSJr & Herrmann HJ (2009) Sand transport on Mars. Computer Physics Communications, 180, Luna MCM, Parteli EJR, Duran O & Herrmann HJ (2009) Modeling transverse dunes with vegetation. Physica A, 388, Duran O, Silva MVN, Bezerra LJC, Herrmann HJ & Maia LP (2008) Measurements and numerical simulations of the degree of activity and vegetation cover on parabolic dunes in north-eastern Brazil. Geomorphology, 102,
3 Orencio Duran Vinent Curriculum Vitae Page! 3 of! 7 7. Herrmann HJ, Duran O, Parteli EJR & Schatz V (2008) Vegetation and induration as sand dunes stabilizators. J. Coastal Res., 24, Parteli EJR, Duran O & Herrmann HJ (2007) Minimal size of a barchan dune. Phys. Rev. E, 75, Parteli EJR, Duran O & Herrmann HJ (2007) Reply to Comment on Minimal size of a barchan dune. Phys. Rev. E, 76, Duran O & Herrmann HJ (2006) Vegetation against dune mobility. Phys. Rev. Lett., 97, Duran O & Herrmann HJ (2006) Modeling of saturated sand flux. J. Stat. Mech. Theory and Experiments, P Duran O, Schwämmle V & Herrmann HJ (2005) Breeding and solitary wave behavior of dunes. Phys. Rev. E, 72, Duran O & Mulet R (2005) Evolutionary prisoner s dilemma in random graphs. Physica D, 208, Manuscripts accepted, in review or submitted Duran Vinent O, Andreotti B, Claudin P & Winter C. A unified model of bedforms across the laminar turbulent transition. Nature Geoscience, in review. Claudin P, Duran O & Andreotti B. Dissolution instability and roughening transition. Journal of Fluid Mechanics, in review. Pähtz T & Duran Vinent O. Unified theory of the cessation of sediment transport mediated by a Newtonian fluid. JGR: Earth Surface, in review. Pähtz T & Duran Vinent O. The reason why sediment transport is analog to sliding friction. Phys. Rev. Lett., in review. Conference proceedings 2013 Duran O, Andreotti B & Claudin P. Turbulent sediment transport a numerical study. Proceedings of the SHF workshop Two-pHase modelling for Sediment dynamics (THESIS), Chatou, France. Duran O, Andreotti B & Claudin P. Numerical simulation of turbulent sediment transport. Fourth international workshop on marine and river dune dynamics (MARID) in Bruges, Belgium, pp V. Van Lancker and T. Garlan editors Andreotti B, Claudin P, Devauchelle O, Duran O & Fourrière A. Bedforms in a turbulent stream: transverse and inclined patterns. Proceedings of the 7th IAHR symposium on River, Coastal and Estuarine Morphodynamics, Tsinghua University, Beijing, China, pp Göncü F, Duran O & Luding S. Jamming in frictionless packings of spheres: determination of the critical volume fraction, Powders and Grains 2009, AIP Conference Proceedings, 1145 (1), Duran O, Schatz V, Herrmann HJ & Tsoar H. Transformation of barchans into parabolic dunes under the influence of vegetation, In R. Garcia-Rojo, H.J. Herrmann & S. McNamara (Eds.), Powders and Grains 2005: Proceedings of the International Conference on Powders & Grains 2005, Stuttgart, Germany, July 2005 (pp )
4 Orencio Duran Vinent Curriculum Vitae Page! 4 of! 7 GRANTS Awarded 2015 The Role of Vegetation in Coastal Response to Sea Level Rise. National Oceanic and Atmospheric Association, Ecological Effects of Sea LevelRise Program, ~$599,550. Lead-PI: P. Ruggiero (OSU), PIs: S. Hacker (OSU) and L. Moore (UNC-CH), Senior Personnel: O. Duran Vinent. Sep. 15, 2015 Sep. 14, Collaborative Research: Exploring the Role of Ecomorphodynamic Feedbacks in Barrier Island Response to Climate Change. National Science Foundation, Geomorphology and Land Use Program, $481,982. Lead-PI: L. J. Moore (UNC-CH), PI: D. Young (VCU), Senior Personnel: O. Duran Vinent (Sep. 15, 2013 Sep. 14, 2016) CONFERENCE ACTIVITY Invited and presented papers 2016 Duran Vinent O & Kirwan ML. Competition between barrier island migration and marsh-upland migration could determine the fate of coastal lagoons under sea level rise. AGU Fall Meeting. (Oral) 2014 Duran Vinent O. Sand transport by wind, erosion and deposition and the origin of aeolian bedforms. EGU General Assembly, Vienna, Austria. (Invited) Duran Vinent O & Moore LJ. Vegetation controls on the maximum size of coastal dunes. EGU General Assembly, Vienna, Austria. (Oral) 2012 Duran Vinent O, Moore LJ & Young D. The role of vegetation in shaping dune morphology, AGU Fall Meeting. (Invited) Duran Vinent O. The role of dune interactions and wind fluctuations in the selection of dune sizes within barchan fields, AGU Fall Meeting. (Invited) Duran Vinent O, Moore LJ & Young D. Modeling the formation of dunes in barrier islands, GSA Annual Meeting. (Oral) 2010 Duran Vinent O, Andreotti B & Claudin P. Emergence of aeolian ripples: direct simulations, actual dynamical mechanisms and scaling laws, AGU Fall Meeting. (Poster) Duran Vinent O, Claudin P & Andreotti B. Aeolian sand transport: numerical evidence of a two species description of the granular flow, 7th International Conference on Aeolian Research (ICAR VII), Santa Rosa, Argentina. (Oral) Duran Vinent O, Claudin P & Andreotti B. Numerical simulations of aeolian sand ripples, 7th International Conference on Aeolian Research (ICAR VII), Santa Rosa, Argentina. (Poster) 2008 Duran O, Parteli EJR & Herrmann HJ. A continuous model for sand dunes and its application to barchan dunes, Marine Sandwave and River Dune Dynamics III, Leeds, UK. (Poster) 2007 Duran O, Schwämmle V, Lind PG & Herrmann HJ. How barchan distributes over desert, EGU General Assembly, Vienna, Austria. (Oral) 2005 Duran O, Schatz V, Herrmann HJ & Tsoar H. Transformation of barchans into parabolic dunes under the influence of vegetation, Powders and Grains 2005, Stuttgart, Germany. (Poster)
5 Orencio Duran Vinent Curriculum Vitae Page! 5 of! 7 Others 2016 Moore LJ, Duran Vinent O, Ruggiero P & Goldstein EB. From stem to crest: Vegetation control on the maximum height, alongshore continuity, number and spacing of coastal foredunes. AGU Fall Meeting (forthcoming). Ruggiero P, Cohn N, Hacker S, Moore LJ, Duran Vinent O & de Vries S. Beach and dune building processes: Linking nearshore to backshore and events to decades. AGU Fall Meeting (forthcoming). Goldstein EB, Moore LJ, devries E, Duran Vinent O & Kenneth ED. Using structure-frommotion data to calibrate a model of coastal dune formation. AGU Fall Meeting (forthcoming). Pähtz T & Duran Vinent O. How common are aeolian processes on planetary bodies with very thin atmospheres? EGU General Assembly. Pähtz T & Duran Vinent O. What causes frictional behavior in fluid-mediated sediment transport? EGU General Assembly. Hoonhout B, Cohn N, de Vries S, Roelvink JA, Ruggiero P, Moore LJ, Duran Vinent O & Goldstein EB. How Tides and Waves Enhance Aeolian Sediment Transport at The Sand Motor. Ocean Sciences Meeting. Moore LJ, Roelvink JA, Ruggiero P, Cohn N, Hoonhout B, Duran Vinent O, Goldstein EB & de Vries S. Crossing the Shoreline Divide: Toward modeling the co-evolution of dune, beach and nearshore systems. Ocean Sciences Meeting. Cohn N, Hoonhout B, Ruggiero P, Moore LJ, de Vries S, Roelvink JA, Duran Vinent O & Goldstein EB. Exploring Nearshore-Beach-Dune Interaction through a Coupled Modeling Framework. Ocean Sciences Meeting Pähtz T & Duran Vinent O. A universal dynamical critical condition controls cessation of sediment transport in fluid. AGU Fall Meeting. Goldstein EB, Moore LJ, devries E, Jass T, Duran Vinent O. Plant Sensitivity to Burial and Coastal Foredune Morphology. AGU Fall Meeting. Moore LJ, Duran Vinent O, Walters DC, Lauzon R, Murray AB & Kirwan ML. Ecomorphodynamic feedbacks and couplings between barrier and back-barrier environments influence holistic system response to changing climate. GSA Annual Meeting Goldstein EB, Moore LJ, Duran Vinent O & Jass TL. Species-Specific Control on Coastal Foredune Morphology along the U.S. East Coast, AGU Fall Meeting. Jass TL, Moore LJ, Young DR, Bruno JF, Duran Vinent O & Goldstein EB. Considering the Different Roles of Ammophila breviligulata and Spartina patens in Coastal Foredune Formation and Growth, AGU Fall Meeting. Moore LJ, Bruno J, Duran Vinent O, Fagherazzi S, Goldstein EB, Jass T, Lauzon R, Mariotti G, Murray AB, Walters D & Young D. Ecomorphodynamic feedbacks and couplings between landscape subsystems influence barrier island response to changing climate, AGU Fall Meeting. Walters D, Moore LJ, Duran Vinent O, Fagherazzi S, Mariotti G & Kirwan M. How much is too much: The impact of overwash deposition on back-barrier marsh vegetation. GSA Abstracts with Programs, Vol. 46, no.6. Duran Vinent O, Claudin P & Andreotti B. Direct simulations of aeolian sand ripples, 8th International Conference on Aeolian Research (ICAR VIII), Lanzhou, China.
6 Orencio Duran Vinent Curriculum Vitae Page! 6 of! Moore LJ & Duran Vinent O. Barriers on the brink? Interactions between biological and physical processes lead to bistability and the potential for rapid response to gradually changing conditions, AGU Fall Meeting. (Invited) Moore LJ, Duran Vinent O, Walters D, Young D, Fagherazzi S & Mariotti G. Ecomorphodynamic feedbacks determine barrier island response to climate change, 8th IAG International conference in geomorphology, Paris, France Moore LJ, Duran Vinent O, Walters D, Fagherazzi S, Mariotti G, Young D, Wolner CV. Biological-physical feedbacks determine coastal environmental response to climate change, AGU Fall Meeting. (Invited) Moore LJ, Duran Vinent O & Young D. The role of ecomorphodynamics in barrier island response to climate change, AGU Fall Meeting. Walters D, Moore LJ, Duran Vinent O, Mariotti G & Fagherazzi S. Modeling Dynamic interactions and feedbacks between barrier islands and fringing back-barrier marshes, GSA Annual Meeting. Walters D, Moore LJ, Duran Vinent O, Mariotti G & Fagherazzi S. Dynamic interactions and feedbacks between barrier and back-barrier environments and their role in barrier-marsh coevolution, AGU Fall Meeting Göncü F, Duran O & Luding S. Jamming in frictionless packings of spheres: determination of the critical volume fraction, Powders and Grains 2009, Golden, USA Parteli EJR, Almeida MP, Duran O, Andrade JSJr & Herrmann HJ. Sand transport on Mars, Conference on Computational Physics, Ouro Preto, Brazil Parteli EJR, Duran O & Herrmann HJ. The shape of Barchan dunes in the Arkhangelsky Crater on Mars, Lunar and Planetary Science Conference XXXVII, Lunar and Planetary Institute, Houston. INVITED TALKS 2013 Granular flows: from wind ripples formation to coastal vulnerability. Deutsches GeoForschungsZentrum, Postdam, Germany. From grains to bedforms: direct numerical simulations of aeolian ripples. Workshop on numerical modeling of grains/fluid flows, ENS de Lyon, France. Vegetation controls on the maximum size of coastal dunes. University of Twente, Water Engineering & Management Group, The Netherlands Coastal eco-morphodynamics. Duke University, Nicholas School of the Environment, Earth and Ocean Sciences, USA Modeling dune formation and evolution. Politecnico di Milano, Modeling and Scientific Computing Lab, Italy Dune morphodynamic: from single dunes to dune fields. University Carlos III, Modeling and Numerical Simulation Institute, Madrid, Spain Collective genesis of sand dunes. University of Lisbon, Center for Theoretical and Computational Physics, Lisbon, Portugal Modeling dune formation and evolution. National research center for mathematics and computer science, The Netherlands.
7 Orencio Duran Vinent Curriculum Vitae Page! 7 of! 7 PROFESSIONAL AND COMMUNITY SERVICE Editor: Earth Surface Dynamics, Associate Editor, 2015 present. Open Source Models: Coastal Dune Model (CDM). Uploaded to the Community Surface Dynamic Modeling System (CSDMS), doi: /zenodo Member: American Geophysical Union, 2010 present. European Geoscience Union, 2013 present. Coastal Working Group Member, Community Surface Dynamics Modeling System (CSDMS), 2011 present. Manuscript Reviewer: Physics of Fluid, Earth Surface Dynamics, Geophysical Research Letters, Journal of Geophysical Research, Geology, Geomorphology, Physical Review Letters, Aeolian Research, Scientific Reports, Physical Review E, Europhysics Letters, European Physical Journal E, Granular Matter.
Morphodynamic modeling of aeolian sediment landscapes with regard to the stabilization of shifting sands
Morphodynamic modeling of aeolian sediment landscapes with regard to the stabilization of shifting sands Eric J. R. Parteli 1, Orencio Durán 2, Hans Herrmann 3, Haim Tsoar 4 1. Institute for Multiscale
Transformation of barchans into parabolic dunes under the influence of vegetation
Transformation of barchans into parabolic dunes under the influence of vegetation arxiv:cond-mat/0504621 v1 25 Apr 2005 Abstract O. Durán, V. Schatz, H. J. Herrmann Institute for Computer Physics, Universität
How does sand move on Mars?
How does sand move on Mars? Possible solutions to some long-standing mysteries Jasper F. Kok Department of Atmospheric and Oceanic Sciences, UCLA jfkok@ucla.edu Main collaborators: Thomas Pähtz, Hezi Yizhaq,
Analytical Mesoscale Modeling of Aeolian Sand Transport
Analytical Mesoscale Modeling of Aeolian Sand Transport Marc Lämmel, Anne Meiwald, Klaus Kroy GeoFlo16 Dresden Aeolian Sand Transport Mesoscale Process potentially amenable to analytical modeling Mean-Field
Aqueous and Aeolian Bedforms
Aqueous and Aeolian Bedforms 1 Further reading & review articles R.A. Bagnold, 1941, The physics of blown sand and desert dunes Charru et al., 2013, Sand ripples and dunes, Ann. Review of Fluid Mech. 2
PROCESS-BASED MODELING OF COASTAL DUNE DEVELOPMENT
PROCESS-BASED MODELING OF COASTAL DUNE DEVELOPMENT Martijn Muller 1, Dano Roelvink 23, Arjen Luijendijk 12, Sierd de Vries 1 and Jaap van Thiel de Vries 12 In this paper, the aeolian transport model DUNE
Quantifying effects of oil on coastal dune vegetation. Thomas Miller and Elise Gornish Biological Science, Florida State University
Quantifying effects of oil on coastal dune vegetation Thomas Miller and Elise Gornish Biological Science, Florida State University Natural History of Barrier Islands in the Northern Gulf Make up ~70% of
Dunes Growth Estimation for Coastal Protection
Dunes Growth Estimation for Coastal Protection Muhammad Zikra Department of Ocean Engineering, Faculty of Marine Technology, ITS, Kampus ITS Keputih Sukolilo, Surabaya 60111 Abstract: This paper describes
Simulations of binary collisions of barchan dunes: the collision dynamics and its influence on the dune size distribution
Simulations of binary collisions of barchan dunes: the collision dynamics and its influence on the dune size distribution Orencio Durán Institute for Computational Physics, University of Stuttgart, 70569
Calculation of the separation streamlines of barchans and transverse dunes
Calculation of the separation streamlines of barchans and transverse dunes H. J. Herrmann a,b, J. S. Andrade Jr. b, V. Schatz a, G. Sauermann a and E. J. R. Parteli a a ICP, University of Stuttgart, Pfaffenwaldring
RESEARCH INTERESTS and EXPERTISE EDUCATION
{ Patrick Wayland Limber Post-doctoral Associate University of Florida Department of Geological Sciences 241 Williamson Hall Gainesville, FL 32611 plimber@ufl.edu Website: plaza.ufl.edu/plimber RESEARCH
Modelization of saturated sand flux
Modelization of saturated sand flux O. Durán 1 and H. Herrmann 1, 1 Institute for Computer Physics, University of Stuttgart, 7569 Stuttgart, Germany. Departamento de Física, Universidade Federal do Ceará,
This is an author-deposited version published in : Eprints ID : 10568
Open Archive TOULOUSE Archive Ouverte (OATAO) OATAO is an open access repository that collects the work of Toulouse researchers and makes it freely available over the web where possible. This is an author-deposited
Genesis of coastal dune fields with vegetation
Genesis of coastal dune fields with vegetation Marco C. M. de M. Luna a,, Eric J. R. Parteli b,c, Orencio Durán d, Hans J. Herrmann a,c,e a Departamento de Física, Universidade Federal do Ceará - 60455-760,
Reply to Comment on Minimal size of a barchan dune
Reply to Comment on Minimal size of a barchan dune E. J. R. Parteli 1, O. Durán 2 and H. J. Herrmann 3,4 1. Institut für Computerphysik, ICP, Universität Stuttgart, Pfaffenwaldring 27, 70569 Stuttgart,
GEO 433/533: Winter 2009 Coastal Geomorphology
GEO 433/533: Winter 2009 Coastal Geomorphology Instructor: Office Hrs: Lectures/Credits: Peter Ruggiero 541-737-1239 Wilkinson 134 ruggierp@geo.oregonstate.edu Flexible email for an appointment The course
GRANULAR MEDIA. Between Fluid and Solid
GRANULAR MEDIA Between Fluid and Solid Sand, rice, sugar, snow,cement...although ubiquitous in our daily lives, granular media still challenge engineers and fascinate researchers. This book provides the
Ripple Morphodynamics in Wave-Current Boundary-Layer Flows
Ripple Morphodynamics in Wave-Current Boundary-Layer Flows Marcelo H. García Department of Civil and Environmental Engineering University of Illinois at Urbana-Champaign 205 North Mathews Avenue Urbana,
Sand transport over a barchan dune
Sand transport over a barchan dune F. Charru (1), V. Laval (1) 1. IMFT, Toulouse, France - corresponding author: francois.charru@imft.fr Abstract The present work investigates an important and yet unsolved
XBeach modeling at various temporal and spatial scales
//oss.deltares.nl/web/xbeach XBeach modeling at various temporal and spatial scales Ad Reniers, RSMAS, UM : Impact of time and process scales XBeach modeling concepts avalanching dune Wave groups c g Bound
Curriculum Vitae. Jianhua Lu
Curriculum Vitae Jianhua Lu Research Faculty I Center for Ocean-Atmospheric Prediction Studies Florida State University Tallahassee, FL32306 Phone: (850) 345-7299; Fax: (850) 644-4841 Email: jlu@coaps.fsu.edu
ANASTASIA PILIOURAS Speedway Stop C
ANASTASIA PILIOURAS 2275 Speedway Stop C9000 845-891-3988 Austin, TX 78712 anastasia.piliouras@gmail.com EDUCATION 2011-present PhD Candidate, Jackson School of Geosciences, University of Texas at Austin
University of Waterloo, Waterloo, Ontario, Canada Doctor of Philosophy (Applied Mathematics) 2015
Sina Khani, Ph.D. Program in Atmospheric & Oceanic Sciences Princeton University Princeton, New Jersey 08544, USA email: web: skhani@princeton.edu scholar.princeton.edu/sinakhani Education University of
Curriculum Vitae. Ivana Cerovečki
Curriculum Vitae Ivana Cerovečki University of California, San Diego Scripps Institution of Oceanography Physical Oceanography Research Division 9500 Gilman Dr. La Jolla, CA 92093-0230 E-mail: icerovec@ucsd.edu
Phillip Island Nature Parks Coastal Process Study 8 October 2014
Phillip Island Nature Parks Coastal Process Study 8 October 2014 Project Overview Coastal Geology Basaltic and fragmented lavas, granite at Pyramid Rock and Cape Woolamai Weathered basalt (>10m thick)
GLY Coastal Geomorphology Notes
GLY 4734 - Coastal Geomorphology Notes Dr. Peter N. Adams Spring 2011 2 Coastal Classification In this lecture, we discuss some successful classification schemes of the coastal landscape, and pay particular
M.S.E. Johns Hopkins University, Applied MathematicsandStatistics,
PERSONAL DETAILS Name Email Qian Zhang qzhang@umces.edu RESEARCH INTERESTS Statistical analysis and synthesis of water-quality monitoring data to guide watershed management Improvement of statistical methods
arxiv: v1 [physics.flu-dyn] 27 Aug 2016
![arxiv: v1 [physics.flu-dyn] 27 Aug 2016](/thumbs/75/72215152.jpg "arxiv: v1 [physics.flu-dyn] 27 Aug 2016")
Morphology and displacement of dunes in a closed-conduit flow, arxiv:1608.07729v1 [physics.flu-dyn] 27 Aug 2016 E.M. Franklin, F. Charru Institut de Mécanique des Fluides de Toulouse, Allée du Pr. Camille
CURRICULUM VITAE (As of June 03, 2014) Xuefei Hu, Ph.D.
CURRICULUM VITAE (As of June 03, 2014) Xuefei Hu, Ph.D. Postdoctoral Fellow Department of Environmental Health Rollins School of Public Health Emory University 1518 Clifton Rd., NE, Claudia N. Rollins
EARTH SURFACE PROCESSES AND SEDIMENTATION!
Sed and Strat EARTH SURFACE PROCESSES AND SEDIMENTATION! 2/27 Lecture 7- Exposure: Weathering and the Sediment Factory 3/04 Lecture 8 - Rivers and Landscapes 3/06 Lecture 9 - Waves (not Tides) 3/11 Lecture
Tieyuan Zhu Postdoctoral Fellow, Jackson School of Geosciences, the University of Texas at Austin Mail address: Telephone: Website:
Postdoctoral Fellow, Jackson School of Geosciences, the University of Texas at Austin Mail address: Telephone: Email: Website: 10100 Burnet Rd. #130, Austin TX 01-650- 308-6506 tzhu@jsg.utexas.edu http://www.jsg.utexas.edu/tyzhu/
2.2.7 Backbarrier flats
FIGURE 24. VERTICAL PHOTOGRAPH SHOWING THE DEVELOPMENT OF SMALL PARABOLIC DUNES FROM BLOWOUTS IN A LARGE RELICT FOREDUNE NORTHWEST OF HUNTER'S CREEK. PHOTOGRAPH COURTESY OF CAR'T'ER HOLT HARVEY FORESTS
Difference in the wind speeds required for initiation versus continuation of sand transport on Mars: Implications for dunes and dust storms
Difference in the wind speeds required for initiation versus continuation of sand transport on Mars: Implications for dunes and dust storms Jasper F. Kok 1,2,* 1 Department of Atmospheric, Oceanic, and
Curriculum Vitae: Chunsong Lu
Curriculum Vitae: Chunsong Lu PERSONAL INFORMATION Address Room 1005, Qixiang Bldg, No. 219, Ningliu Road, Nanjing, Jiangsu, China 210044 Email luchunsong110@163.com; luchunsong110@gmail.com Cell Phone
Transport capacity and saturation mechanism in a real-space cellular automaton dune model
Manuscript prepared for Adv. Geosci. with version 5. of the L A TEX class copernicus.cls. Date: 5 January 4 Transport capacity and saturation mechanism in a real-space cellular automaton dune model X.
Mid-air collisions enhance saltation
Mid-air collisions enhance saltation M. V. Carneiro1, N. A. M. Arau jo1, T. Pa htz,, and H. J. Herrmann1,4 1 Institut fu r Baustoffe, ETH-Ho nggerberg, Schafmattstrasse 6, 809 Zu rich, Switzerland Department
National Center for Earth-surface Dynamics: Renesse 2003: Non-cohesive Sediment Transport
Introduction to Morphodynamics For the original references on the work of Exner see Graf, W., 1971, Hydraulics of Sediment Transport, McGraw Hill, New York, 513 p. Sediment Properties Dietrich, E. W.,
Anticipation guide # 3
Wind Anticipation guide # 3 Creep is a type of mass movement that happens slowly over many years Oxidation is a type of physical weathering A delta is a depositional feature that occurs with glaciers The
COASTAL EVOLUTION AND CLIMATE CHANGE: CHALLENGES OF MULTI-SCALE SPATIAL AND TEMPORAL VARIABILITY
COASTAL EVOLUTION AND CLIMATE CHANGE: CHALLENGES OF MULTI-SCALE SPATIAL AND TEMPORAL VARIABILITY Dr. Jennifer L. Miselis Naval Research Laboratory Stennis Space Center, MS jmiselis@nrlssc.navy.mil 1 PRIMARY
Timothy Titus, USGS James Zimbelman, SI Jani Radebaugh, BYU
Timothy Titus, USGS James Zimbelman, SI Jani Radebaugh, BYU 10/29/2015 VEXAG 2 Increase the cross-talk and collaborations between Terrestrial Aeolian Scientists Planetary Aeolian Scientists Multiple Disciplines
Eolian Landscapes and Deposits
1 Eolian Landscapes and Deposits Relevant differences in air versus water as the transporting fluid ρwater ρair 800 density µ water µ air 55 dynamic viscosity Good match between present-day distribution
Patrick Hesp. Department of Geography and Anthropology, Louisiana State University
Patrick Hesp Department of Geography and Anthropology, Louisiana State University Incipient ( embryo ) Foredunes - new, or developing foredunes formed by aeolian sand deposition within pioneer plant communities
Australian Coastal Councils Conference
Australian Coastal Councils Conference 11 March 2015 Estimating Future Coastal Inundation and Erosion Hazards Dr Andrew McCowan Dr Christine Lauchlan-Arrowsmith Warwick Bishop Background Victorian Future
Research Background: Researcher Sam Bond taking Sediment Elevation Table (SET) measurements in the marsh. A view of salt marsh hay growing in a marsh
Name Keeping up with the sea level Featured scientist: Anne Giblin from the Marine Biological Laboratory and the Plum Island Ecosystems Long-Term Ecological Research site Research Background: Salt marshes
Minimal size of a barchan dune
Minimal size of a barchan dune E. J. R. Parteli 1, O. Durán 1 and H. J. Herrmann 2,3 1. Institut für Computerphysik, ICP, Universität Stuttgart, Pfaffenwaldring 27, 7569 Stuttgart, Germany. 2. Institut
The rate and fate of coastal carbon burial
The rate and fate of coastal carbon burial Matthew L. Kirwan, Virginia Institute of Marine Science Main Points Marsh size Marsh accretion 1. SLR drives wetland carbon burial in vertical and lateral dimensions
Talks. December 2011.
Talks Oliveira, J.S., Langlais, B., Amit, H., Pais, M.A., Modeling the magnetic field of Mercury using the Time Dependent Equivalent Source Dipole method. European Geosciences Union, Vienna, Austria, April
arxiv: v1 [cond-mat.soft] 24 Apr 2013
![arxiv: v1 [cond-mat.soft] 24 Apr 2013](/thumbs/89/98499551.jpg "arxiv: v1 [cond-mat.soft] 24 Apr 2013")
Barchan dune asymmetry: Numerical investigation Eric J. R. Parteli a,, Orencio Durán b, Mary C. Bourke c,d, Haim Tsoar e, Thorsten Pöschel a, Hans J. Herrmann f,g a Institut für Multiscale Simulation,
2/23/2009. Visualizing Earth Science. Chapter Overview. Deserts and Drylands. Glaciers and Ice Sheets
Visualizing Earth Science By Z. Merali and B. F. Skinner Chapter 6 Deserts, Glaciers and Ice Sheets Chapter Overview Deserts and Drylands Glaciers and Ice Sheets Deserts Geography Categorization of deserts
The dune size distribution and scaling relations of barchan dune fields
Granular Matter (29) :7 DOI.7/s35-8-2-4 The dune size distribution and scaling relations of barchan dune fields Orencio Durán Veit Schämmle Pedro G. Lind Hans J. Herrmann Received: 9 May 28 / Published
GD3.3/GM3.3/GMPV16/TS4.7
GM Geomorphology Orals and PICOs MO1, 08:30 10:00 MO2, 10:30 12:00 MO3, 13:30 15:00 MO4, 15:30 17:00 MO5, 17:30 19:00 TU1, 08:30 10:00 TU2, 10:30 12:00 TUL, 12:15 13:15 TU3, 13:30 15:00 Monday, 08 April
Predicting the Evolution of Tidal Channels in Muddy Coastlines
Predicting the Evolution of Tidal Channels in Muddy Coastlines Sergio Fagherazzi Department of Earth Sciences and Center for Computational Science Boston University, Boston MA 02215 Phone: (617) 353-2092
Coastal Barrier Island Network (CBIN): Management strategies for the future
Coastal Barrier Island Network (CBIN): Management strategies for the future Heather Joesting*, Amy Williams**, Rusty Feagin**, and William K. Smith* *Department of Biology, Wake Forest University, Winston
Sand Ripple Dynamics on the Inner Shelf
Sand Ripple Dynamics on the Inner Shelf Donald N. Slinn Department of Civil and Coastal Engineering, University of Florida Gainesville, FL 32611-6590, Phone: (352) 392-9537 x 1431 Fax: (352) 392-3466 E-mail:
Geol 117 Lecture 18 Beaches & Coastlines. I. Types of Coastlines A. Definition:
I. Types of Coastlines A. Definition: 1. Shore = narrow zone where ocean meets land (e.g. beach) 2. Coast is a broad area where both ocean and land processes act a. Includes onshore marshes, dunes, sea
arxiv:cond-mat/ v2 [cond-mat.soft] 19 May 2011
![arxiv:cond-mat/ v2 [cond-mat.soft] 19 May 2011](/thumbs/83/88521679.jpg "arxiv:cond-mat/ v2 [cond-mat.soft] 19 May 2011")
Manuscript prepared for Nonlin. Processes Geophys. with version 3. of the L A TEX class copernicus.cls. Date: May Size distribution and structure of Barchan dune fields arxiv:cond-mat/737v [cond-mat.soft]
KOROSH TORABI. Ph.D. Chemical Engineering, Purdue University, West Lafayette, IN Dec. 2011
KOROSH TORABI 2 7 2 5 C E N T R A L S T. A P T 2 S E V A N S T O N, I L 6 0 2 0 1 P H O N E ( 3 1 2 ) 3 3 9-0 6 6 5 E - M A I L : K O R O S H. T O R A B I @ N O R T H W E S T E R N. E D U W E B P A G E
Submarine sand ripples formation in a viscous fluid: 2D and 3D linear stability analysis
Marine Sandwave and River Dune Dnamics 1 & April 4 - Enschede, the Netherlands Submarine sand ripples formation in a viscous fluid: D and 3D linear stabilit analsis V. Langlois (1) and A. Valance (1) Groupe
Page 1 of 9 Name: Base your answer to the question on the diagram below. The arrows show the direction in which sediment is being transported along the shoreline. A barrier beach has formed, creating a
Signals of sea-level rise in Delaware and Chesapeake Bay tides
Signals of sea-level rise in Delaware and Chesapeake Bay tides Andrew C. Ross and Raymond G. Najjar Pennsylvania State University Also thanks to Ming Li, Serena Lee, Fan Zhang, Wei Liu Observations show
Transverse instability of dunes
Transverse instability of dunes Eric J. R. Parteli 1,2, José S. Andrade Jr. 1, and Hans J. Herrmann 1,3 1. Departamento de Física, Universidade Federal do Ceará - 60455-760, Fortaleza, Ceará, Brazil. 2.
Sediment and Sedimentary rock
Sediment and Sedimentary rock Sediment: An accumulation of loose mineral grains, such as boulders, pebbles, sand, silt or mud, which are not cemented together. Mechanical and chemical weathering produces
Peter Gaube EDUCATION
Peter Gaube Applied Physics Laboratory Department of Air-Sea Interaction and Remote Sensing (AIRS) Box 355640 University of Washington 1013 NE 40th Street Seattle, WA 98105-6698 (520) 248-1939 pgaube@apl.washington.edu
EOLIAN PROCESSES & LANDFORMS
EOLIAN PROCESSES & LANDFORMS Wind can be an effective geomorphic agent under conditions of sparse vegetation & abundant unconsolidated sediment egs. hot & cold deserts, beaches & coastal regions, glacial
FUTURE MEANDER BEND MIGRATION AND FLOODPLAIN DEVELOPMENT PATTERNS NEAR RIVER MILES 200 TO 191 OF THE SACRAMENTO RIVER
FUTURE MEANDER BEND MIGRATION AND FLOODPLAIN DEVELOPMENT PATTERNS NEAR RIVER MILES 200 TO 191 OF THE SACRAMENTO RIVER Eric W. Larsen University of California, Davis With the assistance of Evan Girvetz
John Breier. CURRICULUM VITAE 28 August 2007 ADDRESS AND TELEPHONE
CURRICULUM VITAE 28 August 2007 John Breier ADDRESS AND TELEPHONE Woods Hole Oceanographic Institution Applied Ocean Physics & Engineering 266 Woods Hole Road Blake Building, Room 200 Woods Hole, MA, 02543
CURRICULUM VITAE. Woods Hole Oceanographic Institution, Woods Hole, Massachusetts USGS Postdoctoral Scholar
CURRICULUM VITAE Andrew Dale Ashton Coastal Geomorphologist Assistant Scientist Geology and Geophysics Department Clark 257 Woods Hole Oceanographic Institution Woods Hole, MA 02543 Telephone: (508) 289-3751
Jun Cheng School of Geosciences, University of South Florida 4202 E. Fowler Ave., NES 117, Tampa, FL 33620
EDUCATION Jun Cheng 4202 E. Fowler Ave., NES 117, Tampa, FL 33620 Phone: 813-974-2759 Email: jun@mail.usf.ed University of South Florida (Tampa, FL) Ph.D. in Geology, 2015 Dissertation: Multiple Scale
Bob Van Dolah. Marine Resources Research Institute South Carolina Department of Natural Resources
Bob Van Dolah Marine Resources Research Institute South Carolina Department of Natural Resources Shoreline Change Will Occur! On our front beaches where it is not easy to retreat Shoreline Change Will
BERZI DIEGO PERSONAL DETAILS EDUCATION TEACHING AND RESEARCH INTERESTS TEACHING EXPERIENCE
BERZI DIEGO Dept. of Civil and Environmental Engineering Politecnico di Milano piazza Leonardo da Vinci 32 20133 Milano, Italy +39 0223996262 diego.berzi@polimi.it PERSONAL DETAILS Nationality: Italian
EXTERNAL LAND FORMING PROCESSES
NAME SCHOOL INDEX NUMBER DATE EXTERNAL LAND FORMING PROCESSES WEATHERING 1 1998 Q 7 (a) (i) What is the difference between weathering and mass wasting (ii) List five processes involved in chemical weathering
Lab 7: Sedimentary Structures
Name: Lab 7: Sedimentary Structures Sedimentary rocks account for a negligibly small fraction of Earth s mass, yet they are commonly encountered because the processes that form them are ubiquitous in the
NAME: GEL 109 Final Study Guide - Winter 2008 Questions 6-24 WILL be on the final exactly as written here; this is 60% of the test.
GEL 109 Final Study Guide - Winter 2008 Questions 6-24 WILL be on the final exactly as written here; this is 60% of the test. 1. Sketch a map view of three types of deltas showing the differences in river,
Developed in Consultation with Florida Educators
Developed in Consultation with Florida Educators Table of Contents Next Generation Sunshine State Standards Correlation Chart... 7 Benchmarks Chapter 1 The Practice of Science...................... 11
Coastal Evolution in Sedimentary Areas in Greenland
Coastal Evolution in Sedimentary Areas in Greenland Mette Bendixen P h D s t u d e n t DANCORE Young Professionals Day Dias 1 Outline Motivation State of the art on Arctic coasts Purpose of my Phd Presentation
GY 402: Sedimentary Petrology
UNIVERSITY OF SOUTH ALABAMA GY 402: Sedimentary Petrology Lecture 5: Bedform Development (Flume Studies) Instructor: Dr. Douglas W. Haywick Today s Lecture 1. What s a flume? 2. Traction induced bed forms
Via Sante Vincenzi, n. 47 Voice: (+39) Bologna (BO) Italy
CURRICULUM VITAE ET STUDIORUM Dr. Giovanni Conti Contact Information Via Sante Vincenzi, n. 47 Voice: (+39) 3297739069 40138 Bologna (BO) Italy E-mail: giovanni.conti83@gmail.com E-mail: giovanni.conti83@pec.it
Vineel Yettella Curriculum Vitae (updated Nov 2017)
Vineel Yettella Curriculum Vitae (updated Nov 2017) ORCID: 0000-0002-9425-9130 Department of Atmospheric and Oceanic Sciences (ATOC) University of Colorado Boulder 311 UCB, Boulder, CO 80309-0311 Email:
Process-based Modeling of Coastal Dune Development M.Sc. Thesis
Process-based Modeling of Coastal Dune Development M.Sc. Thesis Author: M.C. Muller August, 11 Process-Based Modeling of Coastal Dune Development M.C.Muller Deltares, 11 Process-Based Modeling of Coastal
Flux saturation length of sediment transport
Flux saturation length of sediment transport Thomas Pähtz 1,2, Jasper F. Kok 3, Eric J. R. Parteli 4 and Hans J. Herrmann 5,6 1. Department of Ocean Science and Engineering, Zhejiang University, 3158 Hangzhou,
Coastal Working Group, and Coastal Vulnerability Initiative
Coastal Working Group, and Coastal Vulnerability Initiative Because the goals and activities of the Coastal Working Group (WG) and the Coastal Vulnerability Initiative (CV) overlap, we are reporting on
Quantifying Coastal Evolution using Remote Sensing Approaches
Quantifying Coastal Evolution using Remote Sensing Approaches Sojan Mathew, Linh Truong Hong, Xavier Pellicer*, Colman Gallagher University College Dublin Geological Survey of Ireland* INFOMAR SEMINAR,
1 Shoreline Landforms 2. 2 Emergent v. Submergent 2. 3 Wavecutting 3. 4 Planview 4. 5 Marine Terraces 5. 6 California 7. 7 Tombolos, Sea Stacks 8
Shorelines November 9, 2008 Contents 1 Shoreline Landforms 2 2 Emergent v. Submergent 2 3 Wavecutting 3 4 Planview 4 5 Marine Terraces 5 6 California 7 7 Tombolos, Sea Stacks 8 8 Active Processes 9 9 Emergence
Monitoring the atmospheric dust on Mars: the MicroMED sensor
Monitoring the atmospheric dust on Mars: the MicroMED sensor Exomars Atmospheric Science and Missions Workshop Saariselka, Finland, 26-30 March 2017 F. Esposito(1), C.Molfese(1), F.Cozzolino(1), F.Cortecchia(2),
The Coast: Beaches and Shoreline Processes
1 2 3 4 5 6 7 8 9 The Coast: es and Shoreline Processes Trujillo & Thurman, Chapter 10 Oceanography 101 Chapter Objectives Recognize the various landforms characteristic of beaches and coastal regions.
Holocene dune reactivation along the northern Curonian Spit: geological, paleoecological, and archaeological implications
Holocene dune reactivation along the northern Curonian Spit: geological, paleoecological, and archaeological implications Ilya Buynevich Temple University (USA) Collaborators: Albertas Bitinas Donatas
Modelling Aeolian Agro-Environmental Landscape Dynamics
Innovation of Models across Agro-Environmental Scales: Modelling Aeolian Agro-Environmental Landscape Dynamics Andreas Baas Department of Geography King s College London thanks to: Aeolian Agro-Environmental
SUPPLEMENTARY INFORMATION
SUPPLEMENTARY INFORMATION DOI: 10.1038/NCLIMATE1664 Climate-change impact assessment for inlet-interrupted coastlines ROSHANKA RANASINGHE 1,2,3*, TRANG MINH DUONG 1,3, STEFAN UHLENROOK 1,2, DANO ROELVINK
The Coast: Beaches and Shoreline Processes Trujillo & Thurman, Chapter 10
The Coast: es and Shoreline Processes Trujillo & Thurman, Chapter 10 Oceanography 101 Chapter Objectives Recognize the various landforms characteristic of beaches and coastal regions. Identify seasonal
Size distribution and structure of Barchan dune fields
Manuscript prepared for Nonlin. Processes Geophys. with version 3. of the L A TEX class copernicus.cls. Date: 5 July Size distribution and structure of Barchan dune fields Orencio Durán, Veit Schwämmle,
Collision of barchan dunes as a mechanism of size regulation
GEOPHYSICAL RESEARCH LETTERS, VOL. 32, L21403, doi:10.1029/2005gl024179, 2005 Collision of barchan dunes as a mechanism of size regulation Pascal Hersen 1,2 and Stéphane Douady 2 Received 26 July 2005;
Using a Near-Bed Sediment Flux Sensor to Measure Wave Formed Bedform Migrations and Formation Processes
Using a Near-Bed Sediment Flux Sensor to Measure Wave Formed Bedform Migrations and Formation Processes Peter A. Traykovski Woods Hole Oceanographic Institution Woods Hole, MA 02543 1Tel.: (508) 289-2638,
Google Mars: Wind Processes
Google Mars: Wind Processes This assignment will require the use of the latest version of Google Earth (version 5.0 or later), which you can download for free from http://earth.google.com. You must have
1 Shoreline Erosion and Deposition
CHAPTER 12 1 Shoreline Erosion and Deposition SECTION Agents of Erosion and Deposition BEFORE YOU READ After you read this section, you should be able to answer these questions: What is a shoreline? How
Curriculum Vitae. Golomb Visiting Assistant Professor of Mathematics at Purdue University
Dan Li Curriculum Vitae Contact Information Department of Mathematics, Purdue University 150 N. University Street, West Lafayette, IN, USA 47907-2067 Email: li1863@math.purdue.edu Phone: +1 (765) 494-1948
Coastal Foredune Evolution, Part 2: Modeling Approaches for Meso-Scale Morphologic Evolution
Coastal Foredune Evolution, Part 2: Modeling Approaches for Meso-Scale Morphologic Evolution by Margaret L. Palmsten 1, Katherine L. Brodie 2, and Nicholas J. Spore 2 PURPOSE: This Coastal and Hydraulics
Mapping of Future Coastal Hazards. for Southern California. January 7th, David Revell, Ph.D. E.
Mapping of Future Coastal Hazards for Southern California January 7th, 2014 David Revell, Ph.D. drevell@esassoc.com E. Vandebroek, 2012 Outline Coastal erosion hazard zones Flood hazard zones: Coastal
Optics, Acoustics and Stress in Situ (OASIS)
DISTRIBUTION STATEMENT A. Approved for public release; distribution is unlimited. Optics, Acoustics and Stress in Situ (OASIS) John H. Trowbridge 1 and Peter Traykovski 2 Woods Hole Oceanographic Institution
THE INFLUENCE OF WASHOVER DIMENSIONS AND BEACH CHARACTERISTICS ON THE SEDIMENT TRANSPORT DURING INUNDATION. Abstract
THE INFLUENCE OF WASHOVER DIMENSIONS AND BEACH CHARACTERISTICS ON THE SEDIMENT TRANSPORT DURING INUNDATION Daan Wesselman 1, Maarten van der Vegt 1 and Renske de Winter 1 Abstract Barrier islands need
Peruvian Transverse Dunes in the Google Earth Images
Peruvian Transverse Dunes in the Google Earth Images Amelia Carolina Sparavigna To cite this version: Amelia Carolina Sparavigna. Peruvian Transverse Dunes in the Google Earth Images. Philica, Philica,