Heidi Margaret Nepf | |
---|---|
Alma mater | Stanford University |
Scientific career | |
Thesis | The production and mixing effects of Langmuir circulations (1992) |
Heidi Nepf is an American engineer known for her research on fluid flows around aquatic vegetation.
Nepf has a B.S. from Bucknell University (1987) and an M.S. from Stanford University (1988). [1] Nepf earned a Ph.D. in Civil Engineering from Stanford University in 1992 with a dissertation titled "The production and mixing effects of Langmuir circulations". [2] Following her Ph.D., Nepf was a postdoctoral scholar at Woods Hole Oceanographic Institution, and then joined the faculty of Massachusetts Institute of Technology in 1993. [3] As of 2021, she is the Donald and Martha Harleman Professor at Massachusetts Institute of Technology.
In 2018, Nepf was named a fellow of the American Geophysical Union and the citation reads: [4]
For seminal contributions to the theory, modeling, and environmental applications of flow and transport through aquatic vegetation.
Nepf is known for her research on the flow of water around aquatic vegetation. In 1999, she developed a model describing how aquatic plants convert kinetic energy into turbulent energy. [5] She has furthered this research by examining the flow of water around plants [6] [7] and characterizing sediment flow through coastal marshes and mangroves. [8] [9] Using artificial seagrass beds, Nepf and her graduate student Judy Yang determined that turbulence is a good predictor of sediment flow through a seagrass bed. [10] [11] Nepf and another graduate student, Jiarui Lei, used similar artificial seagrass reefs to quantify the dissipation of energy by seagrass [12] [13] and their results indicate seagrass can protect coastlines that are vulnerable to erosion. [14] [15] Nepf's research on water flow around logjams [16] informs river restoration projects by theoretically describing the flow of water around wood placed into a stream. [17] Nepf has also worked on fluid flows in urban regions, specifically on how capturing storm water can be used to control urban flood damage. [18] [19]
The hyporheic zone is the region of sediment and porous space beneath and alongside a stream bed, where there is mixing of shallow groundwater and surface water. The flow dynamics and behavior in this zone is recognized to be important for surface water/groundwater interactions, as well as fish spawning, among other processes. As an innovative urban water management practice, the hyporheic zone can be designed by engineers and actively managed for improvements in both water quality and riparian habitat.
A seagrass meadow or seagrass bed is an underwater ecosystem formed by seagrasses. Seagrasses are marine (saltwater) plants found in shallow coastal waters and in the brackish waters of estuaries. Seagrasses are flowering plants with stems and long green, grass-like leaves. They produce seeds and pollen and have roots and rhizomes which anchor them in seafloor sand.
Daniel Kleppner, born 1932, is the Lester Wolfe Professor Emeritus of Physics at Massachusetts Institute of Technology (MIT) and co-founder and co-director of the MIT-Harvard Center for Ultracold Atoms. His areas of science include atomic, molecular, and optical physics, and his research interests include experimental atomic physics, laser spectroscopy, and high precision measurements.
A riffle is a shallow landform in a flowing channel. Colloquially, it is a shallow place in a river where water flows quickly past rocks. However, in geology a riffle has specific characteristics.
A hydrologic model is a simplification of a real-world system that aids in understanding, predicting, and managing water resources. Both the flow and quality of water are commonly studied using hydrologic models.
Hydrological optimization applies mathematical optimization techniques to water-related problems. These problems may be for surface water, groundwater, or the combination. The work is interdisciplinary, and may be done by hydrologists, civil engineers, environmental engineers, and operations researchers.
Blue carbon is a term used in the climate change mitigation context that refers to "biologically driven carbon fluxes and storage in marine systems that are amenable to management." Most commonly, it refers to the role that tidal marshes, mangroves and seagrasses can play in carbon sequestration. Such ecosystems can contribute to climate change mitigation and also to ecosystem-based adaptation. When blue carbon ecosystems are degraded or lost they release carbon back to the atmosphere.
Dimitris Drikakis, PhD, FRAeS, CEng, is a Greek-British applied scientist, engineer and university professor. His research is multidisciplinary. It covers fluid dynamics, computational fluid dynamics, acoustics, heat transfer, computational science from molecular to macro scale, materials, machine learning, and emerging technologies. He has applied his research to diverse fields such as Aerospace & Defence, Biomedical, and Energy and Environment Sectors. He received The William Penney Fellowship Award by the Atomic Weapons Establishment to recognise his contributions to compressible fluid dynamics. He was also the winner of NEF's Innovator of the Year Award by the UK's Institute of Innovation and Knowledge Exchange for a new generation carbon capture nanotechnology that uses carbon nanotubes for filtering out carbon dioxide and other gases.
Theodore Gordon Shepherd is the Grantham Professor of Climate Science at the University of Reading.
Fotis Sotiropoulos is a Greek-born American engineering professor and university administrator known for his research contributions in computational fluid dynamics for river hydrodynamics, renewable energy, biomedical and biological applications. He currently serves as the Provost and Senior Vice President for Academic Affairs of Virginia Commonwealth University, a position he has held since August 1, 2021
Gareth Huw McKinley is Professor of Teaching Innovation in the Department of Mechanical Engineering at Massachusetts Institute of Technology (MIT).
Lydia Bourouiba is an Esther and Harold E. Edgerton Professor, an Associate Professor in the Civil and Environmental Engineering and Mechanical Engineering departments, and in the Institute for Medical Engineering and Science at the Massachusetts Institute of Technology. She is also a Harvard-MIT Health Sciences and Technology Faculty, and Affiliate Faculty of Harvard Medical School. She directs the Fluid Dynamics of Disease Transmission Laboratory at MIT.
Allan Adams is an American physicist and oceanographer. His research in physics has focused on string theory, QFT, and fluid dynamics, while his work in oceanography and ocean engineering have focused on high-precision optical sensing and imaging and on low-cost scalable instrumentation. He currently leads the Future Ocean Lab at Massachusetts Institute of Technology and is a visiting oceanographer at the Woods Hole Oceanographic Institution.
The nonlinearity of surface gravity waves refers to their deviations from a sinusoidal shape. In the fields of physical oceanography and coastal engineering, the two categories of nonlinearity are skewness and asymmetry. Wave skewness and asymmetry occur when waves encounter an opposing current or a shallow area. As waves shoal in the nearshore zone, in addition to their wavelength and height changing, their asymmetry and skewness also change. Wave skewness and asymmetry are often implicated in ocean engineering and coastal engineering for the modelling of random sea states, in particular regarding the distribution of wave height, wavelength and crest length. For practical engineering purposes, it is important to know the probability of these wave characteristics in seas and oceans at a given place and time. This knowledge is crucial for the prediction of extreme waves, which are a danger for ships and offshore structures. Satellite altimeter Envisat RA-2 data shows geographically coherent skewness fields in the ocean and from the data has been concluded that large values of skewness occur primarily in regions of large significant wave height.
Christa Peters-Lidard is an American hydrologist known for her work on integrating land surface modeling and data assimilation, particularly with remotely sensed measurements of precipitation.
Patricia Wiberg is a professor at University of Virginia known for her research on the transport of sediments in aquatic environments.
Sarah Gille is a physical oceanographer at Scripps Institution of Oceanography known for her research on the role of the Southern Ocean in the global climate system.
Alison Criscitiello is an ice core scientist, National Geographic Explorer, Fellow of the Royal Canadian Geographical Society, and Director of the Canadian Ice Core Lab at the University of Alberta. In addition to her academic work, she is a co-founder of Girls on Ice Canada and an avid adventurer and mountain climber. She led the first all-women ascent of Lingsarmo and has received numerous American Alpine Club grants for her pioneering expeditions.
Yan Zheng is a marine geochemist known for her research on metals in groundwater and private wells in Bangladesh, China, and the United States. She is an elected fellow of the Geological Society of America and the American Geophysical Union.
Internal wave breaking is a process during which internal gravity waves attain a large amplitude compared to their length scale, become nonlinearly unstable and finally break. This process is accompanied by turbulent dissipation and mixing. As internal gravity waves carry energy and momentum from the environment of their inception, breaking and subsequent turbulent mixing affects the fluid characteristics in locations of breaking. Consequently, internal wave breaking influences even the large scale flows and composition in both the ocean and the atmosphere. In the atmosphere, momentum deposition by internal wave breaking plays a key role in atmospheric phenomena such as the Quasi-Biennial Oscillation and the Brewer-Dobson Circulation. In the deep ocean, mixing induced by internal wave breaking is an important driver of the meridional overturning circulation. On smaller scales, breaking-induced mixing is important for sediment transport and for nutrient supply to the photic zone. Most breaking of oceanic internal waves occurs in continental shelves, well below the ocean surface, which makes it a difficult phenomenon to observe.