Zobrazeno 1 - 10
of 173
pro vyhledávání: '"T. T. Janssen"'
Autor:
Sean Celona, Hans C. Graber, Jennifer A. MacKinnon, C. Chris Chickadel, Sutara H. Suanda, Andrew M. Moore, Christopher A. Edwards, Tongtong Xu, André Palóczy, David A. Fertitta, Jim Thomson, William J. Crawford, Annika O'Dea, Amy F. Waterhouse, Jamie MacMahan, P.B. Smit, Sophia Merrifield, Matthew S. Spydell, Nirnimesh Kumar, Melissa Moulton, Lisa Nyman, John A. Colosi, Falk Feddersen, Tony de Paolo, C. Swann, D. J. Grimes, Stephen D. Pierce, Merrick C. Haller, Emanuele Di Lorenzo, Alexandra Simpson, E. F. Braithwaite, Joseph Calantoni, Ryan S. Mieras, Kendall Melville, John A. Barth, T. T. Janssen, Björn Lund, Kevin A. Haas, Sean Haney, Jacqueline M. McSweeney, Eric Terrill, James A. Lerczak, Arthur J. Miller, Luc Lenain, Johannes Becherer, Roland Romeiser, Seongho Ahn, Michael Kovatch, Matt K. Gough, James N. Moum
Publikováno v:
Bulletin of the American Meteorological Society. 102:E1033-E1063
17 USC 105 interim-entered record; under review. The article of record as published may be found at http://dx.doi.org/10.1175/BAMS-D-19-0281.1 The inner shelf, the transition zone between the surfzone and the midshelf, is a dynamically complex region
Autor:
P.B. Smit, T. T. Janssen
Publikováno v:
Journal of Physical Oceanography. 49:2615-2630
The propagation of ocean swells from generating regions to remote coastlines is affected by submesoscale turbulence in the surface flow field. The presence of submesoscale velocity variations results in random scattering of wave rays. While the inter
A distributed sensor network of several hundred free-drifting, real-time marine weather sensors was deployed beginning in early 2019 initially focused in the Pacific Ocean and expanding globally. The Spotter buoys used in the network represent a next
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::703129e0bf2b02836923cde761d7db8b
https://doi.org/10.5194/egusphere-egu21-13717
https://doi.org/10.5194/egusphere-egu21-13717
Publikováno v:
Journal of Geophysical Research: Oceans. 125
Compact wave buoys are increasingly used to provide monitoring of coastal and oceanic conditions by measuring surface waves in real time. Due to their relatively compact size, they are generally not suited to measure wind directly. However, since the
Autor:
T. Portwood, D. Clark, I. A. Houghton, M. Sosa, T. T. Janssen, P.B. Smit, E. Shapiro, K. Jordanova
Publikováno v:
Ocean Modelling. 159:101738
In-situ ocean wave observations are critical to improve model skill and validate remote sensing wave measurements. Historically, such observations are extremely sparse due to the large costs and complexity of traditional wave buoys and sensors. In th
Publikováno v:
Ocean Modelling. 104:203-212
In shallow water, the spectral evolution associated with energy transfers due to three-wave (or triad) interactions is important for the prediction of nearshore wave propagation and wave-driven dynamics. The numerical evaluation of these nonlinear in
Publikováno v:
Journal of Geophysical Research: Oceans. 121:3409-3421
Wave focusing of energetic swell fields can result in small-scale variations associated with coherent interference that can be important for nearshore circulation and beach dynamics. However, coherent interference is difficult to measure with convent
Autor:
T. T. Janssen, T. H. C. Herbers
Publikováno v:
Journal of Physical Oceanography. 46:1009-1021
Nonlinear effects in Lagrangian sea surface motions are important to understanding variability in wave-induced mass transport, wave-driven diffusion processes, and the interpretation of measurements obtained with moored or free-drifting buoys. This s
Publikováno v:
Ocean Modelling. 96:26-35
Refraction of swell waves in coastal waters can result in fast-scale variations of wave statistics due to wave interference. These variations cannot be resolved by wave models based on the radiative transport equation. More advanced models based on q
Publikováno v:
Journal of physical oceanography, 45 (4), April 2015
Refractive focusing of swell waves can result in fast-scale variations in the wave statistics because of wave interference, which cannot be resolved by stochastic wave models based on the radiative transport equation. Quasi-coherent statistical theor