Zobrazeno 1 - 10
of 37
pro vyhledávání: '"E. Mollo-Christensen"'
Publikováno v:
Journal of Atmospheric and Oceanic Technology. 1:358-371
A wave sensor, consisting of parallel, evenly spaced capacitance wires, whose output is the sum of the water surface deflections at the wires, has been built and tested in a wave tank. The probe output simulates Bragg scattering of electromagnetic wa
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0ec196ec3be97fba79be30f792266d8b
https://doi.org/10.1175/1520-0426(1984)001<0358:thpasb>2.0.co
https://doi.org/10.1175/1520-0426(1984)001<0358:thpasb>2.0.co
Autor:
E. Mollo-Christensen
Publikováno v:
Journal of Applied Meteorology. 18:367-370
An obstacle in a boundary-layer flow creates a disturbance upwind of the obstacle, consisting of a stationary vortex extending downstream on both sides of the obstacle. This flow disturbance may interfere with observation of wind profiles or fluxes.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e9cb4ce06d866196b95395c8c752c249
https://doi.org/10.1175/1520-0450(1979)018<0367:uddtps>2.0.co
https://doi.org/10.1175/1520-0450(1979)018<0367:uddtps>2.0.co
Autor:
E. Mollo-Christensen
Publikováno v:
Applied Mechanics ISBN: 9783662278635
This paper presents a description of arterial blood flow from the viewpoint of a fluid dynamicist.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::86dfab661f8310ed835d3aacd4dfba23
https://doi.org/10.1007/978-3-662-29364-5_151
https://doi.org/10.1007/978-3-662-29364-5_151
Publikováno v:
Journal of Geophysical Research: Oceans. 86:2076-2077
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::36115ce1e348d1deb145dabe5ed38d78
https://doi.org/10.1029/jc086ic03p02076
https://doi.org/10.1029/jc086ic03p02076
Publikováno v:
Journal of Geophysical Research. 83:4117
Field and laboratory observations of surface wave fields show that the propagation speed of harmonic wave components differs from the predictions of linear theory. Angular spread fails to account for the observed discrepancy. An explanation is that t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7bcfe278147d43ce0f7c7c55874640ad
https://doi.org/10.1029/jc083ic08p04117
https://doi.org/10.1029/jc083ic08p04117
Publikováno v:
The Journal of the Acoustical Society of America. 86:2471-2471
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ce563b25a03fefcbeef1fcad255b167c
https://doi.org/10.1121/1.398418
https://doi.org/10.1121/1.398418
Publikováno v:
Journal of Geophysical Research. 87:5699
Laboratory experiments in which waves from a mechanical wave generator were injected at the upwind end of a fetch-limited wave field. The injected wave groups appear to grow at the expense of the ambient wind wave field, and the wind profiles in the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8e8a53afaa334ef10f642821be3c946a
https://doi.org/10.1029/jc087ic08p05699
https://doi.org/10.1029/jc087ic08p05699
Publikováno v:
Journal of Geophysical Research. 84:7769
Observations of ocean surface waves under steady wind conditions show that they do not obey the linear dispersion relation, thus confirming that previously reported results of laboratory experiments also apply to the ocean. It is also shown that mech
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::844944db4475dc58b241e13627845c23
https://doi.org/10.1029/jc084ic12p07769
https://doi.org/10.1029/jc084ic12p07769