Zobrazeno 1 - 10
of 45
pro vyhledávání: '"Diane M Henderson"'
Autor:
Louise E Jackson, Irenee Ramirez, Ron Yokota, Steven A Fennimore, Steven T Koike, Diane M Henderson, William E Chaney, Karen M Klonsky
Publikováno v:
California Agriculture, Vol 57, Iss 2, Pp 48-54 (2003)
Use of cover crops and compost increased soil quality in irrigated, intensive production of lettuce and broccoli in the Salinas Valley. These methods had the beneficial impacts of increasing soil microbial biomass, increasing total soil carbon and
Externí odkaz:
https://doaj.org/article/241a30004f3e493f8b522b91f85eb472
Publikováno v:
Studies in Applied Mathematics. 147:1388-1408
When a mechanical wavemaker at one end of a water-wave tank oscillates with a frequency, $\omega_0$, time series of downstream surface waves typically include the dominant frequency (or first harmonic), $\omega_0$, along with the second, $2\omega_0$;
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::0c55942f11b6586472052c94bb6f3d8b
Publikováno v:
International Journal of Multiphase Flow. 142:103709
This paper considers the stability of an unsteady, two-phase flow with heat and mass transfer. The model problem is motivated by loss of coolant accidents in nuclear power plants. For the example problem, two flow geometries are considered: inverted
Publikováno v:
Wave Motion. 75:25-35
An operational formulation is proposed for reconstructing a time series of water surface displacement from waves using measurements of pressure. The approach is based on the fully nonlinear formulation for pressure below traveling-wave solutions of E
Autor:
Diane M. Henderson, Girish Kumar Rajan
Publikováno v:
SIAM Journal on Applied Mathematics. 76:2030-2041
A narrow-banded spectrum of gravity waves propagating in one horizontal direction at the surface of water with finite depth may be governed by a nonlinear Schroźdinger equation (NLSE). If the depth is nonuniform, then the coefficients in the NLSE ar
Frequency downshift (FD) in wave trains on deep water occurs when a measure of the frequency, typically the spectral peak or the spectral mean, decreases as the waves evolve. Many FD models rely on wind or wave breaking. We consider seven models that
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::9450760b8cede35ff3597fbc1ce2603f
Autor:
Diane M. Henderson, Harvey Segur
Publikováno v:
Journal of Geophysical Research: Oceans. 118:5074-5091
[1] Dissipation of ocean swell, inferred from published oceanographic data, is investigated to determine if laboratory results on the dissipative stabilization of narrow-banded wave trains are applicable to ocean swell. Three issues are addressed. (i
Autor:
Diane M. Henderson, Harvey Segur
Publikováno v:
Mathematics and Computers in Simulation. 82:1172-1184
About 40 years ago, Snodgrass and other oceanographers (1966) tracked ocean swell propagating across the entire Pacific Ocean. At about the same time, several investigators (including Benjamin and Feir) showed that a uniform train of plane waves of f
Publikováno v:
Journal of Fluid Mechanics. 658:247-278
Recent predictions from competing theoretical models have disagreed about the stability/instability of bi-periodic patterns of surface waves on deep water. We present laboratory experiments to address this controversy. Growth rates of modulational pe