Zobrazeno 1 - 10
of 52
pro vyhledávání: '"D. A. Yuen"'
Publikováno v:
Nonlinear Processes in Geophysics, Vol 12, Iss 1, Pp 117-128 (2005)
We present a novel technique based on a multi-resolutional clustering and nonlinear multi-dimensional scaling of earthquake patterns to investigate observed and synthetic seismic catalogs. The observed data represent seismic activities around the Jap
Externí odkaz:
https://doaj.org/article/6aa785d07fbe41e8b2da5093ac3c5a51
Publikováno v:
Nonlinear Processes in Geophysics, Vol 12, Iss 2, Pp 257-267 (2005)
We use a four-dimensional variational data assimilation (4D-VAR) algorithm to observe the growth of 2-D plumes from a point heat source. In order to test the predictability of the 4D-VAR technique for 2-D plumes, we perturb the initial conditions and
Externí odkaz:
https://doaj.org/article/76e8c15a958a4b44b1d1ff933375cb35
Publikováno v:
Nonlinear Processes in Geophysics, Vol 9, Iss 3/4, Pp 311-323 (2002)
The thermal conductivity of mantle materials has two components, the lattice component klat from phonons and the radiative component krad due to photons. These two contributions of variable thermal conductivity have a nonlinear dependence in the temp
Externí odkaz:
https://doaj.org/article/ad9d39c514cb443a8b7a4bfadbe0a563
Autor:
D. A. Yuen, S. Balachandar, V. C. Steinbach, S. Honda, D. M. Reuteler, J. J. Smedsmo, G. S. Lauer
Publikováno v:
Nonlinear Processes in Geophysics, Vol 2, Iss 3/4, Pp 206-221 (1995)
We have examined the non-equilibrium effects of core-cooling and time-dependent internal-heating on the thermal evolution of the Earth's mantle and on mantle flush events caused by the two major phase transitions. Both two- and three-dimensional mode
Externí odkaz:
https://doaj.org/article/e9e10fec86e44cbcb75f990febf52cf3
Publikováno v:
Journal of Geophysical Research: Solid Earth. 125
Publikováno v:
Journal of Geophysical Research: Planets. 123:2162-2177
Autor:
A. P. van den Berg, D. A. Yuen, Michael H. G. Jacobs, Renata M. Wentzcovitch, Koichiro Umemoto
Publikováno v:
Icarus, 317, 412-426. Academic Press Inc.
Icarus, 317, 412. Academic Press Inc.
van den Berg, A P, Yuen, D A, Umemoto, K, Jacobs, M H G & Wentzcovitch, R M 2019, ' Mass-dependent dynamics of terrestrial exoplanets using ab initio mineral properties ', Icarus, vol. 317, pp. 412-426 . https://doi.org/10.1016/j.icarus.2018.08.016
Icarus, 317, 412. Academic Press Inc.
van den Berg, A P, Yuen, D A, Umemoto, K, Jacobs, M H G & Wentzcovitch, R M 2019, ' Mass-dependent dynamics of terrestrial exoplanets using ab initio mineral properties ', Icarus, vol. 317, pp. 412-426 . https://doi.org/10.1016/j.icarus.2018.08.016
We present new modelling results for the internal structure and convective dynamics of large terrestrial (rocky) exoplanets. By going out to 20 Earth masses our results show that pressure and temperature can reach several Terapascal (TPa) and 10000 K
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::f23f47fb7e2ac3a5cb71c9fbb0f9d3a1
https://research.vu.nl/en/publications/0dcebbba-6ef0-4791-b711-eac023440925
https://research.vu.nl/en/publications/0dcebbba-6ef0-4791-b711-eac023440925
Publikováno v:
Marine Technology and SNAME News. 45:132-146
The input data in strength calculations (e.g., loads, geometric, and material properties) may have different levels of certainty/uncertainty. In most cases, the level of certainty of the result (e.g., stresses) is unknown. The knowledge of this certa
Publikováno v:
Physics of the Earth and Planetary Interiors. 149:259-278
Most convection studies of thermal history have not considered explicitly the thermal interaction between the mantle flow and the core. We have investigated the influences of variable thermal conductivity and variable viscosity (temperature- and pres
Autor:
D. A. Yuen, Bertram Schott
Publikováno v:
Physics of the Earth and Planetary Interiors. 146:139-145
We have investigated the possibilities for thermochemical convective instability of a low viscous, dense D″-layer heated from below, in either the extended Boussinesq approximation (i.e. with dissipation) or the Boussinesq approximation only. We fi