2011
● IFREE YES seminar
Place: IT-Wing, 4th-floor,Meeting Room, Yokohama Institute for Earth Sciences
Time: June 8(Wed) 14:00-15:30
Speaker: Takashi Nakagawa
Title: Effects of a stably stratified layer near the top boundary in
numerical dynamo simulations in a rotating spherical shell: Implications for
dynamics of Earth's core
Abstract: Abstract: For Earth's core, a stably stratified layer could be recently
found by seismic wave analyses [e.g. Helffrich and Kaneshima, 2010] and
forms by the light element release due to the inner core growth [Lister and
Buffett, 1998] or chemical core-mantle interaction [Buffett and Seagle,
2010]. Several numerical dynamo simulations have investigated how a
stratified layer affects the dynamics of convection in a rotating spherical
shell [e.g., Christensen, 2006; Stanley and Mohammadi, 2008] but not for
Earth's core dynamics.
Here we introduce some interesting results found from numerical dynamo
simulations in a rotating spherical shell with a stably stratified layer
near the top boundary to imply how a stratified layer affects the dynamics
in Earth's core with showing force balances and energy contributions as
well as the influence to the polarity reversals varying with the degree of
stratification.
● IFREE YES seminar
IFREE 1A&LP seminar
Place: 403&404 Meeting room, IT building, Yokohama Institute for Earth Sciences
Time: 14:00-17:00 on 25th, January (Tuesday)
Speaker1: Ayako Nakanishi
Title: Geometry of the Philippine Sea plate subducting beneath the southwestern Nankai Trough
-Progress report of structural study for Nankai Trough seismogenic zone -
Abstract: Sorry, no English abstract.
Speaker2: T. Yamaguchi and M. Doi (Department of Applied Physics, The University of Tokyo)
Title: Heterogeneous stick-slip motion in sliding friction of polymer gels
Abstract:
When a soft polymer gel is slid on a glass plate, it is known
that spatio-temporally heterogeneous stick-slip motions occur during
sliding. In this presentation, we will report our experimental results
on elementary processes, size distributions and size-duration relations
during sliding of the polymer gels. We will also discuss the relations
with earthquake phenomena.