2,196 research outputs found
Bayesian Markov-chain-Monte-Carlo inversion of time-lapse cross hole ground-penetrating radar data to characterize the vadose zone at the Arrenaes field site, Denmark
The ground-penetrating radar (GPR) geophysical method has the potential
to provide valuable information on the hydraulic properties of the
vadose zone because of its strong sensitivity to soil water content.
In particular, recent evidence has suggested that the stochastic
inversion of crosshole GPR traveltime data can allow for a significant
reduction in uncertainty regarding subsurface van Genuchten-Mualem
(VGM) parameters. Much of the previous work on the stochastic estimation
of VGM parameters from crosshole GPR data has considered the case
of steady-state infiltration conditions, which represent only a small
fraction of practically relevant scenarios. We explored in detail
the dynamic infiltration case, specifically examining to what extent
time-lapse crosshole GPR traveltimes, measured during a forced infiltration
experiment at the Arreneas field site in Denmark, could help to quantify
VGM parameters and their uncertainties in a layered medium, as well
as the corresponding soil hydraulic properties. We used a Bayesian
Markov-chain-Monte-Carlo inversion approach. We first explored the
advantages and limitations of this approach with regard to a realistic
synthetic example before applying it to field measurements. In our
analysis, we also considered different degrees of prior information.
Our findings indicate that the stochastic inversion of the time-lapse
GPR data does indeed allow for a substantial refinement in the inferred
posterior VGM parameter distributions compared with the corresponding
priors, which in turn significantly improves knowledge of soil hydraulic
properties. Overall, the results obtained clearly demonstrate the
value of the information contained in time-lapse GPR data for characterizing
vadose zone dynamics
When threat matters: Self-regulation, threat salience, and stereotyping
The final publication is available at Elsevier via http://dx.doi.org/10.1016/j.jesp.2015.03.003 © 2015. This manuscript version is made available under the CC-BY-NC-ND 4.0 license http://creativecommons.org/licenses/by-nc-nd/4.0/Four experiments examined whether information implying imminent threat to safety would interact with regulatory focus (Higgins, 1997) to affect the utilization of threat-relevant stereotypes. Because information suggesting imminent danger is more relevant to the safety goals of prevention-focused individuals than the advancement goals of promotion-focused individuals, utilization of threat-relevant stereotypes was expected to increase under such conditions only under prevention focus. Support for this prediction was obtained in four distinct and socially important domains. Using scenarios describing a violent crime committed by an African-American male (Experiment 1) or a petty crime committed by an undocumented immigrant (Experiment 2), prevention-focused individuals made judgments consistent with stereotypes when threat was perceived to be high rather than low. In studies that manipulated the stereotypicality of the target in a terrorism scenario (Experiments 3 & 4), prevention-focused individuals were more likely to endorse scrutinizing a stereotypical compared with a non-stereotypical target when terrorism was described as an increasing problem. Implications for models of stereotyping, self-regulation, and responding to threat are discussed.NSF Grant [1147779
Fast magnetic reconnection in free space: self-similar evolution process
We present a new model for time evolution of fast magnetic reconnection in
free space, which is characterized by self-similarity. Reconnection triggered
by locally enhanced resistivity assumed at the center of the current sheet can
self-similarly and unlimitedly evolve until external factors affect the
evolution. The possibility and stability of this type of evolution are verified
by numerical simulations in a very wide spatial dynamic range. Actual
astrophysical reconnection in solar flares and geomagnetospheric substorms can
be treated as an evolutionary process in free space, because the resultant
scale is much larger than the initial scale. In spite of this fact, most of the
previous numerical works focused on the evolutionary characters strongly
affected by artificial boundary conditions on the simulation boundary. Our new
model clarifies a realistic evolution for such cases. The characteristic
structure around the diffusion region is quite similar to the Petschek model
which is characterized by a pair of slow-mode shocks and the fast-mode
rarefaction-dominated inflow. However, in the outer region, a vortex-like
return flow driven by the fast-mode compression caused by the piston effect of
the plasmoid takes place. The entire reconnection system expands
self-similarly.Comment: 17 Pages, 17 Figure
Estimation of the correlation structure of crustal velocity heterogeneity from seismic reflection data
Numerous sources of evidence point to the fact that heterogeneity
within the Earth's deep crystalline crust is complex and hence may
be best described through stochastic rather than deterministic approaches.
As seismic reflection imaging arguably offers the best means of sampling
deep crustal rocks in situ, much interest has been expressed in using
such data to characterize the stochastic nature of crustal heterogeneity.
Previous work on this problem has shown that the spatial statistics
of seismic reflection data are indeed related to those of the underlying
heterogeneous seismic velocity distribution. As of yet, however,
the nature of this relationship has remained elusive due to the fact
that most of the work was either strictly empirical or based on incorrect
methodological approaches. Here, we introduce a conceptual model,
based on the assumption of weak scattering, that allows us to quantitatively
link the second-order statistics of a 2-D seismic velocity distribution
with those of the corresponding processed and depth-migrated seismic
reflection image. We then perform a sensitivity study in order to
investigate what information regarding the stochastic model parameters
describing crustal velocity heterogeneity might potentially be recovered
from the statistics of a seismic reflection image using this model.
Finally, we present a Monte Carlo inversion strategy to estimate
these parameters and we show examples of its application at two different
source frequencies and using two different sets of prior information.
Our results indicate that the inverse problem is inherently non-unique
and that many different combinations of the vertical and lateral
correlation lengths describing the velocity heterogeneity can yield
seismic images with the same 2-D autocorrelation structure. The ratio
of all of these possible combinations of vertical and lateral correlation
lengths, however, remains roughly constant which indicates that,
without additional prior information, the aspect ratio is the only
parameter describing the stochastic seismic velocity structure that
can be reliably recovered
Fast Collisionless Reconnection Condition and Self-Organization of Solar Coronal Heating
I propose that solar coronal heating is a self-regulating process that keeps
the coronal plasma roughly marginally collisionless. The self-regulating
mechanism is based on the interplay of two effects. First, plasma density
controls coronal energy release via the transition between the slow collisional
Sweet-Parker regime and the fast collisionless reconnection regime. This
transition takes place when the Sweet--Parker layer becomes thinner than the
characteristic collisionless reconnection scale. I present a simple criterion
for this transition in terms of the upstream plasma density (n_e), the
reconnecting (B_0) and guide (B_z) magnetic field components, and the global
length (L) of the reconnection layer: L < 6.10^9 cm [n_e/(10^{10}/cm^3)]^(-3)
(B_0/30G)^4 (B_0/B_z)^2. Next, coronal energy release by reconnection raises
the ambient plasma density via chromospheric evaporation and this, in turn,
temporarily inhibits subsequent reconnection involving the newly-reconnected
loops. Over time, however, radiative cooling gradually lowers the density again
below the critical value and fast reconnection again becomes possible. As a
result, the density is highly inhomogeneous and intermittent but,
statistically, does not deviate strongly from the critical value which is
comparable with the observed coronal density. Thus, in the long run, the
coronal heating process can be represented by repeating cycles that consist of
fast reconnection events (i.e., nanoflares), followed by rapid evaporation
episodes, followed by relatively long periods (1-hour) during which magnetic
stresses build up and simultaneously the plasma cools down and precipitates.Comment: 17 pages, no figures; accepted to the Astrophysical Journal; replaced
to match the accepted versio
Simulations of Electron Acceleration at Collisionless Shocks: The Effects of Surface Fluctuations
Energetic electrons are a common feature of interplanetary shocks and
planetary bow shocks, and they are invoked as a key component of models of
nonthermal radio emission, such as solar radio bursts. A simulation study is
carried out of electron acceleration for high Mach number, quasi-perpendicular
shocks, typical of the shocks in the solar wind. Two dimensional
self-consistent hybrid shock simulations provide the electric and magnetic
fields in which test particle electrons are followed. A range of different
shock types, shock normal angles, and injection energies are studied. When the
Mach number is low, or the simulation configuration suppresses fluctuations
along the magnetic field direction, the results agree with theory assuming
magnetic moment conserving reflection (or Fast Fermi acceleration), with
electron energy gains of a factor only 2 - 3. For high Mach number, with a
realistic simulation configuration, the shock front has a dynamic rippled
character. The corresponding electron energization is radically different:
Energy spectra display: (1) considerably higher maximum energies than Fast
Fermi acceleration; (2) a plateau, or shallow sloped region, at intermediate
energies 2 - 5 times the injection energy; (3) power law fall off with
increasing energy, for both upstream and downstream particles, with a slope
decreasing as the shock normal angle approaches perpendicular; (4) sustained
flux levels over a broader region of shock normal angle than for adiabatic
reflection. All these features are in good qualitative agreement with
observations, and show that dynamic structure in the shock surface at ion
scales produces effective scattering and can be responsible for making high
Mach number shocks effective sites for electron acceleration.Comment: 26 pages, 12 figure
Analytic solution for nonlinear shock acceleration in the Bohm limit
The selfconsistent steady state solution for a strong shock, significantly
modified by accelerated particles is obtained on the level of a kinetic
description, assuming Bohm-type diffusion. The original problem that is
commonly formulated in terms of the diffusion-convection equation for the
distribution function of energetic particles, coupled with the thermal plasma
through the momentum flux continuity equation, is reduced to a nonlinear
integral equation in one variable. Its solution provides selfconsistently both
the particle spectrum and the structure of the hydrodynamic flow. A critical
system parameter governing the acceleration process is found to be , where , with a suitably
normalized injection rate , the Mach number M >> 1, and the cut-off
momentum . We particularly focus on an efficient solution, in which
almost all the energy of the flow is converted into a few energetic particles.
It was found that (i) for this efficient solution (or, equivalently, for
multiple solutions) to exist, the parameter
must exceed a critical value ( is the injection
momentum), (ii) the total shock compression ratio r increases with M and
saturates at a level that scales as $ r \propto \Lambda_1 (iii) the downstream
power-law spectrum has the universal index q=3.5 over a broad momentum range.
(iv) completely smooth shock transitions do not appear in the steady state
kinetic description.Comment: 39 pages, 3 PostScript figures, uses aasms4.sty, to appear in Aug.
20, 1997 issue ApJ, vol. 48
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