535 research outputs found
Oscillation modes of relativistic slender tori
Accretion flows with pressure gradients permit the existence of standing
waves which may be responsible for observed quasi-periodic oscillations (QPO's)
in X-ray binaries. We present a comprehensive treatment of the linear modes of
a hydrodynamic, non-self-gravitating, polytropic slender torus, with arbitrary
specific angular momentum distribution, orbiting in an arbitrary axisymmetric
spacetime with reflection symmetry. We discuss the physical nature of the
modes, present general analytic expressions and illustrations for those which
are low order, and show that they can be excited in numerical simulations of
relativistic tori. The mode oscillation spectrum simplifies dramatically for
near Keplerian angular momentum distributions, which appear to be generic in
global simulations of the magnetorotational instability. We discuss our results
in light of observations of high frequency QPO's, and point out the existence
of a new pair of modes which can be in an approximate 3:2 ratio for arbitrary
black hole spins and angular momentum distributions, provided the torus is
radiation pressure dominated. This mode pair consists of the axisymmetric
vertical epicyclic mode and the lowest order axisymmetric breathing mode.Comment: submitted to MNRA
6 hr tide seen in sporadic E layers
The GPS radio occultation technique is used to study sporadic E (Es) layer plasma irregularities of the Earth’s ionosphere on a global scale using COSMIC/FORMOSAT-3 satellite constellation GPS signal-to-noise ratio (SNR) profiles. The maximum deviation from the mean SNR is attributed to the height of the Es layer. Es are produced by ion convergence due to vertical wind shear in the presence of a horizontal component of the Earth magnetic field, while the wind shear is provided mainly by solar tides. Indeed, close correlation between Es and wind shear phases have already been found for the semidiurnal and terdiurnal tidal components. Here, we present the global distribution of quarterdiurnal (QDT) signatures in Es occurrence rates. We find that, in accordance with upward energy flux, negative vertical phase
gradients of QDT Es signatures are observed. The maximum signal of QDT Es is found at altitudes above 100 km. In the southern hemisphere, maximum QDT Es occurrence rates are found in winter and during equinoxes. In the northern hemisphere, however, at altitudes above 100 km strong QDT activity is also visible.Die GPS-Radiookkultationstechnik wird verwendet, um ionosphärische Plasmairregularitäten in Verbindung mit sporadischen E- (Es) Schichten auf globaler Skala zu untersuchen. Verwendet werden Signal-Rauschverhältnis- (SNR-) Profile. Die maximale Abweichung vom mittleren SNR wird der Höhe der Es-Schicht zugeordnet. Es werden durch Ionenkonvergenz aufgrund von vertikaler Windscherung
in Anwesenheit einer horizontalen Komponente des Erdmagnetfeldes hervorgerufen, wobei die Scherung hauptsächlich durch solare Gezeiten verursacht wird. Tatsächlich wurden schon früher deutliche Übereinstimmungen zwischen dem Auftreten von Es und den Phasen der halb- und dritteltägigen Gezeiten gefunden. Hier stellen wir die globale Verteilung der vierteltägigen (QDT) Signaturen in Es-
Auftretensraten vor. Es zeigt sich dass, in Übereinstimmung mit einem aufwärts gerichteten Energietransport, negative vertikale Phasengradienten der QDT in Es auftreten. Die maximale Auftretenswahrscheinlichkeit liegt bei Höhen oberhalb von 100 km. Auf der Südhemisphäre fällt das Maximum der QDT in Es-Auftretensraten in den Winter, während auf der Nordhemisphäre oberhalb von 100 km auch im Sommer starke QDT-Aktivität zu verzeichnen ist
A swift approach for identifying vulnerable linear transport infrastructures in areas prone to floods and erosion
Linear transport infrastructures are essential for the socio-economic development of industrialized countries. However, adverse meteorological and hydrogeological events can result in significant economic losses.Globally, floods have the most substantial socio-economic impact. Climate Change, due to the extent of transport infrastructures over flood-prone territories, is a very important factor in worsening flood risk.The main objective of this study is to identify the sections of the hydrographic network that are susceptible to flood and erosion hazards where road infrastructures are located. The Metropolitan City of Cagliari (Sardinia, Italy) is selected as test site, due to the presence of several coastal watersheds and of a high population density.A swift methodological approach, based on already available datasets from public repositories and GIS analyses, is presented. This approach includes: i) geomorphological characterization of the hydrographic network; ii) census of stream tracts where bridges were damaged in past flood events; iii) identification of potentially critical tracts (PCT), based on similar geomorphological conditions; iv) multi-temporal satellite imagery analysis of PCT for the identification of flood-prone areas and, therefore, vulnerable road crossings.The adopted methodology has proved to be effective for the identification of vulnerable road crossings over wide portion of territories, identifying critical sites that need further investigation
Strain and correlation of self-organized Ge_(1-x)Mn_x nanocolumns embedded in Ge (001)
We report on the structural properties of Ge_(1-x)Mn_x layers grown by
molecular beam epitaxy. In these layers, nanocolumns with a high Mn content are
embedded in an almost-pure Ge matrix. We have used grazing-incidence X-ray
scattering, atomic force and transmission electron microscopy to study the
structural properties of the columns. We demonstrate how the elastic
deformation of the matrix (as calculated using atomistic simulations) around
the columns, as well as the average inter-column distance can account for the
shape of the diffusion around Bragg peaks.Comment: 9 pages, 7 figure
Migrating and nonmigrating tidal signatures in sporadic E layer occurrence rates
We analyse sporadic E (ES) layer occurrence rates (OR) obtained from ionospheric GPS radio occultation measurements by the FORMOSAT-3/COSMIC constellation. Maximum OR are seen at 95–105 km altitude. Midlatitude ES layers are mainly due to wind shear in the presence of tides, and the strongest signals are the migrating diurnal and semidiurnal components. Especially in the Southern Hemisphere, nonmigrating components such as a diurnal westward wave 2 and a semidiurnal westward wave 1 are also visible, especially at higher latitudes. Near the equator, a strong diurnal eastward wavenumber 3 component and a semidiurnal eastward wavenumber 2 component occur in summer and autumn. Terdiurnal and quarterdiurnal components are weaker than the diurnal and semidiurnal ones.</p
Hydrogen Burning on Magnetar Surfaces
We compute the rate of diffusive nuclear burning for hydrogen on the surface
of a "magnetar" (Soft Gamma-Ray Repeater or Anomalous X-Ray Pulsar). We find
that hydrogen at the photosphere will be burned on an extremely rapid timescale
of hours to years, depending on composition of the underlying material.
Improving on our previous studies, we explore the effect of a maximally thick
"inert" helium layer, previously thought to slow down the burning rate. Since
hydrogen diffuses faster in helium than through heavier elements, we find this
helium buffer actually increases the burning rate for magnetars. We compute
simple analytic scalings of the burning rate with temperature and magnetic
field for a range of core temperature. We conclude that magnetar photospheres
are very unlikely to contain hydrogen. This motivates theoretical work on heavy
element atmospheres that are needed to measure effective temperature from the
observed thermal emission and constrains models of AXPs that rely on magnetar
cooling through thick light element envelopes.Comment: 4 pages, 2 figures, To be published in ApJ Letter
Can Parity Violation in Neutrino Transport Lead to Pulsar Kicks?
In magnetized proto-neutron stars, neutrino cross sections depend
asymmetrically on the neutrino momenta due to parity violation. However, these
asymmetric opacities do not induce any asymmetric flux in the bulk interior of
the star where neutrinos are nearly in thermal equilibrium. Consequently,
parity violation in neutrino absorption and scattering can only give rise to
asymmetric neutrino flux above the neutrino-matter decoupling layer. The kick
velocity is substantially reduced from previous estimates, requiring a dipole
field ~G to get of order a few hundred km~s.Comment: REVTEX, 4 pages, no figures. Submitted to Phys. Rev. Letter
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