646 research outputs found
Critical decay index at the onset of solar eruptions
Magnetic flux ropes are topological structures consisting of twisted magnetic
field lines that globally wrap around an axis. The torus instability model
predicts that a magnetic flux rope of major radius undergoes an eruption
when its axis reaches a location where the decay index of the ambient magnetic field is larger than a critical value. In
the current-wire model, the critical value depends on the thickness and
time-evolution of the current channel. We use magneto-hydrodynamic (MHD)
simulations to investigate if the critical value of the decay index at the
onset of the eruption is affected by the magnetic flux rope's internal current
profile and/or by the particular pre-eruptive photospheric dynamics. The
evolution of an asymmetric, bipolar active region is driven by applying
different classes of photospheric motions. We find that the critical value of
the decay index at the onset of the eruption is not significantly affected by
either the pre-eruptive photospheric evolution of the active region or by the
resulting different magnetic flux ropes. As in the case of the current-wire
model, we find that there is a `critical range' , rather than a
`critical value' for the onset of the torus instability. This range is in good
agreement with the predictions of the current-wire model, despite the inclusion
of line-tying effects and the occurrence of tether-cutting magnetic
reconnection.Comment: 15 pages, 9 figures. To appear in The Astrophysical Journa
Satellite observations of reconnection between emerging and pre-existing small-scale magnetic fields
We report multi-wavelength ultraviolet observations taken with the IRIS
satellite, concerning the emergence phase in the upper chromosphere and
transition region of an emerging flux region (EFR) embedded in the unipolar
plage of active region NOAA 12529. The photospheric configuration of the EFR is
analyzed in detail benefitting from measurements taken with the
spectropolarimeter aboard the Hinode satellite, when the EFR was fully
developed. In addition, these data are complemented by full-disk, simultaneous
observations of the SDO satellite, relevant to the photosphere and the corona.
In the photosphere, magnetic flux emergence signatures are recognized in the
fuzzy granulation, with dark alignments between the emerging polarities,
cospatial with highly inclined fields. In the upper atmospheric layers, we
identify recurrent brightenings that resemble UV bursts, with counterparts in
all coronal passbands. These occur at the edges of the EFR and in the region of
the arch filament system (AFS) cospatial to the EFR. Jet activity is also found
at chromospheric and coronal levels, near the AFS and the observed brightness
enhancement sites. The analysis of the IRIS line profiles reveals the heating
of dense plasma in the low solar atmosphere and the driving of bi-directional
high-velocity flows with speeds up to 100 km/s at the same locations.
Furthermore, we detect a correlation between the Doppler velocity and line
width of the Si IV 1394 and 1402 \AA{} line profiles in the UV burst pixels and
their skewness. Comparing these findings with previous observations and
numerical models, we suggest evidence of several long-lasting, small-scale
magnetic reconnection episodes between the emerging bipole and the ambient
field. This process leads to the cancellation of a pre-existing photospheric
flux concentration of the plage with the opposite polarity flux patch of the
EFR. [...]Comment: 4 pages, 2 figures, to be published in "Nuovo Cimento C" as
proceeding of the Third Meeting of the Italian Solar and Heliospheric
Communit
Plasma flows and magnetic field interplay during the formation of a pore
We studied the formation of a pore in AR NOAA 11462. We analysed data
obtained with the IBIS at the DST on April 17, 2012, consisting of full Stokes
measurements of the Fe I 617.3 nm lines. Furthermore, we analysed SDO/HMI
observations in the continuum and vector magnetograms derived from the Fe I
617.3 nm line data taken from April 15 to 19, 2012. We estimated the magnetic
field strength and vector components and the LOS and horizontal motions in the
photospheric region hosting the pore formation. We discuss our results in light
of other observational studies and recent advances of numerical simulations.
The pore formation occurs in less than 1 hour in the leading region of the AR.
The evolution of the flux patch in the leading part of the AR is faster (< 12
hour) than the evolution (20-30 hour) of the more diffuse and smaller scale
flux patches in the trailing region. During the pore formation, the ratio
between magnetic and dark area decreases from 5 to 2. We observe strong
downflows at the forming pore boundary and diverging proper motions of plasma
in the vicinity of the evolving feature that are directed towards the forming
pore. The average values and trends of the various quantities estimated in the
AR are in agreement with results of former observational studies of steady
pores and with their modelled counterparts, as seen in recent numerical
simulations of a rising-tube process. The agreement with the outcomes of the
numerical studies holds for both the signatures of the flux emergence process
(e.g. appearance of small-scale mixed polarity patterns and elongated granules)
and the evolution of the region. The processes driving the formation of the
pore are identified with the emergence of a magnetic flux concentration and the
subsequent reorganization of the emerged flux, by the combined effect of
velocity and magnetic field, in and around the evolving structure.Comment: Accepted for publication in Astronomy and Astrophysic
Height dependence of the penumbral fine-scale structure in the inner solar atmosphere
We studied the physical parameters of the penumbra in a large and
fully-developed sunspot, one of the largest over the last two solar cycles, by
using full-Stokes measurements taken at the photospheric Fe I 617.3 nm and
chromospheric Ca II 854.2 nm lines with the Interferometric Bidimensional
Spectrometer. Inverting measurements with the NICOLE code, we obtained the
three-dimensional structure of the magnetic field in the penumbra from the
bottom of the photosphere up to the middle chromosphere. We analyzed the
azimuthal and vertical gradient of the magnetic field strength and inclination.
Our results provide new insights on the properties of the penumbral magnetic
fields in the chromosphere at atmospheric heights unexplored in previous
studies. We found signatures of the small-scale spine and intra-spine structure
of both the magnetic field strength and inclination at all investigated
atmospheric heights. In particular, we report typical peak-to-peak variations
of the field strength and inclination of G and , respectively, in the photosphere, and of G and
in the chromosphere. Besides, we estimated the vertical
gradient of the magnetic field strength in the studied penumbra: we find a
value of G km between the photosphere and the middle
chromosphere. Interestingly, the photospheric magnetic field gradient changes
sign from negative in the inner to positive in the outer penumbra.Comment: 14 page, 9 figures, accepted for Ap
Modeling environmental responses of plantassociations by fuzzy set theory
A method for studying the response of vegetation to environmental gradients, based on the community niche and fuzzy set theory, is presented. The approach is illustrated using an example from perennial halophilous vegetation along the Northern Adriatic coast of Italy. Compatibility curves are obtained by fuzzy set theoretical methods, and are used tomodel the response functions of plant associations to environmental gradients, including soil and ground water salinity, soil pH, soil and ground water temperature, percentage of sand, and variations in the ground water level. The compatibility curves summarize the similarity of a given plant community, with a particular value of an environmental variable, to the species combination of a given plant association. Compatibility curves offer an alternative approach to non-linear regression and best fit analyses normally used to model single species responses to environmental gradients. The approach is particularly useful given there is no singlemechanisticmodel that can capture the exact shape of the functional response along environmental gradients, and given that environmental data are commonly affected by high levels of noise
A data sequence aquired at Mt. Etna during the 2002 - 2003 eruption highlights the potential of continuous gravity observations as a tool to monitor and study active volcanoes
A 2.5-month long gravity sequence, encompassing the starting period of the 2002–2003 Etna eruption and coming from a summit
station only 1 km away from the new fractures, is presented and discussed. The sequence comprises some hours-long anomalies that
have a great chance to reflect mass redistributions linked to the ensuing activity. In particular, the start of the eruptive activity on
the northeastern flank was marked by a gravity decrease as strong as about 400 Gal, which reverted soon afterwards. This strong
decrease/increase anomaly is interpreted as the opening, by tectonic forces, of a fracture system along the Northeastern Rift of Mt. Etna, followed by an intrusion of magma from the central conduit to the new fractures. They were used by the intruding magma as
a path to the eruptive vents at lower elevations.
Afterwards, on three occasions, in November and December 2002, 6–12 h-lasting gravity decreases, with amplitude ranging
between 10 and 30 Gal, were observed simultaneously with increases in the amplitude of the volcanic tremor from four seismic
stations. A correlation analysis, between the gravity signal and the overall spectral amplitude of each tremor sequence is performed
over the 7 November–9 December period. A marked anti-correlation is found over each contemporaneous gravity decrease/tremor
increase, while, over the rest of the investigated period, the correlation is negligible. Accordingly, a joint source is inferred to have
acted during the occurrence of the three common anomalies. On the grounds of some volcanological observations spanning the
period covered by our analysis, we propose the temporary accumulation of a gas cloud at some level within the plumbing system
of the volcano to have acted as a joint source.
The present work is a further evidence of the potential of continuous gravity observations as a tool to monitor and study active
volcanoes and encourages their employment in spite of the difficulty of running spring gravimeters in a continuous fashion under
the adverse conditions normally encountered on the summit zone of an active volcano
Recent insights on the penumbra formation process
Using high-resolution spectropolarimetric data acquired by \textit{IBIS}, as
well as \textit{SDO}/HMI observations, we studied the penumbra formation in AR
NOAA 11490 and in a sample of twelve ARs appeared on the solar disk on 2011 and
2012, which were characterized by -type magnetic field configuration.
The results show that the onset of the classical Evershed flow occurs in a very
short time scale, 1-3 hours. Studying the formation of the first penumbral
sector around the following proto-spot, we found that a stable penumbra forms
in the area facing the opposite polarity, which appears to be co-spatial with
an AFS, i.e. in a flux emergence region, in contrast with the results of
\cite{Schlichenmaier2010} concerning the leading polarity of AR NOAA 11490.
Conversely, analyzing the sample of twelve ARs, we noticed that there is not a
preferred location for the formation of the first penumbral sector. We also
observed before the penumbra formation an inverse Evershed flow, which changes
its sign when the penumbra appears. This confirms the observational evidence
that the appearance of the penumbral filaments is correlated with the
transition from the inverse Evershed to the classical Evershed flow.
Furthermore, the analysis suggests that the time needed to form the penumbra
may be related to the location where the penumbra first appears. New
high-resolution observations, like those that will be provided by the European
Solar Telescope, are expected to increase our understanding of the penumbra
formation process.Comment: 3 pages, 2 figures, to be published in "Nuovo Cimento C" as
proceeding of the Third Meeting of the Italian Solar and Heliospheric
Communit
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