115 research outputs found
Nature of stochastic ion heating in the solar wind: testing the dependence on plasma beta and turbulence amplitude
The solar wind undergoes significant heating as it propagates away from the
Sun; the exact mechanisms responsible for this heating are not yet fully
understood. We present for the first time a statistical test for one of the
proposed mechanisms, stochastic ion heating. We use the amplitude of magnetic
field fluctuations near the proton gyroscale as a proxy for the ratio of
gyroscale velocity fluctuations to perpendicular (with respect to the magnetic
field) proton thermal speed, defined as . Enhanced proton
temperatures are observed when is larger than a critical value
(). This enhancement strongly depends on the proton plasma
beta (); when only the perpendicular proton
temperature increases, while for increased
parallel and perpendicular proton temperatures are both observed. For
smaller than the critical value and no
enhancement of is observed while for minor increases
in are measured. The observed change of proton temperatures
across a critical threshold for velocity fluctuations is in agreement with the
stochastic ion heating model of Chandran et al. (2010). We find that
in 76\% of the studied periods implying that
stochastic heating may operate most of the time in the solar wind at 1 AU.Comment: Accepted for publication in The Astrophysical Journal Letter
Empirical Constraints on Proton and Electron Heating in the Fast Solar Wind
We analyze measured proton and electron temperatures in the high-speed solar
wind in order to calculate the separate rates of heat deposition for protons
and electrons. When comparing with other regions of the heliosphere, the fast
solar wind has the lowest density and the least frequent Coulomb collisions.
This makes the fast wind an optimal testing ground for studies of collisionless
kinetic processes associated with the dissipation of plasma turbulence. Data
from the Helios and Ulysses plasma instruments were collected to determine mean
radial trends in the temperatures and the electron heat conduction flux between
0.29 and 5.4 AU. The derived heating rates apply specifically for these mean
plasma properties and not for the full range of measured values around the
mean. We found that the protons receive about 60% of the total plasma heating
in the inner heliosphere, and that this fraction increases to approximately 80%
by the orbit of Jupiter. A major factor affecting the uncertainty in this
fraction is the uncertainty in the measured radial gradient of the electron
heat conduction flux. The empirically derived partitioning of heat between
protons and electrons is in rough agreement with theoretical predictions from a
model of linear Vlasov wave damping. For a modeled power spectrum consisting
only of Alfvenic fluctuations, the best agreement was found for a distribution
of wavenumber vectors that evolves toward isotropy as distance increases.Comment: 11 pages (emulateapj style), 5 figures, ApJ, in pres
Strong Preferential Ion Heating is Limited to within the Solar Alfvén Surface
The decay of the solar wind helium-to-hydrogen temperature ratio due to Coulomb thermalization can be used to measure how far from the Sun strong preferential ion heating occurs. Previous work has shown that a zone of preferential ion heating, resulting in mass-proportional temperatures, extends about 20-40 R-circle dot from the Sun on average. Here we look at the motion of the outer boundary of this zone with time and compare it to other physically meaningful distances. We report that the boundary moves in lockstep with the Alfven point over the solar cycle, contracting and expanding with solar activity with a correlation coefficient of better than 0.95 and with an rms difference of 4.23 R-circle dot. Strong preferential ion heating is apparently predominately active below the Alfven surface. To definitively identify the underlying preferential heating mechanisms, it will be necessary to make in situ measurements of the local plasma conditions below the Alfven surface. We predict that the Parker Solar Probe (PSP) will be the first spacecraft to directly observe this heating in action, but only a couple of years after launch as activity increases, the zone expands, and PSP's perihelion drops.Wind grant [NNX14AR78G]; NASA HSR grant [NNX16AM23G]Open access articleThis item from the UA Faculty Publications collection is made available by the University of Arizona with support from the University of Arizona Libraries. If you have questions, please contact us at [email protected]
Large-scale Control of Kinetic Dissipation in the Solar Wind
In this Letter we study the connection between the large-scale dynamics of
the turbulence cascade and particle heating on kinetic scales. We find that the
inertial range turbulence amplitude (; measured in the range of
0.01-0.1 Hz) is a simple and effective proxy to identify the onset of
significant ion heating and when it is combined with , it
characterizes the energy partitioning between protons and electrons
(), proton temperature anisotropy () and scalar
proton temperature () in a way that is consistent with previous
predictions. For a fixed , the ratio of linear to nonlinear
timescales is strongly correlated with the scalar proton temperature in
agreement with Matthaeus et al., though for solar wind intervals with
some discrepancies are found. For a fixed , an
increase of the turbulence amplitude leads to higher ratios, which is
consistent with the models of Chandran et al. and Wu et al. We discuss the
implications of these findings for our understanding of plasma turbulence.Comment: Accepted in ApJ
Applying Nyquist’s method for stability determination to solar wind observations
The role instabilities play in governing the evolution of solar and astrophysical plasmas is a matter of considerable scientific interest. The large number of sources of free energy accessible to such nearly collisionless plasmas makes general modeling of unstable behavior, accounting for the temperatures, densities, anisotropies, and relative drifts of a large number of populations, analytically difficult. We therefore seek a general method of stability determination that may be automated for future analysis of solar wind observations. This work describes an efficient application of the Nyquist instability method to the Vlasov dispersion relation appropriate for hot, collisionless, magnetized plasmas, including the solar wind. The algorithm recovers the familiar proton temperature anisotropy instabilities, as well as instabilities that had been previously identified using fits extracted from in situ observations in Gary et al. (2016). Future proposed applications of this method are discussed.Plain Language SummaryWaves in some plasma systems can grow, rather than damp, in time drawing energy from the departures from equilibrium. We present a means of efficiently determining if a particular system is susceptible to such unstable behavior. Such determination is typically made by solving a difficult mathematical problem or making simplifying assumptions about the system. Our technique is compared to previously studied cases with good agreement. We then discuss plans for future application of the technique to measurements of the solar wind, a hot and tenuous magnetized plasma that fills our solar system.Key PointsAn efficient and automated algorithm for the general determination of solar wind stability is presentedThis method agrees with traditional stability calculations, including for systems with multiple sources of free energyThis method will be applied to future observations as a method for rapid determination of solar wind stabilityPeer Reviewedhttps://deepblue.lib.umich.edu/bitstream/2027.42/140016/1/jgra53745_am.pdfhttps://deepblue.lib.umich.edu/bitstream/2027.42/140016/2/jgra53745.pd
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