9 research outputs found
Acceleration of electrons by whistler-mode hiss waves at Saturn
Plasmaspheric hiss waves at the Earth are well known for causing losses of electrons from the radiation belts through wave particle interactions. At Saturn, however, we show that the different plasma density environment leads to acceleration of the electrons rather than loss. The ratio of plasma frequency to electron gyrofrequency frequently falls below one creating conditions for hiss to accelerate electrons. The location of hiss at high latitudes ( > 25Ā°) coincides very well with this region of very low density. The interaction between electrons and hiss only occurs at these higher latitudes, therefore the acceleration is limited to mid to low pitch angles leading to butterfly pitch angle distributions. The hiss is typically an order of magnitude stronger than chorus at Saturn and the resulting acceleration is rapid, approaching steady state in one day at 0.4 MeV at L=7 and the effect is stronger with increasing L-shell
Rapid electron acceleration in low density regions of Saturn's radiation belt by whistler mode chorus waves
Electron acceleration at Saturn due to whistler mode chorus waves has previously been assumed to be ineffective; new data closer to the planet shows it can be very rapid (factor of 104 flux increase at 1 MeV in 10 days compared to factor of 2). A full survey of chorus waves at Saturn is combined with an improved plasma density model to show that where the plasma frequency falls below the gyrofrequency additional strong resonances are observed favoring electron acceleration. This results in strong chorus acceleration between approximately 2.5 RS and 5.5 RS outside which adiabatic transport may dominate. Strong pitch angle dependence results in butterfly pitch angle distributions that flatten over a few days at 100s keV, tens of days at MeV energies which may explain observations of butterfly distributions of MeV electrons near L=3. Including cross terms in the simulations increases the tendency towards butterfly distributions
A new approach to constructing models of electron diffusion by EMIC waves in the radiation belts
Electromagnetic Ion Cyclotron (EMIC) waves play an important role in relativistic electron losses in the radiation belts through diffusion via resonant waveāparticle interactions. We present a new approach for calculating bounce and driftāaveraged EMIC electron diffusion coefficients. We calculate bounceāaveraged diffusion coefficients, using quasiālinear theory, for each individual CRRES EMIC wave observation using fitted wave properties, the plasma density and the background magnetic field. These calculations are then combined into bounceāaveraged diffusion coefficients. The resulting coefficients therefore capture the combined effects of individual spectra and plasma properties as opposed to previous approaches that use average spectral and plasma properties, resulting in diffusion over a wider range of energies and pitchāangles. These calculations, and their role in radiation belt simulations, are then compared against existing diffusion models. The new diffusion coefficients are found to significantly improve the agreement between the calculated decay of relativistic electrons and Van Allen Probes data
A case study of HF radar spectral width in the post midnight magnetic local time sector and its relationship to the polar cap boundary
International audienceThe aim of this paper is to advance the current understanding of the spectral width parameter observed by coherent high frequency (HF) radars. In particular, we address the relationship of a frequently observed gradient, between low ( 200 m/s) spectral width, to magnetospheric boundaries. Previous work has linked this gradient in the spectral width, in the nightside sector of magnetic local time, to the Polar Cap Boundary (PCB), and also to the boundary between the Central Plasma Sheet (CPS) and the Plasma Sheet Boundary Layer (PSBL). The present case study investigates the former by comparison with the 630.0 nm optical emission. No suitable data were available to test the second of the two hypotheses. It is found that during the interval in question the spectral width gradient is within the region of the 630.0 nm optical emission. A comparison of coherent and incoherent scatter radar data is also conducted, which indicates that values of high spectral width are typically collocated with elevated F-region electron temperatures. We conclude that the high spectral width region in the interval under study is associated with particle precipitation and also that the spectral width gradient is not a reliable method for locating the PCB
Interhemispheric comparison of spectral width boundary as observed by the SuperDARN radars
Previous studies have
shown that dayside equatorward edge of coherent HF radar backscatter having
broad Doppler spectral width is coincident with the equatorward edge of the
cusp particle precipitation. This enables the boundary between broad and narrow
spectral width backscatters (spectral width boundary) in the dayside magnetic
local time sector to be used as a proxy for the open/closed field line
boundary. The present case study employs magnetically conjugate SuperDARN
coherent HF radars to make an inter-hemispheric comparison of the location and
variation of the spectral width boundaries. Agreement between the magnetic
latitudes of the boundaries in both hemispheres is remarkable. Correlation
coefficients between the latitudes of the boundaries are larger than 0.70.
Temporal variation of the spectral width boundary follows the same equatorward
trend in both hemispheres. This is consistent with the accumulation of open
flux in the polar cap by dayside low-latitude magnetopause reconnection,
expected when IMF B<sub>z</sub> is negative. Boundaries in both hemispheres
also exhibit short-lived poleward motions superposed on the general
equator-ward trend, which follows the onset of substorm expansion phase and a
temporary northward excursion of IMF B<sub>z</sub> during substorm recovery
phase. There is an interhemispheric difference in response time to the substorm
occurrence between two hemispheres. The spectral width boundary in the Southern
Hemisphere starts to move poleward 10 min earlier than that in the Northern
Hemisphere. We discuss this difference in terms of interhemispheric asymmetry
of the substorm breakup region in the longitudinal direction associated with
the effect of IMF B<sub>y</sub>.<br><br><b>Key words. </b>Ionosphere
(ionosphere-magnetosphere interactions; plasma convection) ā Magnetospheric
physics (magnetopause, cusp, boundary layers
Combining incoherent scatter radar data and IRI-2007 to monitor the open-closed field line boundary during substorms
The size of the polar cap is very important for understanding the substorm process as well as reconnection rates in general. In this work we build on previous studies which use a combination of European Incoherent Scatter radar (EISCAT) electron temperature (Te) measurements from two radars running simultaneously to track the motion of the open-closed field line boundary (OCB). The second radar gives an estimate of the background variation of Te with altitude, which can then be subtracted from the radar beam being used to estimate the OCB location. We demonstrate that using the international reference ionosphere 2007 (IRI-2007) model can remove the second radar requirement and therefore increase the number of cases which could benefit from background Te subtraction. In this paper we focus our analysis on substorm intervals. We find that the IRI-2007 method produces an OCB proxy location which on average is 0.25Ā° altitude adjusted corrected geomagnetic coordinate latitude equatorward of the two-radar method. On comparing both the two-radar and IRI-2007 Te OCB finding methods with the OCB identified in the DMSP particle data and IMAGE satellite data we find that both EISCAT methods perform quite well, and neither method is particularly favored over the other. We find that the magnitude of the mean offset to the IMAGE OCB varies between 0.1Ā° and 2.7Ā° latitude, dependent on the event and the IMAGE camera used
The effects of high frequency ULF wave activity on the spectral characteristics of coherent HF radar returns: A case study
It is now a common practice to employ ground-based radars in an attempt to distinguish between those regions of the Earth's upper atmosphere which are magnetically conjugate to open and closed magnetic field lines. Radar returns from ionospheric irregularities inside the polar cap and cusp regions generally exhibit large spectral widths in contrast to those which exist on closed field lines at lower latitudes. It has been suggested that the so-called Spectral Width Boundary (SWB) might act as a proxy for the open-closed field line boundary (OCFLB), which would then be an invaluable tool for investigating reconnection rates in the magnetosphere. The exact cause of the increased spectral widths observed at very high latitudes is still subject to considerable debate. Several mechanisms have been proposed. This paper compares a dusk-sector interval of coherent HF radar data with measurements made by an induction coil magnetometer located at Troms&#248;, Norway (66&deg; N geomagnetic). On this occasion, a number of equatorward excursions of the SWB in the radar backscatter are accompanied by increases in spectral power of ULF waves in the Pc1-2 frequency band as the SWB passes overhead. Thus, these observations support the possibility that high-frequency magnetospheric wave activity at least contribute to the observed spectral characteristics and that such wave activity might play a significant role in the nightside ionosphere. <br><br><b>Key words.</b> Ionosphere (auroral ionosphere) ā Magnetospheric physics (MHD waves and instabilities) ā Radio science (ionospheric physics