Search Publications

Increases in plasma sheet temperature with solar wind driving during substorm growth phases
DOI: 10.1002/2014GL062400 Bibcode: 2014GeoRL..41.8713F

Jackman, C. M.; Dandouras, I.; Fazakerley, A. N. +10 more

During substorm growth phases, magnetic reconnection at the magnetopause extracts ~1015 J from the solar wind which is then stored in the magnetotail lobes. Plasma sheet pressure increases to balance magnetic flux density increases in the lobes. Here we examine plasma sheet pressure, density, and temperature during substorm growth phase…

2014 Geophysical Research Letters
Cluster 22
Evidence of strong energetic ion acceleration in the near-Earth magnetotail
DOI: 10.1002/2014GL060252 Bibcode: 2014GeoRL..41.3724L

Fränz, M.; Wei, Y.; Daly, P. W. +6 more

Until now it is still questionable whether ions are accelerated to energies above 100 keV in the near-Earth current sheet (CS), in the vicinity of a possible near-Earth neutral line. By using 11 years of 3-D energetic ion flux data for protons, helium, and oxygen (~150 keV-1 MeV) from the RAPID instrument on board Cluster 4, we statistically study…

2014 Geophysical Research Letters
Cluster 22
Can magnetopause reconnection drive Saturn's magnetosphere?
DOI: 10.1002/2014GL059288 Bibcode: 2014GeoRL..41.1862M

Coates, A. J.; Russell, C. T.; Dougherty, M. K. +3 more

While solar wind-driven compression of Saturn's magnetosphere is an important trigger of magnetospheric dynamics, the importance of magnetopause reconnection has been the subject of debate. Here we use Cassini observations at Saturn's magnetopause to address this open issue. Measured conditions at the boundary suggest a typical reconnection electr…

2014 Geophysical Research Letters
Cassini 21
Fresh exposures of hydrous Fe-bearing amorphous silicates on Mars
DOI: 10.1002/2014GL062065 Bibcode: 2014GeoRL..41.8744W

Weitz, Catherine M.; Bishop, Janice L.; Baker, Leslie L. +1 more

We have discovered relatively fresh exposures of a hydrated, amorphous material along the wall rock slopes in Coprates Chasma, Mars. Visible and near-infrared reflectance spectra extracted from the deposits exhibit broad absorptions around 1.42, 1.94, and 2.25 µm that are most consistent with laboratory spectra of nanophase hydrated Fe-rich alloph…

2014 Geophysical Research Letters
MEx 21
The scale of the magnetotail reconnecting current sheet in the presence of O+
DOI: 10.1002/2014GL060440 Bibcode: 2014GeoRL..41.4819L

Kistler, L. M.; Mouikis, C. G.; Liu, Y. H. +2 more

The reconnection current layer thickness is expected to scale with either the ion inertial length or the ion gyroradius. Both of these quantities scale with the mass of the ions present. During geomagnetically disturbed times, the reconnection layer in the magnetotail can contain a significant amount of O+. Using Cluster multi-spacecraf…

2014 Geophysical Research Letters
Cluster 20
Discrepancy between ionopause and photoelectron boundary determined from Mars Express measurements
DOI: 10.1002/2014GL062287 Bibcode: 2014GeoRL..41.8221H

Barabash, S.; Wei, Y.; Andrews, D. J. +9 more

The Martian ionosphere directly interacts with the solar wind due to lack of a significant intrinsic magnetic field, and an interface is formed in between. The interface is usually recognized by two kinds of indicators: the ionopause identified from ionospheric density profiles and the photoelectron boundary (PEB) determined from the electron ener…

2014 Geophysical Research Letters
MEx 20
Nanodust detection near 1 AU from spectral analysis of Cassini/Radio and Plasma Wave Science data
DOI: 10.1002/2014GL060566 Bibcode: 2014GeoRL..41.5382S

Schippers, P.; André, N.; Kurth, W. S. +3 more

Nanodust grains of a few nanometers in size are produced near the Sun by collisional breakup of larger grains and picked up by the magnetized solar wind. They have so far been detected at 1 AU by only the two STEREO spacecraft. Here we analyze the spectra measured by the radio and plasma wave instrument onboard Cassini during the cruise phase clos…

2014 Geophysical Research Letters
Cassini 19
The ionosphere of Saturn as observed by the Cassini Radio Science System
DOI: 10.1002/2014GL060512 Bibcode: 2014GeoRL..41.5778K

Anabtawi, Aseel; Barbinis, Elias; Fleischman, Don +5 more

Fifty-nine ionsopheric radio occultation observations of the vertical electron density profile in the Saturn ionosphere have been made since the Cassini spacecraft was inserted in orbit around Saturn in 2004. Significant orbit to orbit variations were observed, but the general trend noted in earlier orbits, namely, increasing electron densities wi…

2014 Geophysical Research Letters
Cassini 17
Ion energization and transport associated with magnetic dipolarizations
DOI: 10.1002/2014GL061209 Bibcode: 2014GeoRL..41.5717P

El-Alaoui, Mostafa; Walker, Raymond J.; Ashour-Abdalla, Maha +1 more

Ion energization in the magnetotail during substorms is examined by simulating a modest substorm event that occurred on 7 February 2009. The simulation scheme combines global magnetohydrodynamic (MHD) modeling of the magnetosphere driven by realistic upstream solar wind conditions, with a large-scale kinetics (LSK) simulation. Multiple earthward p…

2014 Geophysical Research Letters
Cluster 16
Discontinuities in the magnetic field near Enceladus
DOI: 10.1002/2014GL060081 Bibcode: 2014GeoRL..41.3359S

Dougherty, Michele K.; Saur, Joachim; Kriegel, Hendrik +2 more

The plasma interaction of Saturn's icy moon Enceladus generates a hemisphere coupling current system that directly connects the giant planet's northern and southern polar magnetosphere. Based on Cassini magnetometer observations from all 20 targeted Enceladus flybys between 2004 and 2014, we study the magnetic field discontinuities associated with…

2014 Geophysical Research Letters
Cassini 15