Search Publications

Saturn's quasiperiodic magnetohydrodynamic waves
DOI: 10.1002/2016GL071069 Bibcode: 2016GeoRL..4311102Y

Coates, A. J.; Dougherty, M. K.; Hospodarsky, G. B. +11 more

Quasiperiodic ∼1 h fluctuations have been recently reported by numerous instruments on board the Cassini spacecraft. The interpretation of the sources of these fluctuations has remained elusive to date. Here we provide an explanation for the origin of these fluctuations using magnetometer observations. We find that magnetic field fluctuations at h…

2016 Geophysical Research Letters
Cassini 14
Cluster observations of reflected EMIC-triggered emission
DOI: 10.1002/2016GL069096 Bibcode: 2016GeoRL..43.4164G

Santolík, O.; Cornilleau-Wehrlin, N.; Masson, A. +2 more

On 19 March 2001, the Cluster fleet recorded an electromagnetic rising tone on the nightside of the plasmasphere. The emission was found to propagate toward the Earth and toward the magnetic equator at a group velocity of about 200 km/s. The Poynting vector is mainly oblique to the background magnetic field and directed toward the Earth. The propa…

2016 Geophysical Research Letters
Cluster 11
Mass wasting on Phobos triggered by an evolving tidal environment
DOI: 10.1002/2016GL071650 Bibcode: 2016GeoRL..4312371S

Shi, X.; Oberst, J.; Willner, K.

The Martian moon Phobos is experiencing orbital decay, increasing tidal forces, and possible disruption in the near future. We suggest that this changing dynamic tidal environment has contributed to resurfacing of the odd-shaped small moon. We investigated mass wasting features in craters using high-resolution images acquired by the Mars Express o…

2016 Geophysical Research Letters
MEx 11
Cone angle control of the interaction of magnetic clouds with the Earth's bow shock
DOI: 10.1002/2016GL068818 Bibcode: 2016GeoRL..43.4781T

Escoubet, C. P.; Kilpua, E. K. J.; Turc, L. +2 more

We study the interaction of magnetic clouds (MCs) with the near-Earth environment. Recent works suggest that the bow shock crossing may modify significantly the magnetic structure of an MC, and thus its ability to drive geomagnetic storms. This change is largely controlled by the bow shock configuration, which depends on the upstream interplanetar…

2016 Geophysical Research Letters
Cluster 10
Generation of He+ and O+ EMIC waves by the bunch distribution of O+ ions associated with fast magnetosonic shocks in the magnetosphere
DOI: 10.1002/2016GL070465 Bibcode: 2016GeoRL..43.9406L

Lee, L. C.; Lee, K. H.

Electromagnetic ion cyclotron (EMIC) waves are often observed in the magnetosphere with frequency usually in the H+ and He+ cyclotron bands and sometimes in the O+ band. The temperature anisotropy, caused by injection of energetic ions or by compression of magnetosphere, can efficiently generate H+ EMIC …

2016 Geophysical Research Letters
Cluster 9
Dipolarization front and current disruption
DOI: 10.1002/2016GL070980 Bibcode: 2016GeoRL..4310050L

Lui, A. T. Y.

The modification of current density on the dawn-dusk cross section of the magnetotail with the earthward approach of a dipolarization front (DF) is examined through the recently published results of a three-dimensional (3-D) particle-in-cell (PIC) simulation. It is found that the current density intensifies by 37% abruptly within 1.5 ion gyrotime …

2016 Geophysical Research Letters
Cluster 9
A case study of a density structure over a vertical magnetic field region in the Martian ionosphere
DOI: 10.1002/2016GL068686 Bibcode: 2016GeoRL..43.4665D

Gurnett, D. A.; Lundin, R.; Morgan, D. D. +3 more

One of the discoveries made by the radar sounder on the Mars Express spacecraft is the existence of magnetically controlled structures in the ionosphere of Mars, which result in bulges in the ionospheric electron density contours. These bulges lead in turn to oblique echoes, which show up as hyperbola-shaped features in the echograms. A hyperbola-…

2016 Geophysical Research Letters
MEx 9
Two interacting X lines in magnetotail: Evolution of collision between the counterstreaming jets
DOI: 10.1002/2016GL069823 Bibcode: 2016GeoRL..43.7795A

Retinò, Alessandro; Nakamura, Rumi; Nakamura, Takuma +5 more

We study the process of collision between the counterstreaming jets flowing out from two reconnection sites in the Earth's magnetotail. The X lines, bracketing the region of jets collision, were passing by two Cluster probes successively in tailward direction. Two probes observed two different stages of the collision process. At the jets collision…

2016 Geophysical Research Letters
Cluster 6
Thin energetic O+ layer embedded in the magnetotail reconnection current sheet observed by Cluster
DOI: 10.1002/2016GL071184 Bibcode: 2016GeoRL..4311493W

Sun, W. J.; Fu, S. Y.; Zong, Q. G. +6 more

In the classical picture of the magnetotail current sheet, the current carriers are mainly ions that undergo nonadiabatic motions. Oxygen ions could contribute a thicker current sheet than the protons due to their large gyroradii. In this paper, however, we report a thin energetic O+ layer embedded in the magnetotail proton current shee…

2016 Geophysical Research Letters
Cluster 4
Ducted electromagnetic waves in the Martian ionosphere detected by the Mars Advanced Radar for Subsurface and Ionosphere Sounding radar
DOI: 10.1002/2016GL069591 Bibcode: 2016GeoRL..43.7381Z

Huang, Qian; Zhang, Jie; Orosei, Roberto +1 more

In the data of the Mars Advanced Radar for Subsurface and Ionosphere Sounding on board the European Space Agency (ESA) mission Mars Express (MEX), a distinctive type of signals (called the "epsilon signature"), which is similar to that previously detected during radio sounding of the terrestrial F region ionosphere, is found. The signature is inte…

2016 Geophysical Research Letters
MEx 3