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  • 1
    Publication Date: 2015-08-23
    Description: Soon after the Rosetta Orbiter rendezvoused with Comet 67P/Churyumov-Gerasimenko at a solar distance of ~3.5 AU and began to fly in triangular-shaped trajectories around it, the Ion and Electron Sensor detected negative particles at energies from about one hundred eV/q to over 18 keV/q. The lower-energy particles came from roughly the direction of the comet; the higher-energy particles came from approximately the solar direction. These particles are interpreted as clusters of molecules, most likely water, which we refer to as nanograins because their inferred diameters are less than one hundred nm. Acceleration of the grains away from the comet is through gas drag by the expanding cometary atmosphere while acceleration back to the vicinity of the comet is caused partly by solar radiation pressure but mainly by the solar-wind electric field. These observations represent the first measurements of energetic charged submicron-sized dust or ice grains (nanograins) in a cometary environment.
    Print ISSN: 0094-8276
    Electronic ISSN: 1944-8007
    Topics: Geosciences , Physics
    Published by Wiley on behalf of American Geophysical Union (AGU).
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  • 2
    Publication Date: 2016-07-30
    Description: Magnetic reconnection is known to be an important process for coupling solar-wind mass and momentum into the Earth's magnetosphere. Reconnection is initiated in an electron-scale dissipation/diffusion region around an X-line but its consequences are large scale. While past experimental efforts have advanced our understanding of ion-scale physics and the consequences of magnetic reconnection, much higher spatial and temporal resolution are needed to understand the electron-scale processes that cause reconnection. The Magnetospheric Multiscale (MMS) mission was implemented to probe the electron scale of reconnection. This article reports on results from the first scan of the dayside magnetopause with MMS. Specifically we introduce a new event involving the radial traversal of guide-field reconnection to illustrate features of reconnection physics on the electron scale.
    Print ISSN: 0094-8276
    Electronic ISSN: 1944-8007
    Topics: Geosciences , Physics
    Published by Wiley on behalf of American Geophysical Union (AGU).
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  • 3
    Publication Date: 2015-06-20
    Description: As Rosetta was orbiting Comet 67P/Churyumov-Gerasimenko, the Ion and Electron Sensor detected negative particles with angular distributions like those of the concurrently-measured solar-wind protons but with fluxes of only about 10% of the proton fluxes and energies of about 90% of the proton energies. Using well-known cross sections and energy-loss data, it is determined that the fluxes and energies of the negative particles are consistent with the production of H − ions in the solar wind by double charge exchange with molecules in the coma.
    Print ISSN: 0094-8276
    Electronic ISSN: 1944-8007
    Topics: Geosciences , Physics
    Published by Wiley on behalf of American Geophysical Union (AGU).
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  • 4
    Publication Date: 2011-02-18
    Description: Probability maps for encountering the reconnection electron diffusion region of the dayside magnetopause have been developed using a model of reconnection and solar wind observations. The maps indicate that along the magnetopause surface, the chance of directly sampling the diffusion region during a given season varies considerably. The probability distribution depends strongly on the distribution of interplanetary magnetic field directions and, also, is significantly influenced by the Earth's intrinsic magnetic dipole field tilt angle. The probability also scales with the assumed size of the diffusion region. The probability distribution shows little dependence on the phase of the solar cycle.
    Print ISSN: 0148-0227
    Topics: Geosciences , Physics
    Published by Wiley on behalf of American Geophysical Union (AGU).
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  • 5
    Publication Date: 2017-11-01
    Description: We use theory and simulations to study how the out-of-plane (guide) magnetic field strength modifies the location where the energy conversion rate between the electric field and the plasma is appreciable during asymmetric magnetic reconnection, motivated by observations (Genestreti et al. , this issue). For weak guide fields, energy conversion is maximum on the magnetospheric side of the X-line, midway between the X-line and electron stagnation point. As the guide field increases, the electron stagnation point gets closer to the X-line, and energy conversion occurs closer to the electron stagnation point. We motivate one possible non-rigorous approach to extend the theory of the stagnation point location to include a guide field. The predictions are compared to two-dimensional particle-in-cell (PIC) simulations with vastly different guide fields. The simulations have upstream parameters corresponding to three events observed with MMS. The predictions agree reasonably well with the simulation results, capturing trends with the guide field. The theory correctly predicts that the X-line and stagnation points approach each other as the guide field increases. The results are compared to MMS observations, Active Magnetosphere and Planetary Electrodynamics Response Experiment (AMPERE) observations of each event, and a global resistive magnetohydrodynamics simulation of the 2015 Oct 16 event. The PIC simulation results agree well with the global observations and simulation, but differ in the strong electric fields and energy conversion rates found in MMS observations. The observational, theoretical, and numerical results suggest that the strong electric fields observed by MMS do not represent a steady global reconnection rate.
    Print ISSN: 0148-0227
    Topics: Geosciences , Physics
    Published by Wiley on behalf of American Geophysical Union (AGU).
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  • 6
    Publication Date: 2019
    Description: Abstract Debate persists concerning the timing and geodynamics of intercontinental collision, style of syn‐collisional deformation, and development of topography and fold‐and‐thrust belts along the 〉1700‐km‐long İzmir‐Ankara‐Erzincan suture zone (İAESZ) in Turkey. Resolving this debate is a necessary precursor to evaluating the integrity of convergent margin models, and kinematic, topographic and biogeographic reconstructions of the Mediterranean domain. Geodynamic models argue either for a synchronous or diachronous collision during either the Late Cretaceous and/or Eocene, followed by Eocene slab breakoff and post‐collisional magmatism. We investigate the collision chronology in western Anatolia as recorded in the sedimentary archives of the 90‐km‐long Sarıcakaya Basin perched at shallow structural levels along the İAESZ. Based on new zircon U‐Pb geochronology, and depositional environment and sedimentary provenance results, we demonstrate that the Sarıcakaya Basin is an Eocene sedimentary basin with sediment sourced from both the İAESZ and Söğüt Thrust fault to the south and north, respectively, and formed primarily by flexural loading from north‐south shortening along the syn‐collisional Söğüt Thrust. Our results refine the timing of collision between the Anatolides and Pontide terranes in western Anatolia to Maastrichtian‐Middle Paleocene, and Early Eocene crustal shortening and basin formation. Furthermore, we demonstrate contemporaneous collision, deformation and magmatism across the İAESZ, supporting synchronous collision models. We show that regional post‐collisional magmatism can be explained by renewed underthrusting instead of slab breakoff. This new İAESZ chronology provides additional constraints for kinematic, geodynamic and biogeographic reconstructions of the Mediterranean domain.
    Print ISSN: 0278-7407
    Electronic ISSN: 1944-9194
    Topics: Geosciences
    Published by Wiley on behalf of American Geophysical Union (AGU).
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