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Dive into the research topics where A. Retinò is active.

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Featured researches published by A. Retinò.


Geophysical Research Letters | 2006

Structure of the separatrix region close to a magnetic reconnection X-line: Cluster observations

A. Retinò; Andris Vaivads; Mats André; F. Sahraoui; Y. V. Khotyaintsev; Jolene S. Pickett; M. B. Bavassano Cattaneo; M. F. Marcucci; M. W. Morooka; C. J. Owen; Stephan C. Buchert; N. Cornilleau-Wehrlin

We use Cluster spacecraft observations to study in detail the structure of a magnetic reconnection separatrix region on the magnetospheric side of the magnetopause about 50 ion inertial lengths away from the X-line. The separatrix region is the region between the magnetic separatrix and the reconnection jet. It is several ion inertial lengths wide and it contains a few subregions showing different features in particle and wave data. One subregion, a density cavity adjacent to the separatrix, has strong electric fields, electron beams and intense wave turbulence. The separatrix region shows structures even at smaller scales, for example, solitary waves at Debye length scale. We describe in detail electron distribution functions and electric field spectra in the separatrix region and we compare them to a numerical simulation. Our observations show that while reconnection is ongoing the separatrix region is highly structured and dynamic in the electric field even if the X-line is up to 50 ion inertial lengths away.


Geophysical Research Letters | 2013

Dipolarization fronts as a consequence of transient reconnection : In situ evidence

Huishan Fu; Jinbin Cao; Yu. V. Khotyaintsev; M. I. Sitnov; A. Runov; S. Y. Fu; Maria Hamrin; Mats André; A. Retinò; Y. D. Ma; H. Y. Lu; X. H. Wei; Shiyong Huang

Dipolarization fronts (DFs) are frequently detected in the Earths magnetotail from X-GSM=-30 R-E to X-GSM=-7 R-E. How these DFs are formed is still poorly understood. Three possible mechanisms have been suggested in previous simulations: (1) jet braking, (2) transient reconnection, and (3) spontaneous formation. Among these three mechanisms, the first has been verified by using spacecraft observation, while the second and third have not. In this study, we show Cluster observation of DFs inside reconnection diffusion region. This observation provides in situ evidence of the second mechanism: Transient reconnection can produce DFs. We suggest that the DFs detected in the near-Earth region (X-GSM>-10 R-E) are primarily attributed to jet braking, while the DFs detected in the mid- or far-tail region (X-GSM<-15 R-E) are primarily attributed to transient reconnection or spontaneous formation. In the jet-braking mechanism, the high-speed flow pushes the preexisting plasmas to produce the DF so that there is causality between high-speed flow and DF. In the transient-reconnection mechanism, there is no causality between high-speed flow and DF, because the frozen-in condition is violated.


Geophysical Research Letters | 2012

Electron acceleration in the reconnection diffusion region: Cluster observations

S. Y. Huang; Andris Vaivads; Yuri V. Khotyaintsev; M. Zhou; Huishan Fu; A. Retinò; X. H. Deng; Mats André; C. M. Cully; Jiansen He; F. Sahraoui; Zhigang Yuan; Y. Pang

We present one case study of magnetic islands and energetic electrons in the reconnection diffusion region observed by the Cluster spacecraft. The cores of the islands are characterized by strong c ...


Journal of Geophysical Research | 2007

Quantitative estimates of magnetic field reconnection properties from electric and magnetic field measurements

F. S. Mozer; A. Retinò

Reconnection occurs in a reconnection magnetic field geometry when there are positive electric field components tangential to the magnetopause and a magnetic field component normal to it. Because these three components are the smallest of the six electric and magnetic fields, their magnitudes are difficult to determine because of errors in, or oscillations of, the assumed constant direction normal to the current sheet. A method is described for minimizing these errors by appropriate selection of the normal direction and by analyzing the correlations between the large normal electric field and the large tangential magnetic field. The correlation coefficients are equal to ratios of the small fields, which are combined with the less accurate measurements of the averages of the small fields to produce best estimates of the small fields. For more than 120 magnetopause crossings, about 40% had such correlations that signify static conditions during those crossings. This method is applied to 22 polar subsolar magnetopause crossings to show that most were located in the ion diffusion region, as defined by the change of the total magnetic field, and that 14 had a large and steady reconnection rate with a zero parallel electric field. In these events the reconnection rate decreased with increasing guide magnetic field.


Geophysical Research Letters | 2016

Currents and associated electron scattering and bouncing near the diffusion region at Earth's magnetopause

B. Lavraud; Y. C. Zhang; Y. Vernisse; D. J. Gershman; J. C. Dorelli; P. A. Cassak; J. Dargent; C. J. Pollock; B. Giles; N. Aunai; M. R. Argall; L. A. Avanov; Alexander C. Barrie; J. L. Burch; M. O. Chandler; Li-Jen Chen; G. Clark; I. J. Cohen; Victoria N. Coffey; J. P. Eastwood; J. Egedal; S. Eriksson; R. E. Ergun; C. J. Farrugia; S. A. Fuselier; Vincent Génot; D. B. Graham; E. E. Grigorenko; H. Hasegawa; Christian Jacquey

Based on high-resolution measurements from NASAs Magnetospheric Multiscale mission, we present the dynamics of electrons associated with current systems observed near the diffusion region of magnetic reconnection at Earths magnetopause. Using pitch angle distributions (PAD) and magnetic curvature analysis, we demonstrate the occurrence of electron scattering in the curved magnetic field of the diffusion region down to energies of 20 eV. We show that scattering occurs closer to the current sheet as the electron energy decreases. The scattering of inflowing electrons, associated with field-aligned electrostatic potentials and Hall currents, produces a new population of scattered electrons with broader PAD which bounce back and forth in the exhaust. Except at the center of the diffusion region the two populations are collocated and appear to behave adiabatically: the inflowing electron PAD focuses inward (toward lower magnetic field), while the bouncing population PAD gradually peaks at 90° away from the center (where it mirrors owing to higher magnetic field and probable field-aligned potentials).


The Astrophysical Journal | 2015

THIN CURRENT SHEETS AND ASSOCIATED ELECTRON HEATING IN TURBULENT SPACE PLASMA

A. Chasapis; A. Retinò; F. Sahraoui; Andris Vaivads; Yuri V. Khotyaintsev; David Sundkvist; A. Greco; Luca Sorriso-Valvo; P. Canu

Intermittent structures, such as thin current sheets, are abundant in turbulent plasmas. Numerical simulations indicate that such current sheets are important sites of energy dissipation and particle heating occurring at kinetic scales. However, direct evidence of dissipation and associated heating within current sheets is scarce. Here, we show a new statistical study of local electron heating within proton-scale current sheets by using high-resolution spacecraft data. Current sheets are detected using the Partial Variance of Increments (PVI) method which identifies regions of strong intermittency. We find that strong electron heating occurs in high PVI (>3) current sheets while no significant heating occurs in low PVI cases ( 5) show the strongest heating and most of the time are consistent with ongoing magnetic reconnection. This suggests that reconnection is important for electron heating and dissipation at kinetic scales in turbulent plasmas.


Geophysical Research Letters | 2016

Electron jet of asymmetric reconnection

Yuri V. Khotyaintsev; D. B. Graham; C. Norgren; Wenya Li; Andreas Johlander; Andris Vaivads; Mats André; P. L. Pritchett; A. Retinò; T. D. Phan; R. E. Ergun; K. A. Goodrich; P.-A. Lindqvist; Göran Marklund; O. Le Contel; F. Plaschke; W. Magnes; R. J. Strangeway; C. T. Russell; H. Vaith; M. R. Argall; C. A. Kletzing; R. Nakamura; R. B. Torbert; W. R. Paterson; D. J. Gershman; J. C. Dorelli; L. A. Avanov; B. Lavraud; Y. Saito

We present Magnetospheric Multiscale observations of an electron-scale current sheet and electron outflow jet for asymmetric reconnection with guide field at the subsolar magnetopause. The electron ...


Journal of Geophysical Research | 2013

Asymmetric distribution of reconnection jet fronts in the Jovian nightside magnetosphere

Satoshi Kasahara; E. A. Kronberg; Tomoki Kimura; Chihiro Tao; S. V. Badman; A. Masters; A. Retinò; N. Krupp; M. Fujimoto

Magnetic reconnection plays important roles in mass transport and energy conversion in planetary magnetospheres. It is considered that transient reconnection causes localized auroral arcs or spots in the Jovian magnetosphere, by analogy to the case in the Earths magnetosphere. However, the local structures of transient reconnection events (i.e., magnetospheric plasma parameters) and their spatial distribution have not been extensively investigated for the Jovian magnetosphere. Here we examine plasma velocity and density during strong north-south magnetic field events in the Jovian nightside magnetosphere, which may be associated with tail reconnection. We find prominent reconnection jet fronts predominantly on the dawnside of the nightside magnetosphere, which would be a signature unique to rotation-dominant planetary magnetospheres. The observed plasma structures are consistent with significant field-aligned currents which would generate localized aurora.


Geophysical Research Letters | 2017

Intermittent energy dissipation by turbulent reconnection

Huishan Fu; Andris Vaivads; Yuri V. Khotyaintsev; Mats André; J. B. Cao; Vyacheslav Olshevsky; J. P. Eastwood; A. Retinò

Magnetic reconnection—the process responsible for many explosive phenomena in both nature and laboratory—is efficient at dissipating magnetic energy into particle energy. To date, exactly how this dissipation happens remains unclear, owing to the scarcity of multipoint measurements of the “diffusion region” at the sub-ion scale. Here we report such a measurement by Cluster—four spacecraft with separation of 1/5 ion scale. We discover numerous current filaments and magnetic nulls inside the diffusion region of magnetic reconnection, with the strongest currents appearing at spiral nulls (O-lines) and the separatrices. Inside each current filament, kinetic-scale turbulence is significantly increased and the energy dissipation, E′ ⋅ j, is 100 times larger than the typical value. At the jet reversal point, where radial nulls (X-lines) are detected, the current, turbulence, and energy dissipations are surprisingly small. All these features clearly demonstrate that energy dissipation in magnetic reconnection occurs at O-lines but not X-lines.


Nature Physics | 2013

Electron acceleration to relativistic energies at a strong quasi-parallel shock wave

A. Masters; L. Stawarz; M. Fujimoto; S. J. Schwartz; N. Sergis; M. F. Thomsen; A. Retinò; H. Hasegawa; B. Zieger; G. R. Lewis; A. J. Coates; P. Canu; M. K. Dougherty

Data from the Cassini spacecraft identify strong electron acceleration as the solar wind approaches the magnetosphere of Saturn. This so-called bow shock unexpectedly occurs even when the magnetic field is roughly parallel to the shock-surface normal. Knowledge of the magnetic dependence of electron acceleration will aid understanding of supernova remnants.

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Andris Vaivads

Swedish Institute of Space Physics

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R. Nakamura

Austrian Academy of Sciences

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R. E. Ergun

University of Colorado Boulder

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Yu. V. Khotyaintsev

Swedish Institute of Space Physics

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M. Fujimoto

Tokyo Institute of Technology

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W. Baumjohann

Austrian Academy of Sciences

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J. L. Burch

Southwest Research Institute

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B. Lavraud

University of Toulouse

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Mats André

Swedish Institute of Space Physics

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Yuri V. Khotyaintsev

Swedish Institute of Space Physics

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