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  • 1.
    Beth, Arnaud
    et al.
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik.
    Gunell, Herbert
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik.
    Simon Wedlund, C.
    Goetz, C.
    Nilsson, H.
    Hamrin, Maria
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik.
    First investigation of the diamagnetic cavity boundary layer with a 1D3V PIC simulation2022Ingår i: Astronomy and Astrophysics, ISSN 0004-6361, E-ISSN 1432-0746, Vol. 667, artikel-id A143Artikel i tidskrift (Refereegranskat)
    Abstract [en]

    Context: Amongst the different features and boundaries encountered around comets, one remains of particular interest to the plasma community: the diamagnetic cavity. Crossed for the first time at 1P/Halley during the Giotto flyby in 1986 and later met more than 700 times by the ESA Rosetta spacecraft around Comet 67P/Churyumov-Gerasimenko, this region, almost free of any magnetic field, surrounds nuclei of active comets. However, previous observations and modelling of this part of the coma have not yet provided a definitive answer as to the origin of such a cavity and on its border, the diamagnetic cavity boundary layer.

    Aims: We investigate which forces and equilibrium might be at play and balance the magnetic pressure at this boundary down to the spatial and temporal scales of the electrons in the 1D collisionless case. In addition, we scrutinise assumptions made in magneto-hydrodynamic and hybrid simulations of this environment and check for their validity.

    Methods: We simulated this region at the electron scale by means of 1D3V particle-in-cell simulations and SMILEI code.

    Results: Across this layer, depending on the magnetic field strength, the electric field is governed by different equilibria, with a thin double-layer forming ahead. In addition, we show that the electron distribution function departs from Maxwellian and/or gyrotropic distributions and that electrons do not behave adiabatically. We demonstrate the need to investigate this region at the electron scale in depth with fully kinetic simulations.

  • 2.
    Chong, Ghai Siung
    et al.
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik.
    De Spiegeleer, Alexandre
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik.
    Hamrin, Maria
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik.
    Pitkänen, Timo
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik. Institute of Space Sciences, Shandong University, Weihai, China; Space Physics and Astronomy Research Unit, University of Oulu, Oulu, Finland.
    Gunell, Herbert
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik.
    Aizawa, S.
    Research Institute in Astrophysics and Planetology, Toulouse, France.
    Tailward Flows in the Vicinity of Fast Earthward Flows2021Ingår i: Journal of Geophysical Research - Space Physics, ISSN 2169-9380, E-ISSN 2169-9402, Vol. 126, nr 4, artikel-id e2020JA028978Artikel i tidskrift (Refereegranskat)
    Abstract [en]

    The occurrence of tailward flows in the magnetotail plasma sheet is closely linked to the dynamics of earthward bursty bulk flows (BBFs). Tailward flows that are observed in the vicinity of these BBFs (or TWABs – Tailward flows around BBFs) may hold unique information on its origin. In this study, we conduct a statistical survey on TWABs by using data from the Cluster mission. We find that TWABs are observed in the vicinity of ∼75% of the BBFs and their occurrence does not depend on BBF velocity magnitude. TWABs have a flow convection pattern consistent with the general tailward flows (GTWs) in the plasma sheet and they do not resemble vortical-like flows. However, TWABs have a flow velocity magnitude twice larger than the GTWs. The plasma density and temperature of TWABs are comparable with BBFs. It is more common to observe a TWAB succeeding than preceding a BBF. However, there is no distinctive difference (in flow pattern, plasma density and temperature) between preceding and succeeding TWABs. We suggest that TWABs are likely the “freshly” rebounded BBFs from the near-Earth region where the magnetic field is stronger. TWABs may represent the early stage of the evolution of tailward flows in the plasma sheet. We also discuss and argue that other mechanisms such as shear-induced vortical flows and tailward slipping of depleted flux tubes cannot be the principal causes of TWABs.

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  • 3.
    De Spiegeleer, Alexandre
    et al.
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik.
    Hamrin, Maria
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik.
    Gunell, Herbert
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik.
    Pitkänen, Timo
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik.
    Chong, Ghai Siung
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik.
    In Which Magnetotail Hemisphere is a Satellite? Problems Using in Situ Magnetic Field Data2021Ingår i: Journal of Geophysical Research - Space Physics, ISSN 2169-9380, E-ISSN 2169-9402, Vol. 126, nr 2, artikel-id e2020JA028923Artikel i tidskrift (Refereegranskat)
    Abstract [en]

    In Earth's magnetotail plasma sheet, the sunward-tailward Bx component of the magnetic field is often used to separate the region above and below the cross-tail current sheet. Using a three-dimensional magneto-hydrodynamic simulation, we show that high-speed flows do not only affect the north-south magnetic field component (causing dipolarization fronts), but also the sunward-tailward component via the formation of a magnetic dent. This dent is such that, in the Northern Hemisphere, the magnetic field is tailward while in the Southern Hemisphere, it is earthward. This is opposite to the expected signatures where Bx > 0 (Bx < 0) above (below) the neutral sheet. Therefore, the direction of the magnetic field cannot always be used to identify in which hemisphere an in situ spacecraft is located. In addition, the cross-tail currents associated with the dent is different from the currents in a tail without a dent. From the simulation, we suggest that the observation of a dawnward current and a tailward magnetic tension force, possibly together with an increase in the plasma beta, may indicate the presence of a magnetic dent. To exemplify, we also present data of a high-speed flow observed by the Cluster mission, and we show that the changing sign of Bx is likely due to such a dent, and not to the spacecraft moving across the neutral sheet.

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  • 4.
    De Spiegeleer, Alexandre
    et al.
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik.
    Hamrin, Maria
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik.
    Gunell, Herbert
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik.
    Volwerk, M.
    Andersson, L.
    Karlsson, T.
    Pitkänen, Timo
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik.
    Mouikis, C. G.
    Nilsson, H.
    Kistler, L. M.
    Oscillatory Flows in the Magnetotail Plasma Sheet: Cluster Observations of the Distribution Function2019Ingår i: Journal of Geophysical Research - Space Physics, ISSN 2169-9380, E-ISSN 2169-9402, Vol. 124, nr 4, s. 2736-2754Artikel i tidskrift (Refereegranskat)
    Abstract [en]

    Plasma dynamics in Earth's magnetotail is often studied using moments of the distribution function, which results in losing information on the kinetic properties of the plasma. To better understand oscillatory flows observed in the midtail plasma sheet, we investigate two events, one in each hemisphere, in the transition region between the central plasma sheet and the lobes using the 2-D ion distribution function from the Cluster 4 spacecraft. In this case study, the oscillatory flows are a manifestation of repeated ion flux enhancements with pitch angle changing from 0 degrees to 180 degrees in the Northern Hemisphere and from 180 degrees to 0 degrees in the Southern Hemisphere. Similar pitch angle signatures are observed seven times in about 80 min for the Southern Hemisphere event and three times in about 80 min for the Northern Hemisphere event. The ion flux enhancements observed for both events are slightly shifted in time between different energy channels, indicating a possible time-of-flight effect from which we estimate that the source of particle is located similar to 5-25R(E) and similar to 40-107R(E) tailward of the spacecraft for the Southern and Northern Hemisphere event, respectively. Using a test particle simulation, we obtain similar to 21-46 R-E for the Southern Hemisphere event and tailward of X similar to - 65R(E) (outside the validity region of the model) for the Northern Hemisphere event. We discuss possible sources that could cause the enhancements of ion flux.

  • 5.
    De Spiegeleer, Alexandre
    et al.
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik.
    Hamrin, Maria
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik.
    Volwerk, M.
    Karlsson, T.
    Gunell, Herbert
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik. Belgian Institute for Space Aeronomy, Brussels, Belgium.
    Chong, Ghai Siung
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik.
    Pitkänen, Timo
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik. Shandong Provincial Key Laboratory of Optical Astronomy and Solar-Terrestrial Environment, Institute of Space Sciences, Shandong University, Weihai, China.
    Nilsson, H.
    Oxygen Ion Flow Reversals in Earth's Magnetotail: A Cluster Statistical Study2019Ingår i: Journal of Geophysical Research - Space Physics, ISSN 2169-9380, E-ISSN 2169-9402, Vol. 124, nr 11, s. 8928-8942Artikel i tidskrift (Refereegranskat)
    Abstract [en]

    We present a statistical study of magnetotail flows that change direction from earthward to tailward using Cluster spacecraft. More precisely, we study 318 events of particle flux enhancements in the O+ data for which the pitch angle continuously changes with time, either from 0 degrees to 180 degrees or from 180 degrees to 0 degrees. These structures are called "Pitch Angle Slope Structures" (PASSes). PASSes for which the pitch angle changes from 0 degrees to 180 degrees are observed in the Northern Hemisphere while those for which the pitch angle changes from 180 degrees to 0 degrees are observed in the Southern Hemisphere. These flux enhancements result in a reversal of the flow direction from earthward to tailward regardless of the hemisphere where they are observed. Sometimes, several PASSes can be observed consecutively which can therefore result in oscillatory velocity signatures in the earth-tail direction. The PASS occurrence rate increases from 1.8% to 3.7% as the AE index increases from similar to 0 to similar to 600 nT. Also, simultaneously to PASSes, there is typically a decrease in the magnetic field magnitude due to a decrease (increase) of the sunward component of the magnetic field in the Northern (Southern) Hemisphere. Finally, based on the 115 (out of 318) PASSes that show energy-dispersed structures, the distance to the source from the spacecraft is estimated to be typically R-E along the magnetic field line. This study is important as it sheds light on one of the causes of tailward velocities in Earth's magnetotail.

  • 6. Echim, M. M.
    et al.
    Lamy, H.
    De Keyser, J.
    Maggiolo, R.
    Gunell, Herbert
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik. Royal Belgian Institute for Space Aeronomy, Brussels, Belgium.
    Wedlund, C. L. Simon
    A Method to Estimate the Physical Properties of Magnetospheric Generators From Observations of Quiet Discrete Auroral Arcs2019Ingår i: Journal of Geophysical Research - Space Physics, ISSN 2169-9380, E-ISSN 2169-9402, Vol. 124, nr 12, s. 10283-10293Artikel i tidskrift (Refereegranskat)
    Abstract [en]

    We discuss a method to estimate the properties of a magnetospheric generator using a quasi-electrostatic magnetosphere-ionosphere coupling model and in situ or remote sensing observations of discrete quiet arcs. We first construct an ensemble of Vlasov equilibrium solutions for generator structures formed at magnetospheric plasma interfaces. For each generator solution, we compute the ionospheric electric potential from the current continuity equation. Thus, we estimate the field-aligned potential drop that allows us to assess several properties of the discrete auroral arc, such as the field-aligned potential difference, the field-aligned current density, the flux of precipitating energy, and the height-integrated Pedersen conductance. A minimization procedure based on comparing the numerical results with observations is defined and applied to find which solution of the current continuity equation and which generator model give auroral arc properties that best fit the observations. The procedure is validated in a case study with observations by DMSP and Cluster and can be generalized to other types of data.

  • 7.
    Edberg, N.J.T.
    et al.
    Swedish Institute of Space Physics (IRF), Uppsala, Sweden.
    Eriksson, A.I.
    Swedish Institute of Space Physics (IRF), Uppsala, Sweden.
    Vigren, E.
    Swedish Institute of Space Physics (IRF), Uppsala, Sweden.
    Nilsson, H.
    Swedish Institute of Space Physics (IRF), Kiruna, Sweden.
    Gunell, Herbert
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik.
    Götz, C.
    Department of Mathematics, Physics and Electrical Engineering, Northumbria University, Newcastle-upon-Tyne, United Kingdom.
    Richter, I.
    Institut fur Geophysik und Extraterrestrische Physik, Technische Universität Braunschweig, Braunschweig, Germany.
    Henri, P.
    Laboratoire de Physique et Chimie de l'Environnement et de l'Espace, Cnrs, Orléans, France; Laboratoire Lagrange, Oca, Cnrs, Uca, Nice, France.
    De Keyser, J.
    Royal Belgian Institute for Space Aeronomy, BIRA-IASB, Brussels, Belgium.
    Scale size of cometary bow shocks2024Ingår i: Astronomy and Astrophysics, ISSN 0004-6361, E-ISSN 1432-0746, Vol. 682, artikel-id A51Artikel i tidskrift (Refereegranskat)
    Abstract [en]

    Context. In past decades, several spacecraft have visited comets to investigate their plasma environments. In the coming years, Comet Interceptor will make yet another attempt. This time, the target comet and its outgassing activity are unknown and may not be known before the spacecraft has been launched into its parking orbit, where it will await a possible interception. If the approximate outgassing rate can be estimated remotely when a target has been identified, it is desirable to also be able to estimate the scale size of the plasma environment, defined here as the region bound by the bow shock.

    Aims. This study aims to combine previous measurements and simulations of cometary bow shock locations to gain a better understanding of how the scale size of cometary plasma environments varies. We compare these data with models of the bow shock size, and we furthermore provide an outgassing rate-dependent shape model of the bow shock. We then use this to predict a range of times and cometocentric distances for the crossing of the bow shock by Comet Interceptor, together with expected plasma density measurements along the spacecraft track.

    Methods. We used data of the location of cometary bow shocks from previous spacecraft missions, together with simulation results from previously published studies. We compared these results with an existing model of the bow shock stand-off distance and expand on this to provide a shape model of cometary bow shocks. The model in particular includes the cometary outgassing rate, but also upstream solar wind conditions, ionisation rates, and the neutral flow velocity.

    Results. The agreement between the gas-dynamic model and the data and simulation results is good in terms of the stand-off distance of the bow shock as a function of the outgassing rate. For outgassing rates in the range of 1027-1031-s-1, the scale size of cometary bow shocks can vary by four orders of magnitude, from about 102 km to 106 km, for an ionisation rate, flow velocity, and upstream solar wind conditions typical of those at 1 AU. The proposed bow shock shape model shows that a comet plasma environment can range in scale size from the plasma environment of Mars to about half of that of Saturn.

    Conclusions. The model-data agreement allows for the planning of upcoming spacecraft comet encounters, such as that of Comet Interceptor, when a target has been identified and its outgassing rate is determined. We conclude that the time a spacecraft can spend within the plasma environment during a flyby can range from minutes to days, depending on the comet that is visited and on the flyby speed. However, to capture most of the comet plasma environment, including pick-up ions and upstream plasma waves, and to ensure the highest possible scientific return, measurements should still start well upstream of the expected bow shock location. From the plasma perspective, the selected target should preferably be an active comet with the lowest possible flyby velocity.

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  • 8.
    Fatemi, Shahab
    et al.
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik.
    Hamrin, Maria
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik.
    Krämer, Eva
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik.
    Gunell, Herbert
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik.
    Nordin, Gabriella
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik.
    Karlsson, T.
    School of Electric Engineering and Computer Science, KTH Royal Institute of Technology, Stockholm, Sweden.
    Goncharov, O.
    Faculty of Mathematics and Physics, Charles University, 121 16 Prague, The Czech Republic.
    Unveiling the 3D structure of magnetosheath jets2024Ingår i: Monthly notices of the Royal Astronomical Society, ISSN 0035-8711, E-ISSN 1365-2966, Vol. 531, nr 4, s. 4692-4713Artikel i tidskrift (Refereegranskat)
    Abstract [en]

    Magnetosheath jets represent localized enhancements in dynamic pressure observed within the magnetosheath. These energetic entities, carrying excess energy and momentum, can impact the magnetopause and disrupt the magnetosphere. Therefore, they play a vital role in coupling the solar wind and terrestrial magnetosphere. However, our understanding of the morphology and formation of these complex, transient events remains incomplete over two decades after their initial observation. Previous studies have relied on oversimplified assumptions, considering jets as elongated cylinders with dimensions ranging from $0.1\, R_{\rm E}$ to $5\, R_{\rm E}$ (Earth radii). In this study, we present simulation results obtained from Amitis, a high-performance hybrid-kinetic plasma framework (particle ions and fluid electrons) running in parallel on graphics processing units (GPUs) for fast and more environmentally friendly computation compared to CPU-based models. Considering realistic scales, we present the first global, three-dimensional (3D in both configuration and velocity spaces) hybrid-kinetic simulation results of the interaction between solar wind plasma and the Earth. Our high-resolution kinetic simulations reveal the 3D structure of magnetosheath jets, showing that jets are far from being simple cylinders. Instead, they exhibit intricate and highly interconnected structures with dynamic 3D characteristics. As they move through the magnetosheath, they wrinkle, fold, merge, and split in complex ways before a subset reaches the magnetopause.

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  • 9. Goetz, C.
    et al.
    Gunell, Herbert
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik.
    Volwerk, M.
    Beth, A.
    Eriksson, A.
    Galand, M.
    Henri, P.
    Nilsson, H.
    Wedlund, C. Simon
    Alho, M.
    Andersson, L.
    Andre, N.
    De Keyser, J.
    Deca, J.
    Ge, Y.
    Glassmeier, K.-H.
    Hajra, R.
    Karlsson, T.
    Kasahara, S.
    Kolmasova, I.
    LLera, K.
    Madanian, H.
    Mann, I.
    Mazelle, C.
    Odelstad, E.
    Plaschke, F.
    Rubin, M.
    Sanchez-Cano, B.
    Snodgrass, C.
    Vigren, E.
    Cometary plasma science: Open science questions for future space missions2022Ingår i: Experimental astronomy, ISSN 0922-6435, E-ISSN 1572-9508, Vol. 54, s. 1129-1167Artikel i tidskrift (Refereegranskat)
    Abstract [en]

    Comets hold the key to the understanding of our Solar System, its formation and its evolution, and to the fundamental plasma processes at work both in it and beyond it. A comet nucleus emits gas as it is heated by the sunlight. The gas forms the coma, where it is ionised, becomes a plasma, and eventually interacts with the solar wind. Besides these neutral and ionised gases, the coma also contains dust grains, released from the comet nucleus. As a cometary atmosphere develops when the comet travels through the Solar System, large-scale structures, such as the plasma boundaries, develop and disappear, while at planets such large-scale structures are only accessible in their fully grown, quasi-steady state. In situ measurements at comets enable us to learn both how such large-scale structures are formed or reformed and how small-scale processes in the plasma affect the formation and properties of these large scale structures. Furthermore, a comet goes through a wide range of parameter regimes during its life cycle, where either collisional processes, involving neutrals and charged particles, or collisionless processes are at play, and might even compete in complicated transitional regimes. Thus a comet presents a unique opportunity to study this parameter space, from an asteroid-like to a Mars- and Venus-like interaction. The Rosetta mission and previous fast flybys of comets have together made many new discoveries, but the most important breakthroughs in the understanding of cometary plasmas are yet to come. The Comet Interceptor mission will provide a sample of multi-point measurements at a comet, setting the stage for a multi-spacecraft mission to accompany a comet on its journey through the Solar System. This White Paper, submitted in response to the European Space Agency’s Voyage 2050 call, reviews the present-day knowledge of cometary plasmas, discusses the many questions that remain unanswered, and outlines a multi-spacecraft European Space Agency mission to accompany a comet that will answer these questions by combining both multi-spacecraft observations and a rendezvous mission, and at the same time advance our understanding of fundamental plasma physics and its role in planetary systems.

  • 10.
    Goetz, Charlotte
    et al.
    ESTEC, European Space Agency, Keplerlaan 1, AZ Noordwijk, Netherlands; Department of Mathematics, Physics and Electrical Engineering, Northumbria University, Newcastle-upon-Tyne, United Kingdom.
    Behar, Etienne
    Swedish Institute of Space Physics, Box 812, Kiruna, Sweden; Lagrange, OCA, UCA, CNRS, Nice, France.
    Beth, Arnaud
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik.
    Bodewits, Dennis
    Physics Department, Leach Science Center, Auburn University, AL, Auburn, United States.
    Bromley, Steve
    Physics Department, Leach Science Center, Auburn University, AL, Auburn, United States.
    Burch, Jim
    Southwest Research Institute, P.O. Drawer 28510, TX, San Antonio, United States.
    Deca, Jan
    Laboratory for Atmospheric and Space Physics, University of Colorado Boulder, 3665 Discovery Drive, CO, Boulder, United States.
    Divin, Andrey
    Earth Physics Department, St. Petersburg State University, Ulianovskaya, 1, St Petersburg, Russian Federation.
    Eriksson, Anders I.
    Swedish Institute of Space Physics, Box 537, Uppsala, Sweden.
    Feldman, Paul D.
    Department of Physics and Astronomy, Johns Hopkins University, MD, Baltimore, United States.
    Galand, Marina
    Department of Physics, Imperial College London, Prince Consort Road, London, United Kingdom.
    Gunell, Herbert
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik.
    Henri, Pierre
    Lagrange, OCA, UCA, CNRS, Nice, France; LPC2E, CNRS, Orléans, France.
    Heritier, Kevin
    Department of Physics, Imperial College London, Prince Consort Road, London, United Kingdom.
    Jones, Geraint H.
    UCL Mullard Space Science Laboratory, Holmbury St. Mary, Dorking, United Kingdom; The Centre for Planetary Sciences at UCL/Birkbeck, Gower Street, London, United Kingdom.
    Mandt, Kathleen E.
    Johns Hopkins Applied Physics Laboratory, MD, Laurel, United States.
    Nilsson, Hans
    Swedish Institute of Space Physics, Box 812, Kiruna, Sweden.
    Noonan, John W.
    Lunar and Planetary Laboratory, University of Arizona, AZ, Tucson, United States.
    Odelstad, Elias
    Swedish Institute of Space Physics, Box 537, Uppsala, Sweden.
    Parker, Joel W.
    Southwest Research Institute, CO, Boulder, United States.
    Rubin, Martin
    Physikalisches Institut, University of Bern, Sidlerstrasse 5, Bern, Switzerland.
    Simon Wedlund, Cyril
    Space Research Institute, Austrian Academy of Sciences, Schmiedlstr. 6, Graz, Austria.
    Stephenson, Peter
    Department of Physics, Imperial College London, Prince Consort Road, London, United Kingdom.
    Taylor, Matthew G. G. T.
    ESTEC, European Space Agency, Keplerlaan 1, AZ Noordwijk, Netherlands.
    Vigren, Erik
    Swedish Institute of Space Physics, Box 537, Uppsala, Sweden.
    Vines, Sarah K.
    Johns Hopkins Applied Physics Laboratory, MD, Laurel, United States.
    Volwerk, Martin
    Space Research Institute, Austrian Academy of Sciences, Schmiedlstr. 6, Graz, Austria.
    The plasma environment of comet 67P/Churyumov-Gerasimenko2022Ingår i: Space Science Reviews, ISSN 0038-6308, E-ISSN 1572-9672, Vol. 218, nr 8, artikel-id 65Artikel, forskningsöversikt (Refereegranskat)
    Abstract [en]

    The environment of a comet is a fascinating and unique laboratory to study plasma processes and the formation of structures such as shocks and discontinuities from electron scales to ion scales and above. The European Space Agency's Rosetta mission collected data for more than two years, from the rendezvous with comet 67P/Churyumov-Gerasimenko in August 2014 until the final touch-down of the spacecraft end of September 2016. This escort phase spanned a large arc of the comet's orbit around the Sun, including its perihelion and corresponding to heliocentric distances between 3.8 AU and 1.24 AU. The length of the active mission together with this span in heliocentric and cometocentric distances make the Rosetta data set unique and much richer than sets obtained with previous cometary probes. Here, we review the results from the Rosetta mission that pertain to the plasma environment. We detail all known sources and losses of the plasma and typical processes within it. The findings from in-situ plasma measurements are complemented by remote observations of emissions from the plasma. Overviews of the methods and instruments used in the study are given as well as a short review of the Rosetta mission. The long duration of the Rosetta mission provides the opportunity to better understand how the importance of these processes changes depending on parameters like the outgassing rate and the solar wind conditions. We discuss how the shape and existence of large scale structures depend on these parameters and how the plasma within different regions of the plasma environment can be characterised. We end with a non-exhaustive list of still open questions, as well as suggestions on how to answer them in the future.

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  • 11.
    Goetz, Charlotte
    et al.
    European Space Research and Technology Centre, European Space Agency, Keplerlaan 1, Noordwijk, Netherlands; Institut für Geophysik und Extraterrestrische Physik, Technische Universität Braunschweig, Braunschweig, Germany.
    Gunell, Herbert
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik. Royal Belgian Institute for Space Aeronomy (BIRA-IASB), Brussels, Belgium.
    Johansson, Fredrik
    Institutet för Rymdfysik, Uppsala, Sweden.
    Llera, Kristie
    Southwest Research Institute, TX, San Antonio, United States.
    Nilsson, Hans
    Institutet för Rymdfysik, Kiruna, Sweden.
    Glassmeier, Karl-Heinz
    Institut für Geophysik und Extraterrestrische Physik, Technische Universität Braunschweig, Braunschweig, Germany.
    Taylor, Matthew G.G.T.
    European Space Research and Technology Centre, European Space Agency, Noordwijk, Netherlands.
    Warm protons at comet 67P/Churyumov-Gerasimenko-implications for the infant bow shock2021Ingår i: Annales Geophysicae, ISSN 0992-7689, E-ISSN 1432-0576, Vol. 39, nr 3, s. 379-396Artikel i tidskrift (Refereegranskat)
    Abstract [en]

    The plasma around comet 67P/Churyumov-Gerasimenko showed remarkable variability throughout the entire Rosetta mission. Plasma boundaries such as the diamagnetic cavity, solar wind ion cavity and infant bow shock separate regions with distinct plasma parameters from each other. Here, we focus on a particular feature in the plasma: warm, slow solar wind protons. We investigate this particular proton population further by focusing on the proton behaviour and surveying all of the Rosetta comet phase data. We find over 300 events where Rosetta transited from a region with fast, cold protons into a region with warm, slow protons. We investigate the properties of the plasma and magnetic field at this boundary and the location where it can be found. We find that the protons are preferentially detected at intermediate gas production rates with a slight trend towards larger cometocentric distances for higher gas production rates. The events can mostly be found in the positive convective electric field hemisphere. These results agree well with simulations of the infant bow shock (IBS), an asymmetric structure in the plasma environment previously detected on only 2 d during the comet phase. The properties of the plasma on both sides of this structure are harder to constrain, but there is a trend towards higher electron flux, lower magnetic field, higher magnetic field power spectral density and higher density in the region that contains the warm protons. This is in partial agreement with the previous IBS definitions; however, it also indicates that the plasma and this structure are highly non-stationary. For future research, Comet Interceptor, with its multi-point measurements, can help to disentangle the spatial and temporal effects and give more clarity on the influence of changing upstream conditions on the movement of boundaries in this unusual environment.

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  • 12.
    Goncharov, Oleksandr
    et al.
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik.
    Gunell, Herbert
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik. Royal Belgian Institute of Space Aeronomy, Brussels, Belgium.
    Hamrin, Maria
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik.
    Chong, G. S.
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik.
    Evolution of High-Speed Jets and Plasmoids Downstream of the Quasi-Perpendicular Bow Shock2020Ingår i: Journal of Geophysical Research - Space Physics, ISSN 2169-9380, E-ISSN 2169-9402, Vol. 125, nr 6, artikel-id e2019JA027667Artikel i tidskrift (Refereegranskat)
    Abstract [en]

    Plasma structures with enhanced dynamic pressure, density, or speed are often observed in Earth's magnetosheath. We present a statistical study of these structures, known as jets and fast plasmoids, in the magnetosheath, downstream of both the quasi-perpendicular and quasi-parallel bow shocks. Using measurements from the four Magnetospheric Multiscale (MMS) spacecraft and OMNI solar wind data from 2015-2017, we present observations of jets during different upstream conditions and in the wide range of distances from the bow shock. Jets observed downstream of the quasi-parallel bow shock are seen to propagate deeper and faster into the magnetosheath and on toward the magnetopause. We estimate the shape of the structures by treating the leading edge as a shock surface, and the result is that the jets are elongated in the direction of propagation but also that they expand more quickly in the perpendicular direction as they propagate through the magnetosheath.

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  • 13. Gronoff, Guillaume
    et al.
    Maggiolo, Romain
    Cessateur, Gaël
    Moore, W. B.
    Airapetian, Vladimir
    De Keyser, Johan
    Dhooghe, Frederick
    Gibbons, Andrew
    Gunell, Herbert
    Royal Belgian Institute for Space Aeronomy(BIRA-IASB), Brussels, Belgium.
    Mertens, C. J.
    Rubin, Martin
    Hosseini, S.
    The Effect of Cosmic Rays on Cometary Nuclei. I. Dose Deposition2020Ingår i: Astrophysical Journal, ISSN 0004-637X, E-ISSN 1538-4357, Vol. 890, nr 1, artikel-id 89Artikel i tidskrift (Refereegranskat)
    Abstract [en]

    Comets are small bodies thought to contain the most pristine material in the solar system. However, since their formation ≈4.5 Gy ago, they have been altered by different processes. While not exposed to much electromagnetic radiation, they experience intense particle radiation. Galactic cosmic rays and solar energetic particles have a broad spectrum of energies and interact with the cometary surface and subsurface; they are the main source of space weathering for a comet in the Kuiper Belt or in the Oort Cloud, and also affect the ice prior to the comet agglomeration. While low-energy particles interact only with the cometary surface, the most energetic ones deposit a significant amount of energy down to tens of meters. This interaction can modify the isotopic ratios in cometary ices and create secondary compounds through radiolysis, such as O2 and H2O2 (Paper II). In this paper, we model the energy deposition of energetic particles as a function of depth using a Geant4 application modified to account for the isotope creation process. We quantify the energy deposited in cometary nucleus by galactic cosmic rays and solar energetic particles. The consequences of the energy deposition on the isotopic and chemical composition of cometary ices and their implication on the interpretation of cometary observations, notably of 67P/Churyumov Gerasimenko by the ESA Rosetta spacecraft, will be discussed in Paper II.

  • 14.
    Gunell, Herbert
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik. Royal Belgian Institute for Space Aeronomy, Brussels, Belgium.
    The equations of the magnetosphere2021Ingår i: Magnetospheres in the solar system: space physics and aeronomy collection, Volume 2 / [ed] Romain Maggiolo; Nicolas André; Hiroshi Hasegawa; Daniel T. Welling, John Wiley & Sons, 2021, 1, s. 37-45Kapitel i bok, del av antologi (Refereegranskat)
    Abstract [en]

    The use of equations and mathematical modelling in magnetospheric and space physics is reviewed. First, the basic equations are discussed. Then, kinetic and fluid theory are treated. The role of approximations and the applicability of the theories in practice are emphasized.

  • 15.
    Gunell, Herbert
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik.
    Waves and boundaries in plasmas at comets and planets - Experimental aspects2021Ingår i: 2021 International Conference on Electromagnetics in Advanced Applications (ICEAA), IEEE, 2021, s. 46-46Konferensbidrag (Refereegranskat)
    Abstract [en]

    In planetary habitability, a crucial question is whether a planet can maintain liquid water on its surface and a stable atmosphere over timescales of the order of the lifetime of a solar system. This applies both to the planets in our solar systems and to exoplanets discovered in other solar systems. Interaction between a stellar wind and a planetary atmosphere can lead to atmospheric escape. The processes behind atmospheric escape depend on stellar wind and atmospheric conditions as well as planetary magnetization. However, an intrinsic magnetic field is not necessary to protect a planet from atmospheric escape, since protective boundaries are formed also at unmagnetized planets and the magnetic field itself enables escape through the polar caps and cusps [1]. Only the planets in our solar system are accessible to in situ measurements and only under present-day contitions. To assess the evolution of planets and exoplanets we must understand the physics of planetary-stellar wind interaction, and here laboratory experiments have a role to play. Two aspects will be examined here: plasma boundaries in the planetary environment, which shield the atmospheres from the stellar wind, and the aurora, which with its optical and radio emissions enable remote sensing of the planetary environment.

  • 16.
    Gunell, Herbert
    et al.
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik. Royal Belgian Institute for Space Aeronomy (BIRA-IASB), Avenue Circulaire 3, B-1180 Brussels, Belgium.
    Goetz, C.
    Eriksson, A.
    Nilsson, H.
    Wedlund, C. Simon
    Henri, P.
    Maggiolo, R.
    Hamrin, Maria
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik.
    De Keyser, J.
    Rubin, M.
    Wieser, G. Stenberg
    Cessateur, G.
    Dhooghe, F.
    Gibbons, A.
    Plasma waves confined to the diamagnetic cavity of comet 67P/Churyumov-Gerasimenko2017Ingår i: Monthly notices of the Royal Astronomical Society, ISSN 0035-8711, E-ISSN 1365-2966, Vol. 469, s. S84-S92Artikel i tidskrift (Refereegranskat)
    Abstract [en]

    Ion acoustic waves were observed in the diamagnetic cavity of comet 67P/Churyumov-Gerasimenko by the Rosetta spacecraft on 2015 August 3, when the comet was 1.25 au from the Sun. Wave spectra recorded by the Langmuir probe (RPC-LAP), peak near 200 Hz, decrease for higher frequencies and reach the noise floor at approximately 1.5 kHz. These waves were observed only when the spacecraft was in the diamagnetic cavity or at its boundary, which is identified as a sharp drop in magnetic field magnitude, measured by RPC-MAG. The plasma, on both sides of the boundary, is dominated by a cold (a few hundred K) water group ion population, one cold (k(B)T(e) similar to 0.1 eV) and one warm (k(B)T(e) similar to 10 eV) electron population. The observations are interpreted in terms of current-driven ion acoustic waves, generated by currents that flow through bulges on the boundary of the diamagnetic cavity.

  • 17.
    Gunell, Herbert
    et al.
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik.
    Goetz, Charlotte
    Department of Mathematics, Physics and Electrical Engineering, Northumbria University, Newcastle upon Tyne, United Kingdom; Space Research and Technology Centre, European Space Agency, Noordwijk, Netherlands.
    Particle-in-cell modelling of comet 67P/Churyumov-Gerasimenko: spatial structures of densities and electric fields2023Ingår i: Astronomy and Astrophysics, ISSN 0004-6361, E-ISSN 1432-0746, Vol. 674, artikel-id A65Artikel i tidskrift (Refereegranskat)
    Abstract [en]

    Context: Sufficiently far from the Sun, all comets go through a phase of low activity. Rosetta observations at large heliocentric distances of approximately 3 au showed that the plasma at a low-activity comet is affected by both steady state electric fields and low-frequency waves.

    Aims: Our goal is to provide a model for the electric fields in the inner coma at a low-activity comet and to simulate waves and field structures farther away from the nucleus.

    Methods: We compare analytical models for the convective, ambipolar, and polarisation electric fields to the results of an electrostatic particle-in-cell simulation of a scaled-down low-activity comet.

    Results: We find good agreement between the steady state field model and the simulation results close to the nucleus. At larger cometocentric distances, waves dominate the electric field. These waves are interpreted as the scaled-down electrostatic limit of the previously observed singing comet waves. The comet ion density is not spherically symmetric.

    Conclusions: Low-activity comets can be modelled using electrostatic particle-in-cell simulations of a scaled-down system. Outside the innermost part of the coma (r ≥ 40 km), the plasma is not spherically symmetric and the electric field is dominated by waves.

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  • 18.
    Gunell, Herbert
    et al.
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik.
    Goetz, Charlotte
    Department of Mathematics, Physics and Electrical Engineering, Northumbria University, Newcastle-upon-Tyne, United Kingdom.
    Fatemi, Shahab
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik.
    Impact of radial interplanetary magnetic fields on the inner coma of comet 67P/Churyumov-Gerasimenko: Hybrid simulations of the plasma environment2024Ingår i: Astronomy and Astrophysics, ISSN 0004-6361, E-ISSN 1432-0746, Vol. 682, artikel-id A62Artikel i tidskrift (Refereegranskat)
    Abstract [en]

    Context. The direction of the interplanetary magnetic field determines the nature of the interaction between a Solar System object and the solar wind. For comets, it affects the formation of both a bow shock and other plasma boundaries, as well as mass-loading. Around the nucleus of a comet, there is a diamagnetic cavity, where the magnetic field is negligible. Observations by the Rosetta spacecraft have shown that, most of the time, the diamagnetic cavity is located within a solar-wind ion cavity, which is devoid of solar wind ions. However, solar wind ions have been observed inside the diamagnetic cavity on several occasions. Understanding what determines whether or not the solar wind can reach the diamagnetic cavity also advances our understanding of cometsolar wind interaction in general.

    Aims. We aim to determine the influence of an interplanetary magnetic field directed radially out from the Sun that is, parallel to the solar wind velocity on the cometsolar wind interaction. In particular, we explore the possibility of solar wind protons entering the diamagnetic cavity under radial field conditions.

    Methods. We performed global hybrid simulations of comet 67P/Churyumov-Gerasimenko using the simulation code Amitis for two different interplanetary magnetic field configurations and compared the results to observations made by the Rosetta spacecraft.

    Results. We find that, when the magnetic field is parallel to the solar wind velocity, no bow shock forms and the solar wind ions are able to enter the diamagnetic cavity. A solar wind ion wake still forms further downstream in this case.

    Conclusions. The solar wind can enter the diamagnetic cavity if the interplanetary magnetic field is directed radially from the Sun, and this is in agreement with observations made by instruments on board the Rosetta spacecraft.

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  • 19.
    Gunell, Herbert
    et al.
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik.
    Goetz, Charlotte
    Space Research and Technology Centre, European Space Agency, Keplerlaan 1, Noordwijk, Netherlands.
    Odelstad, Elias
    Department of Space and Plasma Physics, Royal Institute of Technology, Stockholm, Sweden.
    Beth, Arnaud
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik.
    Hamrin, Maria
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik.
    Henri, Pierre
    LPC2E, CNRS, Orleáns, France; Lagrange, OCA, CNRS, UCA, Nice, France.
    Johansson, Fredrik L.
    Swedish Institute of Space Physics, Box 537, Uppsala, Sweden.
    Nilsson, Hans
    Swedish Institute of Space Physics, Box 812, Kiruna, Sweden.
    Wieser, Gabriella Stenberg
    Swedish Institute of Space Physics, Box 812, Kiruna, Sweden.
    Ion acoustic waves near a comet nucleus: Rosetta observations at comet 67P/Churyumov-Gerasimenko2021Ingår i: Annales Geophysicae, ISSN 0992-7689, E-ISSN 1432-0576, Vol. 39, nr 1, s. 53-68Artikel i tidskrift (Refereegranskat)
    Abstract [en]

    Ion acoustic waves were observed between 15 and 30 km from the centre of comet 67P/Churyumov–Gerasimenko by the Rosetta spacecraft during its close flyby on 28 March 2015. There are two electron populations: one cold at kBTe≈0.2 eV and one warm at kBTe≈2 eV. The ions are dominated by a cold (a few hundredths of electronvolt) distribution of water group ions with a bulk speed of (3–3.7) km s−1. A warm kBTe≈6 eV ion population, which also is present, has no influence on the ion acoustic waves due to its low density of only 0.25 % of the plasma density. Near closest approach the propagation direction was within 50∘ from the direction of the bulk velocity. The waves, which in the plasma frame appear below the ion plasma frequency fpi≈2 kHz, are Doppler-shifted to the spacecraft frame where they cover a frequency range up to approximately 4 kHz. The waves are detected in a region of space where the magnetic field is piled up and draped around the inner part of the ionised coma. Estimates of the current associated with the magnetic field gradient as observed by Rosetta are used as input to calculations of dispersion relations for current-driven ion acoustic waves, using kinetic theory. Agreement between theory and observations is obtained for electron and ion distributions with the properties described above. The wave power decreases over cometocentric distances from 24 to 30 km. The main difference between the plasma at closest approach and in the region where the waves are decaying is the absence of a significant current in the latter. Wave observations and theory combined supplement the particle measurements that are difficult at low energies and complicated by spacecraft charging.

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  • 20.
    Gunell, Herbert
    et al.
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik. Royal Belgian Institute for Space Aeronomy (BIRA-IASB), Avenue Circulaire 3, 1180 Brussels, Belgium.
    Goetz, Charlotte
    Wedlund, Cyril Simon
    Lindkvist, Jesper
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik.
    Hamrin, Maria
    Nilsson, Hans
    LLera, Kristie
    Eriksson, Anders
    Holmström, Mats
    The infant bow shock: a new frontier at a weak activity comet2018Ingår i: Astronomy and Astrophysics, ISSN 0004-6361, E-ISSN 1432-0746, Vol. 619, artikel-id L2Artikel i tidskrift (Refereegranskat)
    Abstract [en]

    The bow shock is the first boundary the solar wind encounters as it approaches planets or comets. The Rosetta spacecraft was able to observe the formation of a bow shock by following comet 67P/Churyumov-Gerasimenko toward the Sun, through perihelion, and back outward again. The spacecraft crossed the newly formed bow shock several times during two periods a few months before and after perihelion; it observed an increase in magnetic field magnitude and oscillation amplitude, electron and proton heating at the shock, and the diminution of the solar wind further downstream. Rosetta observed a cometary bow shock in its infancy, a stage in its development not previously accessible to in situ measurements at comets and planets.

  • 21.
    Gunell, Herbert
    et al.
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik.
    Hamrin, Maria
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik.
    Nesbit-Östman, Sara
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik.
    Krämer, Eva
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik.
    Nilsson, Hans
    Swedish Institute of Space Physics, Kiruna, Sweden.
    Magnetosheath jets at Mars2023Ingår i: Science Advances, E-ISSN 2375-2548, Vol. 9, nr 22, artikel-id eadg5703Artikel i tidskrift (Refereegranskat)
    Abstract [en]

    Plasma entities, known as magnetosheath jets, with higher dynamic pressure than the surrounding plasma, are often seen at Earth. They generate waves and contribute to energy transfer in the magnetosheath. Affecting the magnetopause, they cause surface waves and transfer energy into the magnetosphere, causing throat auroras and magnetic signatures detectable on the ground. We show that jets exist also beyond Earth's environment in the magnetosheath of Mars, using data obtained by the MAVEN spacecraft. Thus, jets can be created also at Mars, which differs from Earth by its smaller bow shock, and they are associated with an increased level of magnetic field fluctuations. Jets couple large and small scales in magnetosheaths in the solar system and can play a similar part in astrophysical plasmas.

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  • 22.
    Gunell, Herbert
    et al.
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik. Royal Belgian Institute for Space Aeronomy (BIRA-IASB), Avenue Circulaire 3, 1180 Brussels, Belgium .
    Lindkvist, Jesper
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik.
    Goetz, Charlotte
    Institut für Geophysik und extraterrestrische Physik, TU Braunschweig, Mendelssohnstr. 3, 38106 Braunschweig, Germany.
    Nilsson, Hans
    Swedish Institute of Space Physics, Box 812, 981 28 Kiruna, Sweden .
    Hamrin, Maria
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik.
    Polarisation of a small-scale cometary plasma environment: Particle-in-cell modelling of comet 67P/Churyumov-Gerasimenko2019Ingår i: Astronomy and Astrophysics, ISSN 0004-6361, E-ISSN 1432-0746, Vol. 631, artikel-id A174Artikel i tidskrift (Refereegranskat)
    Abstract [en]

    Context: The plasma near the nucleus of a comet is subjected to an electric field to which a few different sources contribute: the convective electric field of the solar wind, the ambipolar electric field due to higher electron than ion speeds, and a polarisation field arising from the vastly different ion and electron trajectories.

    Aims: Our aim is to show how the ambipolar and polarisation electric fields arise and develop under the influence of space charge effects, and in doing so we paint a qualitative picture of the electric fields in the inner coma of a comet.

    Methods. We use an electrostatic particle-in-cell model to simulate a scaled-down comet, representing comet 67P/Churyumov-Gerasimenko with parameters corresponding to a 3.0 AU heliocentric distance.

    Results: We find that an ambipolar electric field develops early in the simulation and that this is soon followed by the emergence of a polarisation electric field, manifesting itself as an anti-sunward component prevalent in the region surrounding the centre of the comet. As plasma is removed from the inner coma in the direction of the convectional electric field of the solar wind, a density maximum develops on the opposite side of the centre of the comet.

    Conclusions: The ambipolar and polarisation electric fields both have a significant influence on the motion of cometary ions. This demonstrates the importance of space charge effects in comet plasma physics.

  • 23.
    Gunell, Herbert
    et al.
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik.
    Schaeffer, Derek
    University of California-Los Angeles, United States.
    Goetz, Charlotte
    Northumbria University, United Kingdom.
    Cruz, Filipe
    Universidade de Lisboa, Portugal.
    Wedlund, Cyril Simon
    Austrian Academy of Sciences, Space Research Institute, Graz, Austria.
    Nilsson, Hans
    Swedish Institute of Space Physics, Kiruna, Sweden.
    Moeslinger, Anja
    Swedish Institute of Space Physics, Kiruna, Sweden.
    Wieser, Gabriella Stenberg
    Swedish Institute of Space Physics, Kiruna, Sweden.
    Edberg, Niklas
    Swedish Institute of Space Physics, Uppsala, Sweden.
    Plasma physics at comets: what can we learn from laboratory experiments?2024Ingår i: 2024 International Conference on Electromagnetics in Advanced Applications (ICEAA), IEEE, 2024, nr 2024, s. 163-163Konferensbidrag (Refereegranskat)
    Abstract [en]

    Diamagnetic cavities at comets were predicted already in the 1960s [1], and then observed at comet lP/Halley by the ESA/Giotto spacecraft in 1986 [2]. Recently, the ESA/Rosetta spacecraft spent two years orbiting comet 67P/Churyumov-Gerasimenko and encountered the diamagnetic cavity of comet 67P more than 700 times [3, 4]. Most encounters lasted a few minutes, with the duration varying from a few seconds up to more than 30 minutes. As the spacecraft moved very slowly (~lms-1), it can be considered stationary with respect to the plasma. Therefore, the quick succession of detections indicates that the boundary of the diamagnetic cavity moved over the spacecraft. Figure 1 (left) shows three diamagnetic cavity signatures observed with the plasma instruments on Rosetta on 16 September 2015 when the comet was close to perihelion. Rosetta was in the diamagnetic cavity during the periods of nearly zero magnetic field (marked by the coloured regions). Outside the cavity, the plasma was often characterised by a series of asymmetric, steepened waves which are visible in the magnetic field, as well as in the plasma density [5]. Since all observations to date have been made using a single spacecraft, the shape of the diamagnetic cavity boundary cannot be well constrained by measurements. However, it has been suggested, based on wave observations, that bulges on the cavity boundary move past the spacecraft, causing the latter to quickly move in and out of the cavity [6].

  • 24. Hajra, Rajkumar
    et al.
    Henri, Pierre
    Vallières, Xavier
    More, Jeromé
    Gilet, Nicolas
    Wattieaux, Gaetan
    Goetz, Charlotte
    Richter, Ingo
    Tsurutani, Bruce T.
    Gunell, Herbert
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik. Royal Belgian Institute for Space Aeronomy (BIRA-IASB), Avenue Circulaire 3, B-1180 Brussels, Belgium.
    Nilsson, Hans
    Eriksson, Anders I.
    Nemeth, Zoltan
    Burchdegrees, James L.
    Rubin, Martin
    Dynamic unmagnetized plasma in the diamagnetic cavity around comet 67P/Churyumov-Gerasimenko2018Ingår i: Monthly notices of the Royal Astronomical Society, ISSN 0035-8711, E-ISSN 1365-2966, Vol. 475, nr 3, s. 4140-4147Artikel i tidskrift (Refereegranskat)
    Abstract [en]

    The Rosetta orbiter witnessed several hundred diamagnetic cavity crossings (unmagnetized regions) around comet 67P/Churyumov-Gerasimenko during its two year survey of the comet. The characteristics of the plasma environment inside these diamagnetic regions are studied using in situ measurements by the Rosetta Plasma Consortium instruments. Although the unmagnetized plasma density has been observed to exhibit little dynamics compared to the very dynamical magnetized cometary plasma, we detected several localized dynamic plasma structures inside those diamagnetic regions. These plasma structures are not related to the direct ionization of local cometary neutrals. The structures are found to be steepened, asymmetric plasma enhancements with typical rising-to-descending slope ratio of similar to 2.8 (+/- 1.9), skewness similar to 0.43 (+/- 0.36), mean duration of similar to 2.7 (+/- 0.9) min and relative density variation Delta N/N of similar to 0.5 (+/- 0.2), observed close to the electron exobase. Similar steepened plasma density enhancements were detected at the magnetized boundaries of the diamagnetic cavity as well as outside the diamagnetic region. The plausible scalelength and propagation direction of the structures are estimated from simple plasma dynamics considerations. It is suggested that they are large-scale unmagnetized plasma enhancements, transmitted from the very dynamical outer magnetized region to the inner magnetic field-free cavity region.

  • 25.
    Hamrin, Maria
    et al.
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik.
    Gunell, Herbert
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik. Belgian Institute for Space Aeronomy, Brussels,Belgium.
    Goncharov, Oleksandr
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik.
    De Spiegeleer, Alexandre
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik.
    Fuselier, S.
    Mukherjee, J.
    Vaivads, A.
    Pitkänen, Timo
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik. Institute of Space Sciences,Shandong University, Weihai, China.
    Torbert, R. B.
    Giles, B.
    Can Reconnection be Triggered as a Solar Wind Directional Discontinuity Crosses the Bow Shock?: A Case of Asymmetric Reconnection2019Ingår i: Journal of Geophysical Research - Space Physics, ISSN 2169-9380, E-ISSN 2169-9402, Vol. 124, nr 11, s. 8507-8523Artikel i tidskrift (Refereegranskat)
    Abstract [en]

    Here we present some unique observations of reconnection at a quasi-perpendicular bow shock as an interplanetary directional discontinuity (DD) is crossing it simultaneously with the Magnetospheric Multiscale (MMS) mission. There are no burst data, but available data show indications of ongoing reconnection at the shock southward of MMS: a bifurcated current sheet with signatures of Hall magnetic and electric fields, normal magnetic fields indicating a magnetic connection between the two reconnecting regions, field-aligned currents and electric fields, E . J > 0 indicating a conversion of magnetic to kinetic energy, and subspin resolution ion energy-time spectrograms indicating ions being accelerated away from the X-line. The DD is also observed by four upstream spacecraft (ACE, WIND, Geotail, and ARTEMIS P1) and one downstream in the magnetosheath (Cluster 4), but none of them resolve signatures of ongoing reconnection. We therefore suggest that reconnection was temporarily triggered as the DD was compressed by the shock. Reconnection at the bow shock is inevitably asymmetric with both the density and magnetic field strength being higher on one side of the X-line (magnetosheath side) than on the other side where the plasma flow also is supersonic (solar wind side). This is different from the asymmetry exhibited at the more commonly studied case of asymmetric reconnection at the magnetopause. Asymmetric reconnection of the bow shock type has never been studied before, and the data discussed here present some first indications of the properties of the reconnection region for this type of reconnection.

  • 26.
    Hamrin, Maria
    et al.
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik.
    Gunell, Herbert
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik. Belgian Institute for Space Aeronomy, Brussels, Belgium.
    Lindkvist, Jesper
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik.
    Lindqvist, Per-Arne
    Royal Institute of Technology, Stockholm, Sweden.
    Ergun, Robert E.
    Laboratory of Atmospheric and Space Physics, Boulder, CO, USA.
    Giles, Barbara L.
    NASA Goddard Space Flight Center, Greenbelt, MD, USA.
    Bow shock generator current systems: MMS observations of possible current closure2018Ingår i: Journal of Geophysical Research - Space Physics, ISSN 2169-9380, E-ISSN 2169-9402, Vol. 123, s. 242-258Artikel i tidskrift (Refereegranskat)
    Abstract [en]

    We use data from the first two dayside seasons of the Magnetospheric Multiscale (MMS) mission to study current systems associated with quasi‐perpendicular bow shocks of generator type. We have analyzed 154 MMS bow shock crossings near the equatorial plane. We compute the current density during the crossings and conclude that the component perpendicular to the shock normal (J⊥) is consistent with a pileup of the interplanetary magnetic field (IMF) inside the magnetosheath. For predominantly southward IMF, we observe a component Jn parallel (antiparallel) to the normal for GSM Y> 0 (<0), and oppositely directed for northward IMF. This indicates current closure across the equatorial magnetosheath, and it is observed for IMF clock angles near 0∘ and 180∘. To our knowledge, these are the first observational evidence for bow shock current closure across the magnetosheath. Since we observe no clear signatures of |J⊥| decreasing toward large |Y| we suggest that the main region of current closure is further tailward, outside MMS probing region. For IMF clock angles near 90∘, we find indications of the current system being tilted toward the north‐south direction, obtaining a significant Jz component, and we suggest that the current closes off the equatorial plane at higher latitudes where the spacecraft are not probing. The observations are complicated for several reasons. For example, variations in the solar wind and the magnetospheric currents and loads affect the closure, and Jn is distributed over large regions, making it difficult to resolve inside the magnetosheath proper.

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  • 27.
    Hamrin, Maria
    et al.
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik.
    Schillings, Audrey
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik.
    Opgenoorth, Hermann J.
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik.
    Nesbit-Östman, Sara
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik.
    Krämer, Eva
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik.
    Araújo, Juan Carlos
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för naturvetenskapernas och matematikens didaktik.
    Baddeley, Lisa
    Department of Arctic Geophysics, University Centre in Svalbard, Longyearbyen, Norway.
    Gunell, Herbert
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik.
    Pitkänen, Timo
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik. Institute of Space Sciences, Shandong University, Weihai, China.
    Gjerloev, Jesper
    Johns Hopkins University, Laurel, MD, USA.
    Barnes, R. J.
    Johns Hopkins University, Laurel, MD, USA.
    Space weather disturbances in non-stormy times: occurrence of dB/dt spikes during three solar cycles2023Ingår i: Journal of Geophysical Research - Space Physics, ISSN 2169-9380, E-ISSN 2169-9402, Vol. 128, nr 10, artikel-id e2023JA031804Artikel i tidskrift (Refereegranskat)
    Abstract [en]

    Spatio-temporal variations of ionospheric currents cause rapid magnetic field variations at ground level and Geomagnetically Induced Currents (GICs) that can be harmful for human infrastructure. The risk for large excursions in the magnetic field time derivative, “dB/dt spikes”, is known to be high during geomagnetic storms and substorms. However, less is known about the occurrence of spikes during non-stormy times. We use data from ground-based globally covering magnetometers (SuperMAG database) from the years 1985–2021. We investigate the spike occurrence (|dB/dt| > 100 nT/min) as a function of magnetic local time (MLT), magnetic latitude (Mlat), and the solar cycle phases during non-stormy times (−15 nT ≤ SYM-H < 0). We sort our data into substorm (AL < 200 nT) intervals (“SUB”) and less active intervals between consecutive substorms (“nonSUB”). We find that spikes commonly occur in both SUBs and nonSUBs during non-stormy times (3–23 spikes/day), covering 18–12 MLT and 65°–80° Mlat. This also implies a risk for infrastructure damage during non-stormy times, especially when several spikes occur nearby in space and time, possibly causing infrastructure weathering. We find that spikes are more common in the declining phase of the solar cycle, and that the occurrence of SUB spikes propagates from one midnight to one morning hotspot with ∼10 min in MLT for each minute in universal time (UTC). Finally, we discuss causes for the spikes in terms of spatio-temporal variations of ionospheric currents.

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  • 28.
    Jones, Geraint H.
    et al.
    Mullard Space Science Laboratory, University College London, Holmbury St. Mary, Dorking, United Kingdom; The Centre for Planetary Sciences at UCL/Birkbeck, London, United Kingdom.
    Gunell, Herbert
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik.
    Ji, Hantao
    Department of Astrophysical Sciences, Princeton University, Princeton, United States.
    The comet interceptor mission2024Ingår i: Space Science Reviews, ISSN 0038-6308, E-ISSN 1572-9672, Vol. 220, artikel-id 9Artikel, forskningsöversikt (Refereegranskat)
    Abstract [en]

    Here we describe the novel, multi-point Comet Interceptor mission. It is dedicated to theexploration of a little-processed long-period comet, possibly entering the inner Solar System for the first time, or to encounter an interstellar object originating at another star. Theobjectives of the mission are to address the following questions: What are the surface composition, shape, morphology, and structure of the target object? What is the composition ofthe gas and dust in the coma, its connection to the nucleus, and the nature of its interactionwith the solar wind? The mission was proposed to the European Space Agency in 2018, andformally adopted by the agency in June 2022, for launch in 2029 together with the Arielmission. Comet Interceptor will take advantage of the opportunity presented by ESA’s FClass call for fast, flexible, low-cost missions to which it was proposed. The call requireda launch to a halo orbit around the Sun-Earth L2 point. The mission can take advantage ofthis placement to wait for the discovery of a suitable comet reachable with its minimum ΔV capability of 600 ms−1. Comet Interceptor will be unique in encountering and studying, at anominal closest approach distance of 1000 km, a comet that represents a near-pristine sample of material from the formation of the Solar System. It will also add a capability that noprevious cometary mission has had, which is to deploy two sub-probes – B1, provided by theJapanese space agency, JAXA, and B2 – that will follow different trajectories through thecoma. While the main probe passes at a nominal 1000 km distance, probes B1 and B2 willfollow different chords through the coma at distances of 850 km and 400 km, respectively.The result will be unique, simultaneous, spatially resolved information of the 3-dimensionalproperties of the target comet and its interaction with the space environment. We presentthe mission’s science background leading to these objectives, as well as an overview of thescientific instruments, mission design, and schedule.

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  • 29.
    Krämer, Eva
    et al.
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik.
    Hamrin, Maria
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik.
    Gunell, Herbert
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik.
    Karlsson, T.
    Division of Space and Plasma Physics, School of Electrical Engineering and Computer Science, KTH Royal Institute of Technology, Stockholm, Sweden.
    Steinvall, K.
    Swedish Institute of Space Physics, Uppsala, Sweden.
    Goncharov, O.
    Faculty of Mathematics and Physics, Charles University, Prague, Czech Republic.
    André, Mats
    Swedish Institute of Space Physics, Uppsala, Sweden.
    Waves in Magnetosheath Jets—Classification and the Search for Generation Mechanisms Using MMS Burst Mode Data2023Ingår i: Journal of Geophysical Research - Space Physics, ISSN 2169-9380, E-ISSN 2169-9402, Vol. 128, nr 7, artikel-id e2023JA031621Artikel i tidskrift (Refereegranskat)
    Abstract [en]

    Magnetosheath jets are localized dynamic pressure enhancements in the magnetosheath. We make use of the high time resolution burst mode data of the Magnetospheric Multiscale mission for an analysis of waves in plasmas associated with three magnetosheath jets. We find both electromagnetic and electrostatic waves over the frequency range from 0 to 4 kHz that can be probed by the instruments on board the MMS spacecraft. At high frequencies we find electrostatic solitary waves, electron acoustic waves, and whistler waves. Electron acoustic waves and whistler waves show the typical properties expected from theory assuming approximations of a homogeneous plasma and linearity. In addition, 0.2 Hz waves in the magnetic field, 1 Hz electromagnetic waves, and lower hybrid waves are observed. For these waves the approximation of a homogeneous plasma does not hold anymore and the observed waves show properties from several different basic wave modes. In addition, we investigate how the various types of waves are generated. We show evidence that, the 1 Hz waves are connected to gradients in the density and magnetic field. The whistler waves are generated by a butterfly-shaped pitch-angle distribution and the electron acoustic waves by a cold electron population. The lower hybrid waves are probably generated by currents at the boundary of the jets. As for the other waves we can only speculate about the generation mechanism due to limitations of the instruments. Studying waves in jets will help to address the microphysics in jets which can help to understand the evolution of jets better.

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  • 30.
    Krämer, Eva
    et al.
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik.
    Koller, Florian
    Institute of Physics, University of Graz, Universitätsplatz 5, Graz, Austria; Department of Physics and Astronomy, Queen Mary University of London, Mile End Road, London, United Kingdom.
    Suni, Jonas
    Department of Physics, University of Helsinki, Pietari Kalmin katu 5, University of Helsinki, Finland.
    LaMoury, Adrian T.
    Department of Physics, Imperial College London, South Kensington Campus, London, United Kingdom.
    Pöppelwerth, Adrian
    Institute of Geophysics and Extraterrestrial Physics, Technische Universität Braunschweig, Universitätsplatz 2, Braunschweig, Germany.
    Glebe, Georg
    Institute of Geophysics and Extraterrestrial Physics, Technische Universität Braunschweig, Universitätsplatz 2, Braunschweig, Germany; School of Earth and Atmospheric Sciences, Georgia Institute of Technology, 311 Ferst Drive, GA, Atlanta, United States.
    Mohammed-Amin, Tara
    KTH Royal Institute of Technology, Department of Space and Plasma Physics, School of Electrical Engineering and Computer Science, Teknikringen 31, Stockholm, Sweden.
    Raptis, Savvas
    Johns Hopkins University, Applied Physics Laboratory, 11000 Johns Hopkins Rd, MD, Laurel, United States.
    Vuorinen, Laura
    Department of Physics and Astronomy, Queen Mary University of London, Mile End Road, London, United Kingdom; Department of Physics and Astronomy, University of Turku, Vesilinnantie 5, Turku, Finland.
    Weiss, Stefan
    Institute of Physics, University of Graz, Universitätsplatz 5, Graz, Austria.
    Xirogiannopoulou, Niki
    Faculty of Mathematics and Physics, Charles University, V Holešovičkách 2, Prague, Czech Republic.
    Archer, Martin
    Department of Physics, Imperial College London, South Kensington Campus, London, United Kingdom.
    Blanco-Cano, Xóchitl
    Instituto de Geofísica, Universidad Nacional Autónoma de México, Circuito de la Investigación Científica s/n, México City, Mexico.
    Gunell, Herbert
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik.
    Hietala, Heli
    Department of Physics and Astronomy, Queen Mary University of London, Mile End Road, London, United Kingdom.
    Karlsson, Tomas
    KTH Royal Institute of Technology, Department of Space and Plasma Physics, School of Electrical Engineering and Computer Science, Teknikringen 31, Stockholm, Sweden.
    Plaschke, Ferdinand
    Institute of Geophysics and Extraterrestrial Physics, Technische Universität Braunschweig, Universitätsplatz 2, Braunschweig, Germany.
    Preisser, Luis
    Space Research Institute, Austrian Academy of Sciences, Schmiedlstraße 6, Graz, Austria.
    Roberts, Owen
    Department of Physics, Aberystwyth University, Physical Sciences Building, Aberystwyth, United Kingdom.
    Simon Wedlund, Cyril
    Space Research Institute, Austrian Academy of Sciences, Schmiedlstraße 6, Graz, Austria.
    Temmer, Manuela
    Institute of Physics, University of Graz, Universitätsplatz 5, Graz, Austria.
    Vörös, Zoltán
    Space Research Institute, Austrian Academy of Sciences, Schmiedlstraße 6, Graz, Austria; Institute of Earth Physics and Space Science, HUN-REN, Csatkai E. u. 6-8., Sopron, Hungary.
    Jets downstream of collisionless shocks: recent discoveries and challenges2025Ingår i: Space Science Reviews, ISSN 0038-6308, E-ISSN 1572-9672, Vol. 221, nr 1, artikel-id 4Artikel i tidskrift (Refereegranskat)
    Abstract [en]

    Plasma flows with enhanced dynamic pressure, known as magnetosheath jets, are often found downstream of collisionless shocks. As they propagate through the magnetosheath, they interact with the surrounding plasma, shaping its properties, and potentially becoming geoeffective upon reaching the magnetopause. In recent years (since 2016), new research has produced vital results that have significantly enhanced our understanding on many aspects of jets. In this review, we summarise and discuss these findings. Spacecraft and ground-based observations, as well as global and local simulations, have contributed greatly to our understanding of the causes and effects of magnetosheath jets. First, we discuss recent findings on jet occurrence and formation, including in other planetary environments. New insights into jet properties and evolution are then examined using observations and simulations. Finally, we review the impact of jets upon interaction with the magnetopause and subsequent consequences for the magnetosphere-ionosphere system. We conclude with an outlook and assessment on future challenges. This includes an overview on future space missions that may prove crucial in tackling the outstanding open questions on jets in the terrestrial magnetosheath as well as other planetary and shock environments.

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  • 31.
    Lindkvist, Jesper
    et al.
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik.
    Hamrin, Maria
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik.
    Gunell, Herbert
    Umeå universitet, Teknisk-naturvetenskapliga fakulteten, Institutionen för fysik. Royal Belgian Institute for Space Aeronomy (BIRA-IASB), Brussels, Belgium.
    Nilsson, Hans
    Swedish Institute of Space Physics.
    Simon Wedlund, Cyril
    University of Oslo, Department of Physics, Oslo, Norway.
    Kallio, Esa
    Aalto University, Department of Electronics and Nanoengineering, Espoo, Finland.
    Mann, Ingrid
    University of Tromsø, Department of Physics and Technology, Tromsø, Norway.