A. H. Sulaiman
University of Iowa
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Featured researches published by A. H. Sulaiman.
Physical Review Letters | 2015
A. H. Sulaiman; A. Masters; M. K. Dougherty; D. Burgess; M. Fujimoto; G. B. Hospodarsky
Shock waves exist throughout the Universe and are fundamental to understanding the nature of collisionless plasmas. Reformation is a process, driven by microphysics, which typically occurs at high Mach number supercritical shocks. While ongoing studies have investigated this process extensively both theoretically and via simulations, their observations remain few and far between. In this Letter we present a study of very high Mach number shocks in a parameter space that has been poorly explored and we identify reformation using in situ magnetic field observations from the Cassini spacecraft at 10 AU. This has given us an insight into quasiperpendicular shocks across 2 orders of magnitude in Alfvén Mach number (M_{A}) which could potentially bridge the gap between modest terrestrial shocks and more exotic astrophysical shocks. For the first time, we show evidence for cyclic reformation controlled by specular ion reflection occurring at the predicted time scale of ~0.3τ_{c}, where τ_{c} is the ion gyroperiod. In addition, we experimentally reveal the relationship between reformation and M_{A} and focus on the magnetic structure of such shocks to further show that for the same M_{A}, a reforming shock exhibits stronger magnetic field amplification than a shock that is not reforming.
Journal of Geophysical Research | 2016
A. H. Sulaiman; A. Masters; Michele K. Dougherty
Collisionless shocks vary drastically from terrestrial to astrophysical regimes resulting in radically different characteristics. This poses two complexities. First, separating the influences of these parameters on physical mechanisms such as energy dissipation. Second, correlating observations of shock waves over a wide range of each parameter, enough to span across different regimes. Investigating the latter has been restricted since the majority of studies on shocks at exotic regimes (such as supernova remnants) have been achieved either remotely or via simulations, but rarely by means of in situ observations. Here we present the parameter space of MA bow shock crossings from 2004 to 2014 as observed by the Cassini spacecraft. We find that Saturns bow shock exhibits characteristics akin to both terrestrial and astrophysical regimes (MA of order 100), which is principally controlled by the upstream magnetic field strength. Moreover, we determined the θBn of each crossing to show that Saturns (dayside) bow shock is predominantly quasi-perpendicular by virtue of the Parker spiral at 10 AU. Our results suggest a strong dependence on MA in controlling the onset of physical mechanisms in collisionless shocks, particularly nontime stationarity and variability. We anticipate that our comprehensive assessment will yield deeper insight into high MA collisionless shocks and provide a broader scope for understanding the structures and mechanisms of collisionless shocks.
Geophysical Research Letters | 2016
J. N. Yates; D. J. Southwood; Michele K. Dougherty; A. H. Sulaiman; A. Masters; S. W. H. Cowley; M. G. Kivelson; C. H. K. Chen; G. Provan; D. G. Mitchell; G. B. Hospodarsky; N. Achilleos; A. M. Sorba; A. J. Coates
Quasiperiodic ∼1 h fluctuations have been recently reported by numerous instruments on board the Cassini spacecraft. The interpretation of the sources of these fluctuations has remained elusive to date. Here we provide an explanation for the origin of these fluctuations using magnetometer observations. We find that magnetic field fluctuations at high northern latitudes are Alfvenic, with small amplitudes (∼0.4nT), and are concentrated in wave packets similar to those observed in Kleindienst et al. (2009). The wave packets recur periodically at the northern magnetic oscillation period. We use a magnetospheric box model to provide an interpretation of the wave periods. Our model results suggest that the observed magnetic fluctuations are second harmonic Alfven waves standing between the northern and southern ionospheres in Saturns outer magnetosphere.
Journal of Geophysical Research | 2014
A. H. Sulaiman; A. Masters; Michele K. Dougherty; Xianzhe Jia
The magnetosheath of a planet is the region between the freestream solar wind and the planetary magnetosphere. In this chapter, we investigate the large-scale overall configuration of Saturn’s magnetosheath magnetic field using observations made by the Cassini spacecraft. While ongoing studies of high-latitude Cassini orbits aim to constrain the extent of magnetospheric polar flattening, here we present the magnetic field structure of the magnetosheath which is largely at lower latitudes. We compare and contrast the magnetic field observations with outputs from the BATSRUS MHD model in each of the equatorial and meridional planes and further compare four cases when the IMF orientation was relatively steady while Cassini traversed the magnetosheath with an analytical model describing draping between axisymmetric boundaries.
Geophysical Research Letters | 2017
A. H. Sulaiman; W. S. Kurth; A. M. Persoon; J. D. Menietti; W. M. Farrell; S.-Y. Ye; G. B. Hospodarsky; D. A. Gurnett; L. Z. Hadid
The Cassini spacecrafts first Grand Finale orbit was carried out in April 2017. This set of 22 orbits had an inclination of 63 degrees with a periapsis grazing Saturns ionosphere, thus providing ...
Journal of Geophysical Research | 2014
R. Mistry; M. K. Dougherty; A. Masters; A. H. Sulaiman; E. J. Allen
Surface waves on Saturns magnetopause and oscillations of the magnetopause at a period associated with that of planetary rotation have previously been detected. How the amplitudes of these two key perturbations to the magnetopause position compare, however, is unclear. We construct a one-dimensional magnetopause model that considers both types of boundary dynamics and compare it to six sets of magnetopause crossings observed by the Cassini magnetometer instrument, in order to estimate and compare properties of the two phenomena. We identify their relative amplitudes to be approximately one in all cases, suggesting that magnetopause oscillations notably affect the magnetopause position, even when surface waves are present. Furthermore, using this technique, we estimate the surface wave period for crossings on 14 July 2007 as 47 min and periods for all other sets at values between 2.4 h and 4.9 h. These periods are in agreement with previous studies which employed minimum variance analysis of magnetometer data.
The Astrophysical Journal | 2017
Torbjörn Sundberg; D. Burgess; M. Scholer; A. Masters; A. H. Sulaiman
Astrophysical shocks, such as planetary bow shocks or supernova remnant shocks, are often in the high or very-high Mach number regime, and the structure of such shocks is crucial for understanding particle acceleration and plasma heating, as well inherently interesting. Recent magnetic field observations at Saturns bow shock, for Alfven Mach numbers greater than about 25, have provided evidence for periodic non-stationarity, although the details of the ion- and electron-scale processes remain unclear due to limited plasma data. High-resolution, multi-spacecraft data are available for the terrestrial bow shock, but here the very high Mach number regime is only attained on extremely rare occasions. Here we present magnetic field and particle data from three such quasi-perpendicular shock crossings observed by the four-spacecraft Cluster mission. Although both ion reflection and the shock profile are modulated at the upstream ion gyroperiod timescale, the dominant wave growth in the foot takes place at sub-proton length scales and is consistent with being driven by the ion Weibel instability. The observed large-scale behavior depends strongly on cross-scale coupling between ion and electron processes, with ion reflection never fully suppressed, and this suggests a model of the shock dynamics that is in conflict with previous models of non-stationarity. Thus, the observations offer insight into the conditions prevalent in many inaccessible astrophysical environments, and provide important constraints for acceleration processes at such shocks.
Geophysical Research Letters | 2018
D. Píša; A. H. Sulaiman; Ondrej Santolik; G. B. Hospodarsky; W. S. Kurth; D. A. Gurnett
We present an observation of intense emissions in Saturn’s magnetosheath as detected by the Cassini spacecraft. The emissions are observed in the dawn sector (magnetic local time ∼06:45) of the magnetosheath over a time period of 11 h before the spacecraft crossed the bow shock and entered the unshocked solar wind. They are found to be narrow-banded with a peak frequency of about 0.16 fce, where fce is the local electron gyrofrequency. Using plane wave propagation analysis, we show that the waves are right hand circularly polarized in the spacecraft frame and propagate at small wave normal angles (<10∘) with respect to the ambient magnetic field. Electromagnetic waves with the same properties known as “lion roars” have been reported by numerous missions in the terrestrial magnetosheath. Here we show the first evidence such emission outside the terrestrial environment. Our observations suggest that lion roars are a solar-system-wide phenomenon and capable of existing in a broad range of parameter space. This also includes 1 order of magnitude difference in frequencies. We anticipate our result to provide new insight into such emissions in a new parameter regime characterized by a higher plasma beta (owing to the substantially higher Mach number bow shock) compared to Earth.
Geophysical Research Letters | 2018
A. H. Sulaiman; W. S. Kurth; G. B. Hospodarsky; T. F. Averkamp; S.-Y. Ye; J. D. Menietti; W. M. Farrell; D. A. Gurnett; A. M. Persoon; Michele K. Dougherty; G. J. Hunt
Cassini’s Radio and Plasma Wave Science (RPWS) instrument detected intense auroral hiss emissions during one of its perikrone passes of the Grand Finale orbits. The emissions were detected when Cassini traversed a flux tube connected to Enceladus’ orbit (L-shell = 4) and at a time when both the spacecraft and the icy moon were in similar longitudes. Previous observations of auroral hiss related to Enceladus were made only during close flybys and here we present the first observation of such emissions close to Saturn. Further, ray-tracing analysis shows the source location at a latitude of 63°, in excellent agreement with earlier UVIS observations of Enceladus’ auroral footprint by Pryor et al. (2011, https://doi.org/10.1038/nature09928). The detection has been afforded exclusively by the Grand Finale phase, which enabled sampling of Enceladus’ high-latitude flux tube near Saturn. This result provides new insight into the spatial extent of the electrodynamic interaction between Saturn and Enceladus. Plain Language Summary Cassini’s high-inclination Grand Finale orbits brought the spacecraft closer to Saturn than ever before, with the closest approach between the cloud tops and the inner edge of the D ring. This unprecedented set of orbits introduced a new view of Saturn’s system by enabling direct measurements of high-latitude Enceladus flux tubes close to Saturn. Here we present evidence of communication between Saturn’s ionosphere and Enceladus during the Grand Finale orbits, revealing the vast spatial extent of their coupling via plasma waves.
Journal of Geophysical Research | 2017
A. H. Sulaiman; Xianzhe Jia; N. Achilleos; N. Sergis; D. A. Gurnett; W. S. Kurth
The interaction between the solar wind and a magnetosphere is fundamental to the dynamics of a planetary system. Here, we address fundamental questions on the large-scale magnetosheath flow around Saturn using a 3D magnetohydrodynamic (MHD) simulation. We find Saturns polar-flattened magnetosphere to channel ~20% more flow over the poles than around the flanks at the terminator. Further, we decompose the MHD forces responsible for accelerating the magnetosheath plasma to find the plasma pressure gradient as the dominant driver. This is by virtue of a high-beta magnetosheath, and in turn, the high-MA bow shock. Together with long-term magnetosheath data by the Cassini spacecraft, we present evidence of how nonaxisymmetry substantially alters the conditions further downstream at the magnetopause, crucial for understanding solar wind-magnetosphere interactions such as reconnection and shear flow-driven instabilities. We anticipate our results to provide a more accurate insight into the global conditions upstream of Saturn and the outer planets.