The Relationship Between Solar Wind Dynamic Pressure Pulses and Solar Wind Turbulence

Abstract

Solar wind dynamic pressure pulses (DPPs) are small-scale plasma structures with abrupt and large-amplitude plasma dynamic pressure changes on timescales of seconds to several minutes. Overwhelming majority of DPP events (around 79.13%) reside in large-scale solar wind transients, i.e., coronal mass ejections, stream interaction regions, and complex ejecta. In this study, the intermittency, which is a typical feature of solar wind turbulence, is determined and compared during the time intervals in the undisturbed solar wind and in large-scale solar wind transients with clustered DPP events, respectively, as well as in the undisturbed solar wind without DPPs. The probability distribution functions (PDFs) of the fluctuations of proton density increments normalized to the standard deviation at different time lags in the three types of distinct regions are calculated. The PDFs in the undisturbed solar wind without DPPs are near-Gaussian distributions. However, the PDFs in the solar wind with clustered DPPs are obviously non-Gaussian distributions, and the intermittency is much stronger in the large-scale solar wind transients than that in the undisturbed solar wind. The major components of the DPPs are tangential discontinuities (TDs) and rotational discontinuities (RDs), which are suggested to be formed by compressive magnetohydrodynamic (MHD) turbulence. There are far more TD-type DPPs than RD-type DPPs both in the undisturbed solar wind and large-scale solar wind transients. The results imply that the formation of solar wind DPPs could be associated with solar wind turbulence, and much stronger intermittency may be responsible for the high occurrence rate of DPPs in the large-scale solar wind transients.

1 Introduction

Small-scale plasma structures with abrupt and large-amplitude plasma dynamic pressure changes (increase or decrease) on timescales of seconds to several minutes and small pressure variations in the preceding and succeeding regions, are frequently observed in the solar wind. They are usually named as solar wind dynamic pressure pulses (DPPs) [1–5]. DPPs are associated with many fundamental physical processes, such as plasma instability [1, 6], turbulence [7], magnetic reconnection [8], and interactions between different kinds of solar wind streams [9]. Meanwhile, DPPs are very geoeffective, which could affect the transport of energy and momentum from the solar wind to the magnetosphere-ionosphere coupling system [10], compress the Earth’s magnetosphere and cause various types of disturbances in the magnetosphere and ionosphere [5, 11–14]. It is important to investigate the origin of DPPs and their evolution in interplanetary space to understand the basic plasma physical process and the space weather effects.

In the past two decades, the properties of DPPs have been investigated in depth. The sudden dynamic pressure changes of DPPs, which are accompanied by variations in the magnetic field and proton temperature, result mainly from increase or decrease in density, rather than the bulk speed change [1–3]. For the majority of DPPs, the sum of the thermal pressure and magnetic pressure remains in equilibrium. Barkhatov et al. [15] indicated that the balance of the total pressure across the sharp pressure changes could affect the evolution of small-scale solar wind structures. Nearly constant total pressure across the small-scale structures can be regarded as the evidence of pressure balance [6, 16]. Hence, most DPPs can be considered as pressure balance structures (PBSs). According to the jump conditions, Dalin et al. (2002) [1] and Riazantseva et al. (2005a) [16] indicated that most DPPs can be classified into tangential discontinuities (TDs), or rotational discontinuities (RDs) with anisotropic thermal pressure. Zuo et al. (2015b) [3] performed a statistical survey on the properties of DPPs based on nearly 20 years of observations from the WIND spacecraft, and verified that the main components of DPPs may be shocks and directional discontinuities (DDs) and the occurrence rate of shocks is extremely smaller comparing with that of DDs. Specially, DPPs have the feature of grouping occurrence and may exist in specific solar wind environments. Zuo et al. (2015b) [4] and Xie et al. (2015) [2] both found that the overwhelming majority of DPP events in different solar phases reside in large-scale solar wind transients, i.e., coronal mass ejection-related flows, stream interaction regions (SIRs), as well as complex ejecta. Since interplanetary coronal mass ejections (ICMEs), SIRs and complex ejecta, which usually containing sustaining southward interplanetary magnetic field (IMF), are the main drivers of geomagnetic storms [17–20], Zuo et al. (2015b) [4] proposed that the feature of grouping occurrence may be regarded as an indicator of space weather events. Zuo et al. (2015c) [5] inferred that DPPs in different solar wind flows may have different origins. In-situ observations and numerical simulations of magnetohydrodynamic (MHD) turbulence show that magnetic discontinuities closely relate to the intermittent turbulence [21–27]. Zuo et al. (2015b) [4] also found some clues that DPPs may be the product of magnetic turbulence or repeated magnetic reconnections.

In this paper, we comparatively analyze the different features of intermittency and component of DPP events in the undisturbed solar wind and in the large-scale solar wind transients based on nearly 21 years of WIND observations (1995–2016). The origin of DPPs is also discussed. In Section 2, we briefly introduce the data set and DPP event selection approach. Section 3 presents the results of statistical and comparative investigation of the dynamic pressure change and the relative dynamic pressure change in the undisturbed solar wind and solar wind transients. We then compare the intermittency during the time intervals in the undisturbed solar wind and in large-scale solar wind transients with clustered DPP events, respectively, as well as in the undisturbed solar wind without DPPs in Section 4. In the next section, the classification of DPPs is shown. A brief discussion and summary are given in the last section.

2 Data and Event Selection

In this investigation, we primarily use high time resolution solar wind plasma and magnetic field data from the Three-Dimensional Plasma and Energetic Particle Investigation (3DP) [28] and the Magnetic Field Investigation (MFI) [29] instruments onboard the WIND spacecraft, respectively. The solar wind plasma and magnetic field data during the period from 1995 to 2016, used to the DPP event identification, analysis on DPPs component and associated intermittency, are available with a cadence of 3-s in this work.

To identify DPPs in the solar wind, we apply an automated DPP-hunting computer procedure developed by Zuo et al. (2015a) [3]. The procedure is capable of: 1) correctly identifying the DPPs, 2) functionally determining their transition region where abrupt dynamic pressure changes occur, 3) and simultaneously selecting representative preceding and succeeding regions as the upstream and downstream, for which there are very small variations in solar wind dynamic pressure to represent the quiet plasma status. The selection criteria are guided as follows: 1) The sharp change of dynamic pressure exceeds a given threshold value dp₀ = 1 nPa in less than dt₀ = 5 min. 2) The transition region should be isolated in the sense that only small variations in dynamic pressure occur in the preceding and succeeding 3 min. The preceding and succeeding 3-min regions are selected to be representative of the upstream and downstream region. 3) In the upstream and downstream regions, the change in the amplitude of the dynamic pressure is less than 60% of that in the transition region, and the ratio of the square deviation of the dynamic pressure to its corresponding average value is less than 0.6. In order to ensure that the detected DPPs do not occur in the magnetosphere and its foreshock region, the events are discarded if the spacecraft was located in the region with X_WIND < 60R_E and (X_WIND, Y_WIND, and Z_WIND are coordinates of WIND location in GSM. R_E is the radius of the Earth).

An example of DPP event in the solar wind on January 2, 2016 is presented in Figure 1. The region between two red vertical lines is defined as the transition region and the code-given adjacent upstream and downstream regions are marked by the red transverse lines. The top four panels present the magnetic field magnitude, the three magnetic components (in GSM coordinates), latitude angle and azimuthal angle of the magnetic field. As seen in Figure 1, the magnetic field magnitude drops from _~ 7.5 to _~ 1.0 nT, with abrupt directional changes (latitude angle change: Δθ > 50°), suggesting the existence of intermittent structures. The subsequent panels show the proton temperature, proton number density, solar wind bulk speed and solar wind dynamic pressure from the 3DP instruments. The values of the four plasma parameters all increase from upstream to downstream.

FIGURE 1

ICMEs and SIRs are two types of dominant solar wind transients [30–32]. A combined ICME list in 1995–2016 is obtained from publicly available catalogues compiled by Chi Yutian (USTC list)¹, Jian Lan (UCLA list)² and Richardson & Cane (R& C list)³. The lists of SIRs obtained from the websites^4,5 are also referred. We classify the near-Earth solar wind into two types: the undistributed solar wind and the large-scale solar wind transients including ICMEs, CIRs and the complex ejecta formed due to their interaction. A DPP event is considered to be associated with the solar wind transients if its transition region occurs within the time interval of the solar wind transient passages.

3 Statistic of DPP Events

12,077 DPP events in the solar wind from 1995 to 2016 are identified with the automatic searching code. There are 2,521 (20.87%) and 9,556 (79.13%) DPP events residing in the undisturbed solar wind and solar wind transients, respectively. Table 1 shows the annual number of DPPs in undisturbed solar wind and solar wind transients. Figure 2 shows the distribution of DPPs that are associated with the undisturbed solar wind (indian red) and solar wind transients (sky blue) in each year during 1995–2016. It is found that except for 1996 (55.81%), the proportion of DPPs in undisturbed solar wind is much lower than that related to the solar wind transients, ranging from 3.46 to 28.99%, which is consistent with Zuo et al. (2015b) [4].

FIGURE 2

Figure 3 presents the comparison of the dynamic pressure change in the undisturbed solar wind (indian red) and solar wind transients (sky blue). The distribution of the absolute value of the dynamic pressure amplitude change from upstream to downstream, i.e., dP_dy = |p_down − p_up|, is displayed in Figure 3A. The value of for the events in the undisturbed solar wind varies from 1.0 to 14.65 nPa with an average value of 1.63 nPa, and the value of dP_dy in solar wind transients varies from 1.0 to 41.94 nPa with an average value of 2.18 nPa, which is 33.74% larger than that in the undisturbed solar wind. It is found that the distributions of dP_dy about the cases both in the undisturbed solar wind and solar wind transients peak at 1.0–2.0 nPa, and there are about 82.43 and 67.12% of the cases, respectively, in this range. Zuo et al. (2015b) [4] defined that strong DPPs should have dynamic pressure changes over 3 nPa in 5 min. It is noteworthy that there are fewer strong DPPs in the undisturbed solar wind than that in solar wind transients. Only 6.45% of the DPP events are strong DPPs in the undisturbed solar wind, while in solar wind transients this proportion accounts for 15.70%

FIGURE 3

The strength of the DPP compared with the background condition it resides in is determined by the ratio of the absolute value of the dynamic pressure amplitude change to the average dynamic pressure value, i.e., dp_relative = dP_dy/[(p_up + p_down)/2] [2]. Figure 3B shows the distribution of the relative dynamic pressure change. Comparison between the two types of solar wind flows suggests little difference in the distributions. The most probable relative pressure changes are 0.2–0.4 in the undisturbed solar wind and solar wind transients. The value of d_relative for all cases in the undisturbed solar wind varies from 0.20 to 1.97 with an average value of 0.47, and 3.00% of the events have values greater than 1.0. The value of dp_relative for all cases in solar wind transients varies from 0.20 to 1.99 with an average of 0.44, and about 3.40% of the events have values greater than 1.0. However, the most probable relative pressure changes are 0.4–0.6 for strong DPPs (Figure 3C). About 24.54% of the strong DPPs in the undisturbed solar wind and 14.02% of the strong DPPs in solar wind transients have a value of relative change larger than 1.0.

4 Turbulence Associated With DPP Events

Turbulence in the solar wind describes the fluctuation of solar wind parameters over different spatial and temporal scales [33]. Intermittency, manifesting inhomogeneity in the energy transfer between scales [34–37], is a typical feature of turbulence [38]. If the probability distribution function (PDF) of the fluctuations for a given solar wind parameter is not Gaussian at different scales and increasingly departs from a normalized distribution when the time-scale gets smaller, it reveals the presence of intermittency [36].

DPPs mainly reside in the solar wind transients. Here we selected sixteen events containing ICME, CIR or complex ejecta with clustered DPP occurrence, and in front of the solar wind transient, clustered distributed DPPs are also existed. So it is convenient to compare the intermittency during the successive intervals of the undisturbed solar wind without DPPs, the undisturbed solar wind with DPPs, and the solar wind transient with DPPs. For simplicity, these regions are termed as the ndpp-USW region, the dpp-USW region, and the dpp-LSSWT region, respectively. The time information of these events is listed in Table 2. Considering the pressure changes of DPPs are dominated by density variations, we analyzed the intermittency of density fluctuation in this work. The proton density increments are defined by δρ(τ) = ρ(t + τ) − ρ(t), and the function [δρ(τ) − ⟨δρ(τ)⟩] represents the fluctuations of proton density increments. Here, ρ and τ are the proton density, and the time lag between two samples, respectively. The angle bracket denotes ensemble averaging over time.

Figure 4 presents the magnetic field and plasma data observed by WIND during September 14–19, 2000. An ICME, which started at 16:09:00 UT on September 17, 2000 and ended at 06:25:00 UT on September 19, 2000, was observed to interact with a SIR during 18:30:00 UT on September 16 and 23:21:25 UT on September 17, 2000, and formed a complex ejecta. Four remarkably different regions labeled by the red vertical lines can be defined in sequence: the ndpp-USW region, the dpp-USW region, the dpp-LSSWT I region and the dpp-LSSWT II region. The dpp-LSSWT I and dpp-LSSWT II regions are both inside the complex ejecta. The time information of each region is given for the Event with NO. 6 in Table 2. The time scale of ndpp-USW region is same as that of the dpp-USW region and different from that of two dpp-LSSWT regions. The center position of the transition regions of the captured DPP events are marked by sky blue vertical lines. The number of DPP events captured in the dpp-USW, dpp-LSSWT I, dpp-LSSWT II regions is six, eleven and forty-eight, respectively (see also in Table 2).

FIGURE 4

Figure 5 shows the PDFs of solar wind proton density increments normalized to the standard deviation, i.e., [δρ(τ) − ⟨δρ(τ)⟩]/σ_ρ, for different time lags τ of the corresponding ndpp-USW region (Figure 5A), dpp-USW region (Figure 5B), dpp-LSSWT I region (Figure 5C) and dpp-LSSWT II (Figure 5D), respectively. σ_ρ is the standard deviation of δρ(τ). The black curves in Figure 5 denote the standard Gaussian distribution with ⟨δρ(τ)⟩ = 0 and σρ = 1. The different degrees of red lines illustrate the actual distribution function among different time lags (τ = 12, 24, 48, 96, 192, and 384 s). It can be seen that the PDFs in the ndpp-USW region are near-Gaussian with all given time lags ranging from 12 to 384 s. But the PDFs are obviously non-Gaussian and the distributions become more self-similar at larger time lags in the dpp-USW, dpp-LSSWT I, dpp-LSSWT II regions. Deviation from a Gaussian distribution indicates that intermittency exists in the dpp-USW and two dpp-LSSWT regions.

FIGURE 5

In order to unravel the intermittent character of the density fluctuations, the method described in Bruno et al. (2003, 2014) [39, 40] is used to estimate the flatness factor F at different time lags. The flatness factor F, the fourth-order moment of distribution, is defined as: . The larger the flatness factor F is, the longer the tail of the distribution becomes. For a standard Gaussian distribution, the flatness factor F should equal to 3 [7]. The flatness factor F at the time lags ranging from 3 to 3,072 s in the ndpp-USW region, dpp-USW region and two dpp-LSSWT regions, are shown in Figure 6. The flatness factor F approximately equal to 3 in the ndpp-USW region, while the flatness factors in the dpp-USW and two dpp-LSSWT regions are all larger than 3, and the values start to increase at larger time lags and reach higher values at small time lags. It indicates that distributions become more intermittent for small time lags and more Gaussian for larger time lags. This is consistent with the qualitative assessment of distribution shapes discussed in Figure 5. Moreover, the flatness factors in two dpp-LSSWT regions are obviously larger than those in the dpp-USW region. Hence, density fluctuations in two dpp-LSSWT regions can be considered to be more intermittent than those in the dpp-USW region. If the flatness factor remains constant within a certain range of time lags, it indicates that solar wind turbulence is not intermittent but self-similar [7]. Flatness factor in the ndpp-USW region is nearly 3.

FIGURE 6

Figure 7 presents the solar wind data observed by WIND during May 11–17, 2005. A typical ICME preceded by a driven strong shock is detected during May 15–17, 2005. Before the ICME, one ndpp-USW and two dpp-USW regions can be found, which are marked by red vertical lines in the figure. A dpp-LSSWT region is inside the ICME and the sheath region. The time information of each region is given for the Event with NO. 11 in Table 2. The PDFs of solar wind proton density increments normalized to the standard deviation for the four regions are shown in Figure 8. Similarly, as seen in Figure 8A, the PDFs are near-Gaussian distributions in the ndpp-USW region, while the PDFs progressively deviate from a Gaussian distribution in two dpp-USW regions and one dpp-LSSWT region shown in Figures 8B–D. We also calculate corresponding flatness factors F for these four regions. Figure 9 displays the distributions of flatness factor F. It can be found that the flatness factors in the ndpp-USW region are about to 3 and keep self-similar substantially. The F curves for two dpp-USW regions approximately overlap. It indicates that the density fluctuations in the two dpp-USW regions exhibit the same level of intermittency. Besides, the flatness factors in the dpp-LSSWT region are dominantly higher than those in other three regions, which illustrates more intermittent in the dpp-LSSWT region.

FIGURE 7

FIGURE 8

FIGURE 9

In above analysis we have taken two events as examples to compare the intermittency features in the regions with and without DPP occurrence. Both the distributions of PDFs and flatness factor clearly reveal that intermittency does not exist in the ndpp-USW region, but exists in the dpp-USW and dpp-LSSWT regions. Furthermore, the intermittency in dpp-LSSWT regions is stronger than that in the dpp-USW regions. The remaining events, although not discussed here, have the similar distributions of PDFs and flatness factor according to our analysis. Figure 10 illustrates the statistical distributions of the average values of flatness factor F of all dpp-LSSWT regions, dpp-USW regions and ndpp-USW regions for the selected sixteen events. It is found that the average of flatness factor in dpp-USW regions are evidently smaller than that in dpp-LSSWT regions at all discussed time lags.

FIGURE 10

5 Classification of DPP Events

Recent studies about DPPs in the solar wind show that the main components of DPPs are directional discontinuities (DDs) or interplanetary (IP) shocks, but IP shocks are much rare in comparison with DDs so that they do not play a significant role in statistical investigation [4]. DDs are ubiquitous in interplanetary space and are considered to be a mixture of TDs and RDs [21, 41–45]. A TD, which does not propagate but is convected along with the solar wind, is a special kind of pressure-balance structure and usually separate two different plasma regions of solar wind [46]. A RD, which has a magnetic field component normal to the discontinuity surface, is not a static structure and can be regarded as a large-amplitude Alfvén wave propagating along the magnetic field [45, 47, 48]. Due to plasma compression, TDs are less stable than RDs.

Previous studies proposed some criteria to categorize solar wind DDs into TDs and RDs [21, 41, 49–51]. In this study, we follow the criterion of Neugebauer et al. [41] in which only magnetic field data were used for classification. A DD is classified as: 1) TD: |B_n|/B_max < 0.4, [B]/B_max ≥ 0.2; 2) RD: |B_n|/B_max ≥ 0.4, [B]/B_max < 0.2; 3) Either discontinuity (ED): |B_n|/B_max < 0.4, [B]/B_max < 0.2; 4) Neither discontinuity (ND): |B_n|/B_max ≥ 0.4, [B]/B_max ≥ 0.2 [43]. Here |B_n| is the normal field component, [B] is the absolute change value of field magnitude across the transition, B_max is the maximum of the averaged magnetic field magnitude in the selected upstream region and that in the downstream region. EDs with a small field component normal to the discontinuity surface and small absolute magnitude change share the properties of TDs and RDs [41, 43, 52–54]. Thus it is difficult to judge whether an ED is a TD or a RD if only the magnetic field data is used.

To determine the surface normal vector of the DDs, the minimum variance analysis (MVA) [55] was employed. The minimum variance direction of the IMF vectors corresponds to the normal of the discontinuity plane. And the quality of the result has a positive correlation to the ratio of the intermediate (λ₂) to minimum (λ₃) eigenvalue, which gives information about the efficiency of the MVA technique. Here we adopt the consistency requirement to ensure the accurate MVA normal estimates λ₂/λ₃ ≥ 2 [56].

Figure 11 illustrates the percentages of TD, RD, ED, ND for the DPPs in the undisturbed solar wind (Figure 11A) and in the solar wind transients (Figure 11B). In the undisturbed solar wind, 2,121 (84.13%) DPP events match the requirement, and the occurrence of TDs, RDs, EDs, and NDs accounts for 53.47, 9.48, 31.35, and 5.70%. In the solar wind transients, 8,018 (83.91%) DPP events are obtained, and the corresponding proportions of TD, RD, ED, and ND are 36.24, 17.88, 42.68, and 3.20%, respectively. By comparison, the ratio of TD type DPPs in the undisturbed solar wind is distinctly greater than that in the solar wind transients, while the ratio of RD-type DPPs in the solar wind transients is around twice of that in the undisturbed solar wind. Whether DPP events resides in the undisturbed solar wind or in the solar wind transients, TDs are obviously more than RDs.

FIGURE 11

6 Summary and Discussion

DPPs are small-scale plasma structures which are ubiquitous in the solar wind. With the motivation to rapidly and automatically identify the numerous DPPs from the solar wind data for further research, we have developed an automated searching procedure. This code has been applied to hunt for DPPs from the observational data stream of WIND from 1995 to 2016. Totally 12,077 DPP events are identified. Based on these events, we perform a comparative analysis on the turbulence and component classification of DPPs in different types of solar wind. Note that, since we only consider the sharp front with sudden change of dynamic pressure on timescales of seconds to a few minutes, in our code, the crossing time of the transition region dt₀ is restricted to be less than 5 min, which can be easily operated. If we restrict the spatial length of the transition region, the number of samples of DPPs identified and used in the statistical investigation may be changed. But the statistical features of the intermittency of the region with and without clustered DPP occurrence should keep coincident since we don’t consider the DPP itself but the study the turbulence of the environment that the DPPs resided in.

In-situ observations and numerical simulations of MHD turbulence show that magnetic discontinuities may originate from MHD turbulence and closely relate to intermittent turbulence [21–27, 57]. By comparing the statistical analysis with simulations of MHD turbulence about the waiting-time and the PDFs of magnetic field increments, Greco et al. (2009a) [23] found that some discontinuities are reproduced by intermittent turbulence. Zhdankin et al. [57] studied the relationship between exponentially distributed angular discontinuities in the magnetic field and MHD turbulence. They proposed that strong discontinuities are associated with inertial-range MHD turbulence, while weak discontinuities emerge from dissipation-range turbulence. Meanwhile, they found that the structure functions of the magnetic field direction exhibit anomalous scaling exponents, which indicated the existence of intermittent structures. Yang et al. [26] conducted a simulation of decaying compressive MHD turbulence with a RD, and they found that the RD evolves from the steepening, which is caused by the non-uniformity of Alfvén speed in the MHD turbulence, of Alfvén waves. And then, they compared the TD’s lifetime with the travel time of the solar wind from the Sun to 1 AU and inferred that TDs observed at 1 AU are more possibly to be generated by local turbulence [27].

This study shows that the PDFs in the solar wind with clustered DPPs are obviously non-Gaussian distributions and the intermittency is much stronger in the large-scale solar wind transients, while the PDFs in the undisturbed solar wind without DPPs are near-Gaussian distributions. It reveals that strong intermittency is more likely to occur in solar wind transients with clustered DPP events. On the other hand, the main components of the DPPs are two types of discontinuities: TDs and RDs, and the occurrence rate of DPPs is much higher in the solar wind transients than in the undisturbed solar wind. It is inferred that much stronger intermittency may be responsible for the high occurrence rate of DPPs in the large-scale solar wind transients.

References

• 1.

  DalinPAZastenkerGNPaularenaKIRichardsonJD. A Survey of Large, Rapid Solar Wind Dynamic Pressure Changes Observed by Interball-1 and IMP 8.Ann Geophys (2002) 20:293–299. 10.5194/angeo-20-293-2002

  • CrossRef
  • Google Scholar

• 2.

  XieYZuoPFengXZhangY. Solar Wind Dynamic Pressure Pulses at 1 AU during the Deep Minimum between Solar Cycles 23 and 24. Sol Phys (2015) 290:1835–49. 10.1007/s11207-015-0700-5

  • CrossRef
  • Google Scholar

• 3.

  ZuoPFengXXieYWangYLiHXuX. Automatic Detection Algorithm of Dynamic Pressure Pulses in the Solar Wind. ApJ (2015) 803:94. 10.1088/0004-637X/803/2/94

  • CrossRef
  • Google Scholar

• 4.

  ZuoPFengXXieYWangYXuX. A Statistical Survey of Dynamic Pressure Pulses in the Solar Wind Based Onwindobservations. ApJ (2015) 808:83. 10.1088/0004-637X/808/1/83

  • CrossRef
  • Google Scholar

• 5.

  ZuoPFengXXieYWangYXuX. Strong Solar Wind Dynamic Pressure Pulses: Interplanetary Sources and Their Impacts on Geosynchronous Magnetic fields. ApJ (2015) 812:152. 10.1088/0004-637X/812/2/152

  • CrossRef
  • Google Scholar

• 6.

  RiazantsevaMOZastenkerGNRichardsonJDEigesPE. Sharp Boundaries of Small- and Middle-Scale Solar Wind Structures. J Geophys Res (2005) 110:A12110. 10.1029/2005JA011307

  • CrossRef
  • Google Scholar

• 7.

  RiazantsevaMOKhabarovaOVZastenkerGNRichardsonJD. Sharp Boundaries of Solar Wind Plasma Structures and Their Relationship to Solar Wind Turbulence. Adv Space Res (2007) 40:1802–6. 10.1016/j.asr.2007.05.004

  • CrossRef
  • Google Scholar

• 8.

  KhabarovaOVZastenkerGN. Sharp Changes of Solar Wind Ion Flux and Density within and outside Current Sheets. Sol Phys (2011) 270:311–29. 10.1007/s11207-011-9719-4

  • CrossRef
  • Google Scholar

• 9.

  RiazantsevaMODalinPAZastenkerGNRichardsonJD. Orientation of Sharp Fronts of the Solar Wind Plasma. Cosmic Res (2003) 41:382–91. 10.1023/a:1025061711391

  • CrossRef
  • Google Scholar

• 10.

  LyonJG. The Solar Wind-Magnetosphere-Ionosphere System. Science (2000) 288:1987–91. 10.1126/science.288.5473.1987

  • CrossRef
  • Google Scholar

• 11.

  BorovskyJE. Contribution of Strong Discontinuities to the Power Spectrum of the Solar Wind. Phys Rev Lett (2010) 105:111102. 10.1103/physrevlett.105.111102

  • CrossRef
  • Google Scholar

• 12.

  HietalaHPhanTDAngelopoulosVOierosetMArcherMOKarlssonTet alIn Situ Observations of a Magnetosheath High-Speed Jet Triggering Magnetopause Reconnection. Geophys Res Lett (2018) 45:1732–40. 10.1002/2017gl076525

  • CrossRef
  • Google Scholar

• 13.

  PlaschkeFHietalaHArcherMBlanco-CanoXKajdičPKarlssonTet alJets Downstream of Collisionless Shocks. Space Sci Rev (2018) 214:1–77. 10.1007/s11214-018-0516-3

  • CrossRef
  • Google Scholar

• 14.

  NewmanRVainchteinDArtemyevA. Solar Wind Transient Currents: Statistical Properties and Impact on Earth's Magnetosphere. Sol Phys (2020) 295:1–16. 10.1007/s11207-020-01695-z

  • CrossRef
  • Google Scholar

• 15.

  BarkhatovNAKorolevAVZastenkerGNRyazantsevaMODalinPA. MHD Simulations of the Dynamics of Sharp Disturbances of the Interplanetary Medium and Comparison with Spacecraft Observations. Cosmic Res (2003) 41:529–38. 10.1023/B:COSM.0000007951.49454.8a

  • CrossRef
  • Google Scholar

• 16.

  RiazantsevaMOKhabarovaOVZastenkerGNRichardsonJD. Sharp Boundaries of Solar Wind Plasma Structures and an Analysis of Their Pressure Balance. Cosmic Res (2005) 43:157–64. 10.1007/s10604-005-0030-8

  • CrossRef
  • Google Scholar

• 17.

  GonzalezWDJoselynJAKamideYKroehlHWRostokerGTsurutaniBTet alWhat is a Geomagnetic Storm. J Geophys Res (1994) 99:5771–92. 10.1029/93ja02867

  • CrossRef
  • Google Scholar

• 18.

  GonzalezWDTsurutaniBTClúa de GonzalezAL. Interplanetary Origin of Geomagnetic Storms. Space Sci Rev (1999) 88:529–62. 10.1023/a:1005160129098

  • CrossRef
  • Google Scholar

• 19.

  ZhangJRichardsonIGWebbDFGopalswamyNHuttunenEKasperJCet alSolar and Interplanetary Sources of Major Geomagnetic Storms (Dst≤ −100 nT) during 1996-2005. J Geophys Res (2007) 112:a–n. 10.1029/2007JA012321

  • CrossRef
  • Google Scholar

• 20.

  ShenCChiYWangYXuMWangS. Statistical Comparison of the ICME's Geoeffectiveness of Different Types and Different Solar Phases from 1995 to 2014. J Geophys Res Space Phys (2017) 122:5931–48. 10.1002/2016ja023768

  • CrossRef
  • Google Scholar

• 21.

  BurlagaLF. Micro-scale Structures in the Interplanetary Medium. Sol Phys (1968) 4:67–92. 10.1007/BF00146999

  • CrossRef
  • Google Scholar

• 22.

  GrecoAChuychaiPMatthaeusWHServidioSDmitrukP. Intermittent MHD Structures and Classical Discontinuities. Geophys Res Lett (2008) 35. 10.1029/2008GL035454

  • CrossRef
  • Google Scholar

• 23.

  GrecoAMatthaeusWHServidioSChuychaiPDmitrukP. Statistical Analysis of Discontinuities in Solar WIND ACE Data and Comparison with Intermittent Mhd Turbulence. ApJ (2009) 691:L111–L114. 10.1088/0004-637x/691/2/l111

  • CrossRef
  • Google Scholar

• 24.

  GrecoAMatthaeusWHServidioSDmitrukP. Waiting-time Distributions of Magnetic Discontinuities: Clustering or Poisson Process?Phys Rev E (2009) 80:046401. 10.1103/PhysRevE.80.046401

  • CrossRef
  • Google Scholar

• 25.

  ServidioSGrecoAMatthaeusWHOsmanKTDmitrukP. Statistical Association of Discontinuities and Reconnection in Magnetohydrodynamic Turbulence. J Geophys Res (2011) 116:a–n. 10.1029/2011JA016569

  • CrossRef
  • Google Scholar

• 26.

  YangLZhangLHeJTuCWangLMarschEet alThe Formation of Rotational Discontinuities in Compressive Three-Dimensional MHD Turbulence. ApJ (2015) 809:155. 10.1088/0004-637X/809/2/155

  • CrossRef
  • Google Scholar

• 27.

  YangLZhangLHeJTuCLiSWangXet alFormation and Properties of Tangential Discontinuities in Three-Dimensional Compressive MHD Turbulence. ApJ (2017) 851:121. 10.3847/1538-4357/aa9993

  • CrossRef
  • Google Scholar

• 28.

  LinRPAndersonKAAshfordSCarlsonCCurtisDErgunRet alA Three-Dimensional Plasma and Energetic Particle Investigation for the Wind Spacecraft. Space Sci Rev (1995) 71:125–53. 10.1007/BF00751328

  • CrossRef
  • Google Scholar

• 29.

  LeppingRPAcũnaMHBurlagaLFFarrellWMSlavinJASchattenKHet alThe Wind Magnetic Field Investigation. Space Sci Rev (1995) 71:207–29. 10.1007/BF00751330

  • CrossRef
  • Google Scholar

• 30.

  JianLKRussellCTLuhmannJG. Comparing Solar Minimum 23/24 with Historical Solar Wind Records at 1 AU. Sol Phys (2011) 274:321–44. 10.1007/s11207-011-9737-2

  • CrossRef
  • Google Scholar

• 31.

  RichardsonIGCaneHV. Near-earth Solar Wind Flows and Related Geomagnetic Activity during More Than Four Solar Cycles (1963-2011). J Space Weather Space Clim (2012) 2:A02. 10.1051/swsc/2012003

  • CrossRef
  • Google Scholar

• 32.

  ChiYShenCLuoBWangYXuM. Geoeffectiveness of Stream Interaction Regions from 1995 to 2016. Space Weather (2018) 16:1960–71. 10.1029/2018sw001894

  • CrossRef
  • Google Scholar

• 33.

  ColemanPJJ. Turbulence, Viscosity, and Dissipation in the Solar-Wind Plasma. ApJ (1968) 153:371. 10.1086/149674

  • CrossRef
  • Google Scholar

• 34.

  HorburyTSFormanMAOughtonS. Spacecraft Observations of Solar Wind Turbulence: an Overview. Plasma Phys Control Fusion (2005) 47:B703–B717. 10.1088/0741-3335/47/12B/S52

  • CrossRef
  • Google Scholar

• 35.

  Sorriso-ValvoLCarboneVBrunoR. On the Origin of the Strong Intermittent Nature of Interplanetary Magnetic Field. Space Sci Rev (2005) 121:49–53. 10.1007/s11214-006-5559-1

  • CrossRef
  • Google Scholar

• 36.

  BrunoR. Intermittency in Solar Wind Turbulence from Fluid to Kinetic Scales. Earth Space Sci (2019) 6:656–72. 10.1029/2018EA000535

  • CrossRef
  • Google Scholar

• 37.

  VerscharenDKleinKGMarucaBA. The Multi-Scale Nature of the Solar Wind. Living Rev Sol Phys (2019) 16:1–136. 10.1007/s41116-019-0021-0

  • CrossRef
  • Google Scholar

• 38.

  MarschETuC. Non-gaussian Probability Distributions of Solar Wind Fluctuations. Ann Geophys (1994) 12:1127–38. 10.1007/s00585-994-1127-8

  • CrossRef
  • Google Scholar

• 39.

  BrunoRCarboneVSorriso-ValvoLBavassanoB. Radial Evolution of Solar Wind Intermittency in the Inner Heliosphere. J Geophys Res (2003) 108:1130. 10.1029/2002JA009615

  • CrossRef
  • Google Scholar

• 40.

  BrunoRTelloniDPrimaveraLPietropaoloED'AmicisRSorriso-ValvoLet alRadial Evolution of the Intermittency of Density Fluctuations in the Fast Solar Wind. ApJ (2014) 786:53. 10.1088/0004-637x/786/1/53

  • CrossRef
  • Google Scholar

• 41.

  NeugebauerMClayDRGoldsteinBETsurutaniBTZwicklRD. A Reexamination of Rotational and Tangential Discontinuities in the Solar Wind. J Geophys Res (1984) 89:5395–408. 10.1029/JA089iA07p05395

  • CrossRef
  • Google Scholar

• 42.

  HorburyTSBurgessDFränzMOwenCJ. Three Spacecraft Observations of Solar Wind Discontinuities. Geophys Res Lett (2001) 28:677–80. 10.1029/2000GL000121

  • CrossRef
  • Google Scholar

• 43.

  KnetterTNeubauerFMHorburyTBaloghA. Four-point Discontinuity Observations Using Cluster Magnetic Field Data: A Statistical Survey. J Geophys Res (2004) 109:A06102. 10.1029/2003JA010099

  • CrossRef
  • Google Scholar

• 44.

  VasquezBJAbramenkoVIHaggertyDKSmithCW. Numerous Small Magnetic Field Discontinuities of Bartels Rotation 2286 and the Potential Role of Alfvénic Turbulence. J Geophys Res Space Phys (2007) 112:A11102. 10.1029/2007ja012504

  • CrossRef
  • Google Scholar

• 45.

  PaschmannGHaalandSSonnerupBKnetterT. Discontinuities and Alfvénic Fluctuations in the Solar Wind. Ann Geophys (2013) 31:871–87. 10.5194/angeo-31-871-2013

  • CrossRef
  • Google Scholar

• 46.

  TsurutaniBTHoCM. A Review of Discontinuities and Alfvén Waves in Interplanetary Space: Ulysses Results. Rev Geophys (1999) 37:517–41. 10.1029/1999RG900010

  • CrossRef
  • Google Scholar

• 47.

  HudsonPD. Discontinuities in an Anisotropic Plasma and Their Identification in the Solar Wind. Planet Space Sci (1970) 18:1611–22. 10.1016/0032-0633(70)90036-x

  • CrossRef
  • Google Scholar

• 48.

  NeugebauerM. Alignment of Velocity and Field Changes across Tangential Discontinuities in the Solar Wind. J Geophys Res (1985) 90:6627–30. 10.1029/JA090iA07p06627

  • CrossRef
  • Google Scholar

• 49.

  BurlagaLF. Nature and Origin of Directional Discontinuities in the Solar Wind. J Geophys Res (1971) 76:4360–5. 10.1029/JA076i019p04360

  • CrossRef
  • Google Scholar

• 50.

  TurnerJMSiscoeGL. Orientations of ‘Rotational’ and ‘Tangential’ Discontinuities in the Solar Wind. J Geophys Res (1971) 76:1816–22. 10.1029/ja076i007p01816

  • CrossRef
  • Google Scholar

• 51.

  SmithEJ. Identification of Interplanetary Tangential and Rotational Discontinuities. J Geophys Res (1973) 78:2054–63. 10.1029/JA078i013p02054

  • CrossRef
  • Google Scholar

• 52.

  NeugebauerM. Comment on the Abundances of Rotational and Tangential Discontinuities in the Solar Wind. J Geophys Res (2006) 111:A04103. 10.1029/2005JA011497

  • CrossRef
  • Google Scholar

• 53.

  ArtemyevAVAngelopoulosVHalekasJSVinogradovAAVaskoIYZelenyiLM. Dynamics of Intense Currents in the Solar Wind. Astrophysical J (2018) 859:95. 10.3847/1538-4357/aabe89

  • CrossRef
  • Google Scholar

• 54.

  ArtemyevAVAngelopoulosVVaskoIY. Kinetic Properties of Solar Wind Discontinuities at 1 AU Observed by ARTEMIS. J Geophys Res Space Phys (2019) 124:3858–70. 10.1029/2019JA026597

  • CrossRef
  • Google Scholar

• 55.

  SonnerupBUScheibleM. Minimum and Maximum Variance Analysis. Anal Methods multi-spacecraft Data (1998) 1:185–220.

  • Google Scholar

• 56.

  LeppingRPBehannonKW. Magnetic Field Directional Discontinuities: 1. Minimum Variance Errors. J Geophys Res (1980) 85:4695–703. 10.1029/JA085iA09p04695

  • CrossRef
  • Google Scholar

• 57.

  ZhdankinVBoldyrevSPerezJCTobiasSM. Energy Dissipation in Magnetohydrodynamic Turbulence: Coherent Structures or “Nanoflares”?ApJ (2014) 795:127. 10.1088/0004-637X/795/2/127

  • CrossRef
  • Google Scholar