scholarly journals The role of aerodynamic drag in dynamics of coronal mass ejections

2008 ◽  
Vol 4 (S257) ◽  
pp. 271-277
Author(s):  
Bojan Vršnak ◽  
Dijana Vrbanec ◽  
Jaša Čalogović ◽  
Tomislav Žic

AbstractDynamics of coronal mass ejections (CMEs) is strongly affected by the interaction of the erupting structure with the ambient magnetoplasma: eruptions that are faster than solar wind transfer the momentum and energy to the wind and generally decelerate, whereas slower ones gain the momentum and accelerate. Such a behavior can be expressed in terms of “aerodynamic” drag. We employ a large sample of CMEs to analyze the relationship between kinematics of CMEs and drag-related parameters, such as ambient solar wind speed and the CME mass. Employing coronagraphic observations it is demonstrated that massive CMEs are less affected by the aerodynamic drag than light ones. On the other hand, in situ measurements are used to inspect the role of the solar wind speed and it is shown that the Sun-Earth transit time is more closely related to the wind speed than to take-off speed of CMEs. These findings are interpreted by analyzing solutions of a simple equation of motion based on the standard form for the drag acceleration. The results show that most of the acceleration/deceleration of CMEs on their way through the interplanetary space takes place close to the Sun, where the ambient plasma density is still high. Implications for the space weather forecasting of CME arrival-times are discussed.

2012 ◽  
Vol 8 (S294) ◽  
pp. 487-488
Author(s):  
Li-Jia Liu ◽  
Bo Peng

AbstractThe Sun affects the Earth in multiple ways. In particular, the material in interplanetary space comes from coronal expansion in the form of solar wind, which is the primary source of the interplanetary medium. Ground-based Interplanetary Scintillation (IPS) observations are an important and effective method for measuring solar wind speed and the structures of small diameter radio sources. In this paper we will discuss the IPS observations in China.


2021 ◽  
Author(s):  
Tereza Durovcova ◽  
Jana Šafránková ◽  
Zdeněk Němeček

<p>Two large-scale interaction regions between the fast solar wind emanating from coronal holes and the slow solar wind coming from streamer belt are usually distinguished. When the fast stream pushes up against the slow solar wind ahead of it, a compressed interaction region that co-rotates with the Sun (CIR) is created. It was already shown that the relative abundance of alpha particles, which usually serve as one of solar wind source identifiers can change within this region. By symmetry, when the fast stream outruns the slow stream, a corotating rarefaction region (CRR) is formed. CRRs are characterized by a monotonic decrease of the solar wind speed, and they are associated with the regions of small longitudinal extent on the Sun. In our study, we use near-Earth measurements complemented by observations at different heliocentric distances, and focus on the behavior of alpha particles in the CRRs because we found that the large variations of the relative helium abundance (AHe) can also be observed there. Unlike in the CIRs, these variations are usually not connected with the solar wind speed and alpha-proton relative drift changes. We thus apply a superposed-epoch analysis of identified CRRs with a motivation to determine the global profile of alpha particle parameters through these regions. Next, we concentrate on the cases with largest AHe variations and investigate whether they can be associated with the changes of the solar wind source region or whether there is a relation between the AHe variations and the non-thermal features in the proton velocity distribution functions like the temperature anisotropy and/or presence of the proton beam.</p>


2020 ◽  
Author(s):  
Fang Shen ◽  
Yousheng Liu ◽  
Yi Yang

<p>Previous research has shown that the deflection of coronal mass ejections (CMEs) in interplanetary space, especially fast CMEs, is a common phenomenon. The deflection caused by the interaction with background solar wind is an important factor to determine whether CMEs could hit Earth or not. As the Sun rotates, there will be interactions between solar wind flows with different speeds. When faster solar wind runs into slower solar wind<br>ahead, it will form a compressive area corotating with the Sun, which is called a corotating interaction region (CIR). These compression regions always have a higher density than the common background solar wind. When interacting with CME, will this make a difference in the deflection process of CME? In this research, first, a three-dimensional (3D) flux-rope CME initialization model is established based on the graduated cylindrical shell (GCS)<br>model. Then this CME model is introduced into the background solar wind, which is obtained using a 3D IN (INterplanetary) -TVD-MHD model. The Carrington Rotation (CR) 2154 is selected as an example to simulate the propagation and deflection of fast CME when it interacts with background solar wind, especially with the CIR structure.</p><p>The simulation results show that: (1) the fast CME will deflect eastward when it propagates into the background solar wind without the CIR; (2) when the fast CME hits the CIR on its west side, it will also deflect eastward, and the deflection angle will increase compared with the situation without CIR.</p>


2020 ◽  
Vol 891 (2) ◽  
pp. 165 ◽  
Author(s):  
Martin A. Reiss ◽  
Peter J. MacNeice ◽  
Karin Muglach ◽  
Charles N. Arge ◽  
Christian Möstl ◽  
...  

Solar Physics ◽  
2011 ◽  
Vol 276 (1-2) ◽  
pp. 315-336 ◽  
Author(s):  
M. Tokumaru ◽  
S. Fujimaki ◽  
M. Higashiyama ◽  
A. Yokobe ◽  
T. Ohmi ◽  
...  

2018 ◽  
Vol 15 (1) ◽  
pp. 39
Author(s):  
Siska Filawati

Interplanetary space is a hazard precursor for solar eruption toward earth. The solar eruptions enhance electron flux that can lead to anomalies, shifts, and permanent damage to spacecraft, e.g. satellites. The data used in this paper are interplanetary space data represented by interplanetary magnetic field (Bz) and solar wind speed, as well as Dst and AE indexes as comparison indicating disturbance has reached Earth’s poles and equator during 2011-2012. The method used is to determine the value of maximum and minimum Bz in the year 2011-2012 which is taken five days before and after. Analysis and calculation of correlation is done to data of Bz-electron flux and solar wind velocity-electron flux. Clarification of disturbence in interplanetary space and outer electron radiation belt is using index data Dst and AE indexes are used to clarify interplanetary space and outer electron radiation belt disturbances. The aim of this study is to determine the characteristics of interplanetary space that can increase the electron flux so that the space weather early warning can be done. It was found that the period of electron flux enhancement after decrease and increase of Bz was 2 to 3 days. The electron flux would enhance when interplanetary space was in its normal condition at solar wind speed 500 km/sec and Bz is -5 nT to +5 nT. Electron flux correlation with solar wind velocity was better than with Bz. ABSTRAKKondisi ruang antarplanet merupakan prekursor bahaya erupsi matahari terhadap bumi. Erupsi matahari dapat menyebabkan peningkatan fluks elektron. Tingginya fluks elektron dapat menyebabkan anomali, pergeseran, dan kerusakan permanen pada wahana antariksa, misal satelit. Data yang digunakan pada makalah ini adalah data ruang antarplanet yang diwakili oleh kondisi medan magnet antarplanet (Bz) dan kecepatan angin matahari yang merupakan prekursor peningkatan fluks elektron serta data indeks Dst dan indeks AE sebagai pembanding bahwa gangguan telah mencapai kutub dan ekuator bumi selama rentang waktu 2011-2012. Metode yang digunakan adalah menentukan nilai Bz maksimum dan minimum dalam tahun 2011-2012 yang selanjutnya dari penanggalan data tersebut diambil data lima hari sebelum dan sesudah. Analisis dan perhitungan korelasi dilakukan terhadap data Bz-fluks elektron dan kecepatan angin matahari-fluks elektron. Klarifikasi gangguan yang terjadi di ruang antarplanet dan sabuk radiasi elektron luar menggunakan data indeks Dst dan indeks AE. Tujuan ditulisnya makalah ini adalah untuk mengetahui karakteristik kondisi ruang antarplanet yang dapat meningkatkan fluks elektron agar peringatan dini cuaca antariksa dapat dilakukan. Hasil yang didapatkan adalah waktu yang dibutuhkan fluks elektron setelah terjadi penurunan dan peningkatan Bz adalah 2 hingga 3 hari, fluks elektron akan meningkat saat kondisi ruang antarplanet normal yaitu pada kecepatan 500 km/detik dan Bz -5 nT hingga +5 nT, korelasi fluks elektron dengan kecepatan angin matahari lebih baik dibanding fluks elektron dengan Bz.


2018 ◽  
Vol 13 (S340) ◽  
pp. 163-164
Author(s):  
Veena Choithani ◽  
Rajmal Jain ◽  
Duggirala Pallamraju

AbstractWe study 30 solar flare events associated with coronal mass ejections (CMEs) that produced geomagnetic storms as measured in Dst index. Our study reveals that the magnitude of Dst index is significantly associated with maximum solar wind speed, peak of Bz component of the IMF and the product of peak Bz and solar wind speed (minimum and maximum). From our investigations, it can be inferred that CMEs travel with higher speed in the beginning and their speed reduces as they reach L1 location.


1996 ◽  
Vol 154 ◽  
pp. 97-104
Author(s):  
Richard Woo

AbstractSince the 1950s, a wide variety of radio observations based on scattering by electron density fluctuations in the solar wind has provided much of our information on density fluctuations and solar wind speed near the source region of the solar wind. This paper reviews recent progress in the understanding of the nature of these density fluctuations and their relationship to features on the Sun. The results include the first measurements of fine-scale structure within coronal streamers and evidence for structure in solar wind speed in the inner corona.


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