نتایج جستجو برای: called the magnetopause therefore

تعداد نتایج: 16056037  

پایان نامه :وزارت علوم، تحقیقات و فناوری - دانشگاه صنعتی اصفهان 1390

section{introduction} the concept of {sl cartan geometry} appeared at the beginning of the twentieth century, when {e}lie cartan was working on the so-called {sl equivalence problem}, the aim of which is to determine whether two given geometric structures can be mapped bijectively onto each other by some diffeomorphism. this problem can be considered in many different contexts, such as ...

پایان نامه :وزارت علوم، تحقیقات و فناوری - دانشکده اصول الدین 1389

چکیده «محکم و متشابه»، «نسخ» و «قرائات» از موضوعات مهم علوم قرآنی است. آیت الله معرفت در هر سه موضوع ضمن نقد دیدگاههای گذشته و رایج، به ارائه نظریاتی بدیع پرداخته اند. تعریف روشن از محکم و متشابه، تفاوت بین متشابه و مبهم، طبقه بندی تشابه به ذاتی و عرضی و ضابطه مند ساختن معانی تأویلی و باطنی، از جمله نوآوری های آیت الله معرفت در حوزه محکم و متشابه به شمار می رود. در موضوع نسخ، شاهد دو قرائت...

2007
J. A. Wild S. E. Milan J. A. Davies M. W. Dunlop D. M. Wright C. M. Carr A. Balogh H. Rème A. N. Fazakerley

We present spaceand ground-based observations of the signatures of magnetic reconnection during an interval of duskward-oriented interplanetary magnetic field on 25 March 2004. In situ field and plasma measurements are drawn from the Double Star and Cluster satellites during traversals of the pre-noon sector dayside magnetopause at low and high latitudes, respectively. These reveal the typical ...

2001
K. Kauristie T. I. Pulkkinen O. Amm A. Viljanen M. Syrjäsuo P. Janhunen S. Massetti S. Orsini M. Candidi J. Watermann E. Donovan P. Prikryl I. R. Mann P. Eglitis C. Smith W. F. Denig H. J. Opgenoorth

On 7 December 2000, during 13:30–15:30 UT the MIRACLE all-sky camera at Ny Ålesund observed auroras at high-latitudes (MLAT ∼ 76) simultaneously when the Cluster spacecraft were skimming the magnetopause in the same MLT sector (at ∼ 16:00–18:00 MLT). The location of the auroras (near the ionospheric convection reversal boundary) and the clear correlation between their dynamics and IMF variation...

Journal: :South African Journal of Science 2010

Journal: :Social Thought and Research 1998

Journal: :Journal Of Geophysical Research: Space Physics 2021

Magnetosheath jets are localized high-dynamic pressure pulses originating at Earth's bow shock and propagating earthward through the magnetosheath. Jets can influence magnetospheric dynamics upon impacting magnetopause; however, many dissipate before reaching it. In this study we present a database of 13,096 observed by Time History Events Macroscale Interactions during Substorms spacecraft fro...

Journal: :Physical review letters 2011
M W Dunlop Q-H Zhang Y V Bogdanova M Lockwood Z Pu H Hasegawa J Wang M G G T Taylor J Berchem B Lavraud J Eastwood M Volwerk C Shen J-K Shi D Constantinescu H Frey A N Fazakerley D Sibeck P Escoubet J A Wild Z-X Liu

The extent of where magnetic reconnection (MR), the dominant process responsible for energy and plasma transport into the magnetosphere, operates across Earth's dayside magnetopause has previously been only indirectly shown by observations. We report the first direct evidence of X-line structure resulting from the operation of MR at each of two widely separated locations along the tilted, subso...

2005
I. J. Coleman

When the interplanetary magnetic field (IMF) encounters the Earth’s magnetosphere, it is compressed and distorted. This distortion is known as draping, and plays an important role in the interaction between the IMF and the geomagnetic field. This paper considers a particular aspect of draping, namely how the orientation of the IMF in a plane perpendicular to the Sun-Earth line (the clock angle)...

2015
A. Y. Ukhorskiy M. I. Sitnov R. M. Millan B. T. Kress J. F. Fennell S. G. Claudepierre R. J. Barnes

The outer radiation belt consists of relativistic (>0.5 MeV) electrons trapped on closed trajectories around Earth where the magnetic field is nearly dipolar. During increased geomagnetic activity, electron intensities in the belt can vary by orders of magnitude at different spatial and temporal scales. The main phase of geomagnetic storms often produces deep depletions of electron intensities ...

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