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Why does the subsolar magnetopause move sunward for radial interplanetary magnetic field?

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11320%2F12%3A10130673" target="_blank" >RIV/00216208:11320/12:10130673 - isvavai.cz</a>

  • Result on the web

    <a href="http://dx.doi.org/10.1029/2011JA017429" target="_blank" >http://dx.doi.org/10.1029/2011JA017429</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1029/2011JA017429" target="_blank" >10.1029/2011JA017429</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Why does the subsolar magnetopause move sunward for radial interplanetary magnetic field?

  • Original language description

    This paper analyzes the distribution of different pressure components (dynamic, thermal, magnetic) in the magnetosheath along the Sun-Earth line for northward and radial interplanetary magnetic field (IMF) orientations with motivation to explain an unusual location and shape of the magnetopause often observed during the intervals of the radial IMF. The analysis employs isotropic and anisotropic MHD models, and their results are compared with the statistical processing of THEMIS observations. We have found that (1) the temperature anisotropy in the magnetosheath controls the pressure distribution near the magnetopause, and (2) the total pressure exerted on the subsolar magnetopause depends on the IMF orientation being significantly lower than the solarwind dynamic pressure for the radial IMF. The results of both MHD simulations and statistical investigations are quantitatively consistent with already published observations of the average magnetopause location as a function of the IMF o

  • Czech name

  • Czech description

Classification

  • Type

    J<sub>x</sub> - Unclassified - Peer-reviewed scientific article (Jimp, Jsc and Jost)

  • CEP classification

    BL - Plasma physics and discharge through gases

  • OECD FORD branch

Result continuities

  • Project

    Result was created during the realization of more than one project. More information in the Projects tab.

  • Continuities

    P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)<br>Z - Vyzkumny zamer (s odkazem do CEZ)<br>S - Specificky vyzkum na vysokych skolach

Others

  • Publication year

    2012

  • Confidentiality

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Data specific for result type

  • Name of the periodical

    Journal of Geophysical Research

  • ISSN

    0148-0227

  • e-ISSN

  • Volume of the periodical

    117

  • Issue of the periodical within the volume

    A05

  • Country of publishing house

    US - UNITED STATES

  • Number of pages

    13

  • Pages from-to

  • UT code for WoS article

    000304014300001

  • EID of the result in the Scopus database