All

What are you looking for?

All
Projects
Results
Organizations

Quick search

  • Projects supported by TA ČR
  • Excellent projects
  • Projects with the highest public support
  • Current projects

Smart search

  • That is how I find a specific +word
  • That is how I leave the -word out of the results
  • “That is how I can find the whole phrase”

Determination of vertical profiles of shell currents in the ionosphere

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985815%3A_____%2F25%3A00618396" target="_blank" >RIV/67985815:_____/25:00618396 - isvavai.cz</a>

  • Result on the web

    <a href="https://hdl.handle.net/11104/0365405" target="_blank" >https://hdl.handle.net/11104/0365405</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.5194/angeo-43-193-2025" target="_blank" >10.5194/angeo-43-193-2025</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Determination of vertical profiles of shell currents in the ionosphere

  • Original language description

    In previous works, we found Euler potentials for the combined magnetic field of Earth's dipole, field-aligned currents, ring current, and the magnetopause surface currents (represented by Dungey's term) in the magnetosphere. Field-aligned currents, also known as Birkeland currents, experience closure in the ionosphere through the shell current patterns, also known as Pedersen and Cowley currents. Field-aligned currents can be measured at an altitude of around 800 km and can be reconstructed in the entire magnetosphere by means of tracing along the magnetic-field lines. The determination of shell currents is more difficult. They can only be measured in the ionosphere because they form a closure of field-aligned currents in the ionosphere. Analytical modeling and numerical modeling of the shell currents are not easy tasks and require knowledge of the conductivity tensor in the ionosphere. We propose an alternative approach for shell current modeling. In this paper, we determine the current density distribution in a finite-thickness ionosphere. Our system consists of the ionosphere, a region above it (outer region), and a region below it (inner region). The dipole field is present in the entire system. In addition, there is a field generated by the field-aligned currents in the outer region. We search for a continuation of these currents into the ionosphere, that is, for shell currents.

  • Czech name

  • Czech description

Classification

  • Type

    J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database

  • CEP classification

  • OECD FORD branch

    10308 - Astronomy (including astrophysics,space science)

Result continuities

  • Project

    <a href="/en/project/GA21-26463S" target="_blank" >GA21-26463S: Magnetopause processes, their drivers and consequences</a><br>

  • Continuities

    I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Others

  • Publication year

    2025

  • Confidentiality

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

Data specific for result type

  • Name of the periodical

    Annales Geophysicae

  • ISSN

    0992-7689

  • e-ISSN

    1432-0576

  • Volume of the periodical

    43

  • Issue of the periodical within the volume

    1

  • Country of publishing house

    DE - GERMANY

  • Number of pages

    8

  • Pages from-to

    193-200

  • UT code for WoS article

    001446584700001

  • EID of the result in the Scopus database

    2-s2.0-105000449553