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”

Observations of traveling ionospheric disturbances driven by gravity waves from sources in the upper and lower atmosphere

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F68378289%3A_____%2F25%3A00639147" target="_blank" >RIV/68378289:_____/25:00639147 - isvavai.cz</a>

  • Result on the web

    <a href="https://angeo.copernicus.org/articles/43/511/2025/" target="_blank" >https://angeo.copernicus.org/articles/43/511/2025/</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.5194/angeo-43-511-2025" target="_blank" >10.5194/angeo-43-511-2025</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Observations of traveling ionospheric disturbances driven by gravity waves from sources in the upper and lower atmosphere

  • Original language description

    The observed traveling ionospheric disturbances (TIDs) are attributed to atmospheric gravity waves generated by auroral sources in the lower thermosphere or gravity waves generated in the troposphere by midlatitude weather systems. TIDs are observed by the Poker Flat Incoherent Scatter Radar (PFISR), the Super Dual Auroral Radar Network (SuperDARN), multipoint and multifrequency continuous Doppler sounders, and Global Navigation Satellite System (GNSS) receivers using the total electron content (TEC) mapping technique. At high latitudes, the solar wind-magnetosphere-ionosphere-thermosphere coupling modulates the dayside ionospheric convection and currents, the source of the equatorward-propagating TIDs. The horizontal equivalent ionospheric currents are estimated from the ground-based magnetometer data using an inversion technique. At midlatitudes, the eastward- to southeastward-propagating medium-scale TIDs that were observed by the high-frequency (HF) Doppler sounding system, as well as in the detrended TEC, are attributed to gravity waves that are generated by geostrophic adjustment processes and shear instability in the intensifying low-pressure systems and are identified in the stratosphere using the ERA5 meteorological reanalysis.

  • 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

    10509 - Meteorology and atmospheric sciences

Result continuities

  • Project

    <a href="/en/project/EH22_008%2F0004605" target="_blank" >EH22_008/0004605: Natural and anthropogenic georisks</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

    2

  • Country of publishing house

    DE - GERMANY

  • Number of pages

    24

  • Pages from-to

    511-534

  • UT code for WoS article

    001571706800001

  • EID of the result in the Scopus database

    2-s2.0-105016818482