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Statistical investigation of gravity wave characteristics in the ionosphere

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F68378289%3A_____%2F21%3A00540569" target="_blank" >RIV/68378289:_____/21:00540569 - isvavai.cz</a>

  • Result on the web

    <a href="https://earth-planets-space.springeropen.com/articles/10.1186/s40623-021-01379-3" target="_blank" >https://earth-planets-space.springeropen.com/articles/10.1186/s40623-021-01379-3</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1186/s40623-021-01379-3" target="_blank" >10.1186/s40623-021-01379-3</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Statistical investigation of gravity wave characteristics in the ionosphere

  • Original language description

    Propagation of medium-scale gravity waves (GWs) in the thermosphere/ionosphere is observed remotely, using multi-frequency and multi-point continuous Doppler sounding system located in the western part of Czechia. Reflection heights of the sounding radio waves are determined from a nearby ionosonde. Phase velocity vectors of GWs are calculated from time/phase delays between signals corresponding to different transmitter–receiver pairs that reflect in the ionosphere at different locations. As various frequencies reflect at different heights, reflection points of radio signals are separated both horizontally and vertically, and the investigation of GW propagation in the ionosphere is performed in three dimensions. Results obtained for two 1-year periods representing the solar maximum (July 2014–June 2015) and current solar minimum (September 2018–August 2019) are presented. It is shown that GWs in the ionosphere usually propagated with wave vectors directed obliquely downward. A statistical distribution of wave vector elevation angles is presented. A model of neutral winds is used to estimate the wave characteristics in the wind-rest frame. It is found that the distribution of elevation angles is narrower in the wind-rest frame than in the Earth frame. Seasonal and diurnal changes of propagation directions and attenuations of GWs are discussed. The wind-rest frame wavelengths of the analyzed GWs were usually from ~ 80 to 300 km, and the propagation velocities were mostly between ~ 100 and ~ 220 m/s.

  • 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

    10305 - Fluids and plasma physics (including surface physics)

Result continuities

  • Project

    <a href="/en/project/GA18-01969S" target="_blank" >GA18-01969S: Atmospheric waves: dynamics and vertical coupling</a><br>

  • Continuities

    I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Others

  • Publication year

    2021

  • Confidentiality

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

Data specific for result type

  • Name of the periodical

    Earth, Planets and Space

  • ISSN

    1880-5981

  • e-ISSN

    1880-5981

  • Volume of the periodical

    73

  • Issue of the periodical within the volume

    1

  • Country of publishing house

    DE - GERMANY

  • Number of pages

    16

  • Pages from-to

    60

  • UT code for WoS article

    000625387100001

  • EID of the result in the Scopus database

    2-s2.0-85102078925