Fluctuations on vertical profiles of the ionospheric electron density perturbed by the March 11, 2011 M9.0 Tohoku earthquake and tsunami

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F68378289%3A_____%2F19%3A00505560" target="_blank" >RIV/68378289:_____/19:00505560 - isvavai.cz</a>

Výsledek na webu

<a href="https://link.springer.com/article/10.1007/s10291-019-0866-7" target="_blank" >https://link.springer.com/article/10.1007/s10291-019-0866-7</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1007/s10291-019-0866-7" target="_blank" >10.1007/s10291-019-0866-7</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Fluctuations on vertical profiles of the ionospheric electron density perturbed by the March 11, 2011 M9.0 Tohoku earthquake and tsunami

Popis výsledku v původním jazyce

The GPS radio occultation (RO) of FORMOSAT-3/COSMIC (F3/C) with 1-2.5-km-altitude resolution is used to scan fluctuations on vertical profiles of the ionospheric electron density induced by seismic and tsunami waves of the March 11, 2011 M9.0 Tohoku earthquake. The Hilbert-Huang transform is applied to derive the instantaneous wave number and amplitude of the fluctuations in 22 (7 before and 15 after) F3/C profiles within 3000km in radius from the epicenter during the earthquake. Fluctuations of the vertical electron density profile induced by underneath Rayleigh and tsunami waves and their post-waves are examined. It is found that the right underneath Rayleigh wave can induce significant long-wavelength fluctuations of 50-105km on the vertical profile of the electron density, while tsunami and their post-waves activate the prominent short-wavelength fluctuations less than 16km on those profiles in the poleward side of the epicenter. Results show that RO is a powerful tool which is suitable to probe vertical fluctuations in the ionospheric electron density.

Název v anglickém jazyce

Fluctuations on vertical profiles of the ionospheric electron density perturbed by the March 11, 2011 M9.0 Tohoku earthquake and tsunami

Popis výsledku anglicky

The GPS radio occultation (RO) of FORMOSAT-3/COSMIC (F3/C) with 1-2.5-km-altitude resolution is used to scan fluctuations on vertical profiles of the ionospheric electron density induced by seismic and tsunami waves of the March 11, 2011 M9.0 Tohoku earthquake. The Hilbert-Huang transform is applied to derive the instantaneous wave number and amplitude of the fluctuations in 22 (7 before and 15 after) F3/C profiles within 3000km in radius from the epicenter during the earthquake. Fluctuations of the vertical electron density profile induced by underneath Rayleigh and tsunami waves and their post-waves are examined. It is found that the right underneath Rayleigh wave can induce significant long-wavelength fluctuations of 50-105km on the vertical profile of the electron density, while tsunami and their post-waves activate the prominent short-wavelength fluctuations less than 16km on those profiles in the poleward side of the epicenter. Results show that RO is a powerful tool which is suitable to probe vertical fluctuations in the ionospheric electron density.

Druh

J_imp - Článek v periodiku v databázi Web of Science

CEP obor

—

OECD FORD obor

10305 - Fluids and plasma physics (including surface physics)

Projekt

<a href="/cs/project/GA18-01969S" target="_blank" >GA18-01969S: Atmosférické vlny: dynamika a vazby mezi vrstvami</a><br>

Návaznosti

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2019

Kód důvěrnosti údajů

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

Název periodika

GPS Solutions

ISSN

1080-5370

e-ISSN

—

Svazek periodika

23

Číslo periodika v rámci svazku

3

Stát vydavatele periodika

DE - Spolková republika Německo

Počet stran výsledku

10

Strana od-do

76

Kód UT WoS článku

000469020100003

EID výsledku v databázi Scopus

2-s2.0-85067673277