Unexpected Southern Hemisphere ionospheric response to geomagnetic storm of 15 August 2015
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F68378289%3A_____%2F18%3A00486122" target="_blank" >RIV/68378289:_____/18:00486122 - isvavai.cz</a>
Výsledek na webu
<a href="http://dx.doi.org/10.5194/angeo-36-71-2018" target="_blank" >http://dx.doi.org/10.5194/angeo-36-71-2018</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.5194/angeo-36-71-2018" target="_blank" >10.5194/angeo-36-71-2018</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Unexpected Southern Hemisphere ionospheric response to geomagnetic storm of 15 August 2015
Popis výsledku v původním jazyce
Geomagnetic storms are the most pronounced phenomenon of space weather. When studying ionospheric response to a storm of 15 August 2015, an unexpected phenomenon was observed at higher middle latitudes of the Southern Hemisphere. This phenomenon was a localized total electron content (TEC) enhancement (LTE) in the form of two separated plumes, which peaked southward of South Africa. The plumes were first observed at 05:00UT near the southwestern coast of Australia. The southern plume was associated with local time slightly after noontime (1- 2h after local noon). The plumes moved with the Sun. They peaked near 13:00 UT southward of South Africa. The southern plume kept constant geomagnetic latitude (63-64oS), it persisted for about 10h, whereas the northern plume persisted for about 2h more. Both plumes disappeared over the South Atlantic Ocean. No similar LTE event was observed during the prolonged solar activity minimum period of 2006-2009. In 2012-2016 we detected altogether 26 LTEs and all of them were associated with the southward excursion of Bz. The negative Bz excursion is a necessary but not sufficient condition for the LTE occurrence as during some geomagnetic storms associated with negative Bz excursions the LTE events did not appear.
Název v anglickém jazyce
Unexpected Southern Hemisphere ionospheric response to geomagnetic storm of 15 August 2015
Popis výsledku anglicky
Geomagnetic storms are the most pronounced phenomenon of space weather. When studying ionospheric response to a storm of 15 August 2015, an unexpected phenomenon was observed at higher middle latitudes of the Southern Hemisphere. This phenomenon was a localized total electron content (TEC) enhancement (LTE) in the form of two separated plumes, which peaked southward of South Africa. The plumes were first observed at 05:00UT near the southwestern coast of Australia. The southern plume was associated with local time slightly after noontime (1- 2h after local noon). The plumes moved with the Sun. They peaked near 13:00 UT southward of South Africa. The southern plume kept constant geomagnetic latitude (63-64oS), it persisted for about 10h, whereas the northern plume persisted for about 2h more. Both plumes disappeared over the South Atlantic Ocean. No similar LTE event was observed during the prolonged solar activity minimum period of 2006-2009. In 2012-2016 we detected altogether 26 LTEs and all of them were associated with the southward excursion of Bz. The negative Bz excursion is a necessary but not sufficient condition for the LTE occurrence as during some geomagnetic storms associated with negative Bz excursions the LTE events did not appear.
Klasifikace
Druh
J<sub>imp</sub> - Článek v periodiku v databázi Web of Science
CEP obor
—
OECD FORD obor
10509 - Meteorology and atmospheric sciences
Návaznosti výsledku
Projekt
—
Návaznosti
I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace
Ostatní
Rok uplatnění
2018
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
Annales Geophysicae
ISSN
0992-7689
e-ISSN
—
Svazek periodika
36
Číslo periodika v rámci svazku
1
Stát vydavatele periodika
DE - Spolková republika Německo
Počet stran výsledku
9
Strana od-do
71-79
Kód UT WoS článku
000423022100001
EID výsledku v databázi Scopus
2-s2.0-85040924059