Pregled bibliografske jedinice broj: 1104114
Relating CME density derived from remote sensing data to CME sheath solar wind plasma pile up as measured in-situ
Relating CME density derived from remote sensing data to CME sheath solar wind plasma pile up as measured in-situ // European Space Weather Symposium
online, 2020. str. 1-1 (poster, međunarodna recenzija, sažetak, znanstveni)
CROSBI ID: 1104114 Za ispravke kontaktirajte CROSBI podršku putem web obrasca
Naslov
Relating CME density derived from remote sensing data to CME
sheath solar wind plasma pile up as measured in-situ
Autori
Manuela Temmer ; Mateja Dumbovic ; Bojan Vrsnak ; Nishtha Sachdeva ; Stephan Heinemann ; Karin Dissauer ; Camilla Scolini ; Eleanna Asvestari ; Astrid Veronig ; Stefan Hofmeister
Vrsta, podvrsta i kategorija rada
Sažeci sa skupova, sažetak, znanstveni
Skup
European Space Weather Symposium
Mjesto i datum
Online, 02.11.2020. - 06.11.2020
Vrsta sudjelovanja
Poster
Vrsta recenzije
Međunarodna recenzija
Ključne riječi
coronal mass ejections, space weather
(coronal mass ejections, space weather forecast)
Sažetak
For better estimating the drag force acting on coronal mass ejections (CMEs) in interplanetary space and ram-pressure at planets, improved knowledge of the evolution of CME density/mass is highly valuable. We investigate a sample of 29 well observed CME-ICME events, for which we determine the de-projected 3D mass (STEREO- A and -B data), and the CME volume using GCS modeling (STEREO, SoHO). Expanding the volume to 1AU distance, we derive the density and compare the results to in-situ proton density measurements separately for the ICME sheath and magnetic structure. A fair agreement between calculated and measured density is derived for the magnetic structure as well for the sheath if taking into account mass pile up of solar wind plasma. We give evidence and observational assessment that during the interplanetary propagation of a CME 1) the magnetic structure has rather constant mass and 2) the sheath region at the front of the driver is formed from piled-up mass that is rather depending on the solar wind density ahead of the CME, than on the CME speed.
Izvorni jezik
Engleski
Znanstvena područja
Fizika
POVEZANOST RADA
Ustanove:
Geodetski fakultet, Zagreb