Evolution of the alpha-proton Differential Motion across Stream Interaction Regions
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11320%2F19%3A10395966" target="_blank" >RIV/00216208:11320/19:10395966 - isvavai.cz</a>
Výsledek na webu
<a href="https://verso.is.cuni.cz/pub/verso.fpl?fname=obd_publikace_handle&handle=whRdhAhoKW" target="_blank" >https://verso.is.cuni.cz/pub/verso.fpl?fname=obd_publikace_handle&handle=whRdhAhoKW</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.3847/1538-4357/ab01c8" target="_blank" >10.3847/1538-4357/ab01c8</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Evolution of the alpha-proton Differential Motion across Stream Interaction Regions
Popis výsledku v původním jazyce
A corotating interaction region (CIR) develops between the solar wind streams with different bulk speeds emanating from distinct coronal sources. The arising pressure perturbations redistribute momentum between adjacent streams forming the regions of the compressed solar wind around the stream interface. We focus on properties of alpha-particles with respect to protons in CIRs using measurements of the Wind and Helios spacecraft. In the slow solar wind in front of CIRs, the relative helium abundance A(He) is usually low (about 1%) and the alpha-proton differential drift, V-alpha p is close to zero. In the high-speed stream behind CIRs, both of these characteristics are significantly higher. Inside CIRs, a large enhancement of A(He) accompanied by a decrease in V-alpha p is often observed in the compressed and slowed down fast solar wind close to the CIR leading edge. On the other hand, a depletion of A(He) is sometimes present in the compressed and accelerated slow solar winds. We explain these observations in terms of magnetic mirroring of the multicomponent solar wind in a converging magnetic field that develops within CIRs.
Název v anglickém jazyce
Evolution of the alpha-proton Differential Motion across Stream Interaction Regions
Popis výsledku anglicky
A corotating interaction region (CIR) develops between the solar wind streams with different bulk speeds emanating from distinct coronal sources. The arising pressure perturbations redistribute momentum between adjacent streams forming the regions of the compressed solar wind around the stream interface. We focus on properties of alpha-particles with respect to protons in CIRs using measurements of the Wind and Helios spacecraft. In the slow solar wind in front of CIRs, the relative helium abundance A(He) is usually low (about 1%) and the alpha-proton differential drift, V-alpha p is close to zero. In the high-speed stream behind CIRs, both of these characteristics are significantly higher. Inside CIRs, a large enhancement of A(He) accompanied by a decrease in V-alpha p is often observed in the compressed and slowed down fast solar wind close to the CIR leading edge. On the other hand, a depletion of A(He) is sometimes present in the compressed and accelerated slow solar winds. We explain these observations in terms of magnetic mirroring of the multicomponent solar wind in a converging magnetic field that develops within CIRs.
Klasifikace
Druh
J<sub>imp</sub> - Článek v periodiku v databázi Web of Science
CEP obor
—
OECD FORD obor
10305 - Fluids and plasma physics (including surface physics)
Návaznosti výsledku
Projekt
<a href="/cs/project/GA16-04956S" target="_blank" >GA16-04956S: Sluneční vítr jako přírodní laboratoř: struktura, turbulence a rázové vlny.</a><br>
Návaznosti
P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)
Ostatní
Rok uplatnění
2019
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
Astrophysical Journal
ISSN
0004-637X
e-ISSN
—
Svazek periodika
873
Číslo periodika v rámci svazku
1
Stát vydavatele periodika
US - Spojené státy americké
Počet stran výsledku
8
Strana od-do
24
Kód UT WoS článku
000460057100010
EID výsledku v databázi Scopus
2-s2.0-85063481633