2021
DOI: 10.3847/1538-4365/abf659
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Strength of the Termination Shock Inferred from the Globally Distributed Energetic Neutral Atom Flux from IBEX

Abstract: In this study, we estimate the heliospheric termination shock (HTS) compression ratio at multiple directions in the sky from a quantitative comparison of the observed and simulated inner heliosheath (IHS) energetic neutral atom (ENA) fluxes. We use a 3D steady-state simulation of the heliosphere to simulate the ENA fluxes by postprocessing the MHD plasma using a multi-Maxwellian distribution for protons in the IHS. The simulated ENA fluxes are compared with time exposure–averaged IBEX-Hi data for the first 3 y… Show more

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Cited by 10 publications
(12 citation statements)
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“…(2010) method (Zirnstein et al 2017;Kornbleuth et al 2020Kornbleuth et al , 2021Shrestha et al 2021), scaling factors ranging from 1.8 to 2.5 were required to match observations. These methods only included two populations of PUIs: transmitted PUIs and reflected PUIs.…”
Section: Simulating the Ena Flux In The Heliosheathmentioning
confidence: 99%
See 1 more Smart Citation
“…(2010) method (Zirnstein et al 2017;Kornbleuth et al 2020Kornbleuth et al , 2021Shrestha et al 2021), scaling factors ranging from 1.8 to 2.5 were required to match observations. These methods only included two populations of PUIs: transmitted PUIs and reflected PUIs.…”
Section: Simulating the Ena Flux In The Heliosheathmentioning
confidence: 99%
“…This is usually done by partitioning the MHD plasma quantities to represent multiple ion species in postprocessing downstream of the termination shock to properly model ENAs. ENA models that use a combined Maxwellian approach to replicate a kappa distribution in the solar wind plasma for three ion populations at the termination shock (thermal ions, "transmitted PUIs" which have sufficient energy to overcome the cross-shock potential of the termination shock, and "reflected PUIs" which do not initially have sufficient energy to overcome the crossshock potential of the termination shock and are reflected at the shock) require a scaling factor to compare directly with IBEX-Hi observations ranging from 1.8 to 2.5 (Zirnstein et al 2017;Kornbleuth et al 2018Kornbleuth et al , 2020Shrestha et al 2021) regardless of solar wind conditions (steady state or with the inclusion of realistic solar cycle). Baliukin et al (2020) use a kinetic model for PUIs which models the propagation of PUIs in the heliosheath and includes the change in PUI energy due to ∇ • v, where v is the bulk velocity of the plasma, in the heliosheath.…”
Section: Introductionmentioning
confidence: 99%
“…As in Kornbleuth et al (2020), we need to scale modeled ENA maps by a factor of 1.8 to provide an average global agreement with observations. In other works, such as Zirnstein et al (2017) and Shrestha et al (2021) which also use the superposition of Maxwellian distributions for the ions from Zank et al (2010), a scaling factor of 2.5 and ∼3 is required as well, respectively. Baliukin et al (2020) use a kinetic approach to PUI modeling in post-processing and assume that PUIs form a filled shell distribution downstream of the TS.…”
Section: Resultsmentioning
confidence: 99%
“…We use an SW density of 5.74 and 1.82 cm −3 at 1 au depending on heliolatitude for slow and fast SW, respectively, using Equation (4) (Shrestha et al 2020). We note that this compression ratio is greater than the observed HTS compression ratio from V2 (Richardson et al 2008), and the HTS compression ratio inferred from the IBEX ENA observations (Shrestha et al 2021). But its exact value does not have a significant effect on our results since we are only interested in the qualitative nature of the evolution of simulated ENA spectra.…”
Section: Simulation Of Polar Ena Spectrum Evolutionmentioning
confidence: 96%