2022
DOI: 10.3847/1538-4357/ac56da
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Validation of a Wave Heated 3D MHD Coronal-wind Model using Polarized Brightness and EUV Observations

Abstract: The physical properties responsible for the formation and evolution of the corona and heliosphere are still not completely understood. 3D MHD global modeling is a powerful tool to investigate all the possible candidate processes. To fully understand the role of each of them, we need a validation process where the output from the simulations is quantitatively compared to the observational data. In this work, we present the results from our validation process applied to the wave turbulence driven 3D MHD corona-w… Show more

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Cited by 11 publications
(10 citation statements)
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“…1D wind models have also proved to be interesting for their capacity of including realistic physics at reasonable computational costs (Lionello et al 2001;Suzuki & Inutsuka 2005;Grappin et al 2010), and can be used to map the entire sphere to simulate the lower corona as in the MULTI-VP model (Pinto & Rouillard 2017). Other 3D MHD models have been developed and improved over the years with systematic comparisons to both in situ and remote-sensing data for validation; such as AWSoM (van der Holst et al 2010(van der Holst et al , 2014Sachdeva et al 2019); the model from , Usmanov et al (2016, Usmanov et al (2018), Chhiber et al (2021); or Wind-Predict (Réville et al 2015a;Perri et al 2018;Réville et al 2020;Parenti et al 2022). Yet other models have focused on BCs to provide the most physical conditions for time-dependent models (Wu et al 2006), such as in Yalim et al (2017), Singh et al (2018).…”
Section: Introductionmentioning
confidence: 99%
“…1D wind models have also proved to be interesting for their capacity of including realistic physics at reasonable computational costs (Lionello et al 2001;Suzuki & Inutsuka 2005;Grappin et al 2010), and can be used to map the entire sphere to simulate the lower corona as in the MULTI-VP model (Pinto & Rouillard 2017). Other 3D MHD models have been developed and improved over the years with systematic comparisons to both in situ and remote-sensing data for validation; such as AWSoM (van der Holst et al 2010(van der Holst et al , 2014Sachdeva et al 2019); the model from , Usmanov et al (2016, Usmanov et al (2018), Chhiber et al (2021); or Wind-Predict (Réville et al 2015a;Perri et al 2018;Réville et al 2020;Parenti et al 2022). Yet other models have focused on BCs to provide the most physical conditions for time-dependent models (Wu et al 2006), such as in Yalim et al (2017), Singh et al (2018).…”
Section: Introductionmentioning
confidence: 99%
“…The very low atmospheric layers of the corona are important but still difficult to model in two and three dimensions as they involve very steep gradients of density and temperature over only a few thousand kilometers and consequently, much higher spatial resolution would be required. The inner radial boundary is therefore placed in the upper transition region at a fixed temperature of 5 × 10 5 K. A similar approach has been adopted in 3D simulations of Alfvén wave turbulence (Parenti et al 2022).…”
Section: Numerical Setup and Boundary Conditionsmentioning
confidence: 99%
“…Turbulence cannot be sustained in a homogeneous medium with no reflection. Alfvén-wave turbulence could operate when there are counter-propagating Alfvén waves in an inhomogeneous medium where they reflect partially (Goldreich & Sridhar 1995;Cranmer & Van Ballegooijen 2005;Parenti et al 2022;Velli 1993). Counter-propagating Alfvén waves in the corona can couple nonlinearly and produce turbulence that dissipates and heats up the corona (Kraichnan 1999;Dobrowolny et al 1980;Ghosh et al 1988;Dmitruk et al 2001).…”
mentioning
confidence: 99%
See 1 more Smart Citation
“…1-D wind models have also proved to be interesting for their capacity of including realistic physics at reasonable computational costs (Lionello et al 2001;Suzuki & Inutsuka 2005;Grappin et al 2010), and can be used to map the entire sphere to simulate the lower corona as in the MULTI-VP model (Pinto & Rouillard 2017). Other 3-D MHD models have been developed and improved over the years with systematic comparisons to both in-situ and remote-sensing data for validation, such as AWSoM (van der Holst et al 2010;van der Holst et al 2014;Sachdeva et al 2019), the model from Usmanov et al (2014Usmanov et al ( , 2016Usmanov et al ( , 2018; Chhiber et al (2021) or Wind-Predict (Réville et al 2015a;Perri et al 2018;Réville et al 2020;Parenti et al 2022). Yet other models have focused on boundary conditions to provide the most physical conditions for time-dependent models (Wu et al 2006), such as in Yalim et al (2017); Singh et al (2018).…”
Section: Introductionmentioning
confidence: 99%