Abstract

AbstractEmpirical models of the Earth's bow shock are often used to place in situ measurements in context and to understand the global behavior of the foreshock/bow shock system. They are derived statistically from spacecraft bow shock crossings and typically treat the shock surface as a conic section parameterized according to a uniform solar wind ram pressure, although more complex models exist. Here a global magnetohydrodynamic simulation is used to analyze the variability of the Earth's bow shock under real solar wind conditions. The shape and location of the bow shock is found as a function of time, and this is used to calculate the shock velocity over the shock surface. The results are compared to existing empirical models. Good agreement is found in the variability of the subsolar shock location. However, empirical models fail to reproduce the two‐dimensional shape of the shock in the simulation. This is because significant solar wind variability occurs on timescales less than the transit time of a single solar wind phase front over the curved shock surface. Empirical models must therefore be used with care when interpreting spacecraft data, especially when observations are made far from the Sun‐Earth line. Further analysis reveals a bias to higher shock speeds when measured by virtual spacecraft. This is attributed to the fact that the spacecraft only observes the shock when it is in motion. This must be accounted for when studying bow shock motion and variability with spacecraft data.

Highlights

  • The interaction of the solar wind, streaming out radially from the Sun, with the magnetosphere leads to the formation of a bow shock upstream of the magnetopause, with a turbulent sheath region in between (Burgess & Scholer, 2013; Fairfield, 1976; Krasnoselskikh et al, 2013; Lucek et al, 2005; Ness et al, 1964)

  • A global MHD simulation has been performed on real solar wind parameters during an event analyzed by Maksimovic et al (2003)

  • Size, and velocity of the bow shock is analyzed as it readjusts to the arrival of new solar wind phase fronts

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Summary

Introduction

The interaction of the solar wind, streaming out radially from the Sun, with the magnetosphere leads to the formation of a bow shock upstream of the magnetopause, with a turbulent sheath region (the magnetosheath) in between (Burgess & Scholer, 2013; Fairfield, 1976; Krasnoselskikh et al, 2013; Lucek et al, 2005; Ness et al, 1964). Empirical models of the shock shape and location, derived statistically from spacecraft observations, are crucial in this regard. They are fundamental to many spacecraft investigations of shock and foreshock physics, as they are used to place local measurements in the global context, and to correctly interpret shock geometry. While such models agree well with the average location and shape of bow shock or magnetopause, they often need to be scaled in order to agree with the specific spacecraft crossing location for any particular event (Schwartz, 1998)

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