Abstract

Abstract. The present work has investigated the midlatitudinal magnetopause locations under radial interplanetary field (RIMF) conditions. Among 262 (256) earthward (sunward) RIMF events from years of 2001 to 2009, Cluster satellites have crossed the magnetopause 22(12) times, with 10 (7) events occurring at midlatitudes. The observed midlatitudinal magnetopause positions are compared with two empirical magnetopause models (Shue et al., 1998; Boardsen et al., 2000) (hereafter referred to as the Shue98 model and the Boardsen00 model). The observation–model differences exhibit local time asymmetry. For earthward RIMF cases, the Shue98 model underestimates the magnetopause positions in the postnoon sector, while it overestimates the magnetopause positions in the dawn and dusk sectors. The Boardsen00 model generally underestimates the magnetopause after 6 MLT (magnetic local time), with larger deviations in the postnoon sector as compared to those in the prenoon. For sunward RIMF cases, the selected events are mainly clustered around the dawn and dusk sectors. The comparison with the Shue98 model indicates contractions in the dawn and expansions in the dusk sector, while the comparison with Boardsen00 indicates general expansions, with larger expansions in the later local time sectors. The local time variations in the differences between observations and the Shue98 and the Boardsen00 models indicate that the real magnetopause could be asymmetrically shaped during radial IMF periods, which should be considered by magnetopause models. The observation–model differences in the magnetopause positions (Δ RMP) during RIMF periods correlate well with the solar wind dynamic pressure, with larger Δ RMP for larger Pd. The southern magnetopause expands further outward relative to the model prediction when the dipole tilt angle is more negative (local summer in the Southern Hemisphere). For earthward RIMF cases, the generally good correlations between Δ RMP and the IMF cone angle are consistent with the previous hypothesis (Dušík et al., 2010) that, with more radial IMF, the subsolar magnetopause will expand further outward, owever, this is not the case for the comparison with Boardsen00 during sunward IMF periods, as it shows less dependence on the IMF cone angle.

Highlights

  • The magnetopause is a thin boundary layer balanced by the total pressure in the magnetosheath and the magnetic pressure in the magnetosphere

  • The local time variations in the differences between observations and the Shue98 or the Boardsen00 models indicate that the real magnetopause could be asymmetrically shaped during radial interplanetary magnetic field (IMF) periods, which should be considered by magnetopause models

  • From the years 2001 to 2009, Cluster satellites have crossed the magnetopause 22 (12) times, with 10 (7) events occurring in midlatitudes during earthward radial IMF (RIMF) periods

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Summary

Introduction

The magnetopause is a thin boundary layer balanced by the total pressure in the magnetosheath and the magnetic pressure in the magnetosphere. Boardsen et al (2000) have constructed an empirical magnetopause model parameterized by solar wind dynamic pressure, IMF Bz and dipole tilt angle, based on highlatitude magnetopause crossings from the Hawkeye observations and nose crossings from both Roelof and Sibeck (1993) and the Hawkeye spacecraft. For disturbed conditions the dayside magnetopause is more accurately predicted by models that have taken into account the saturation effect and dawn–dusk asymmetry (Dmitriev et al, 2004, 2011; Shue et al, 1998). In the present work we will investigate the magnetopause locations during radial IMF conditions when IMF is parallel/antiparallel to the solar wind velocity. In the Discussion section we compare the results with previous reports and offer explanations for the results

Satellite data
The Shue98 model
The Boardsen00 model
Case study
19 MAY 2002
Multi-events study
Discussion
Findings
14 Apr 2009
Summary
Full Text
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