A comparative study of reconnection

X-line predictions on dayside magnetopause of Earth

Ramiz A. Qudsi,   Brian Walsh, J. Broll

Boston University,   Los Alamos National Lab

*(qudsira@bu.edu)

(https://qudsiramiz.github.io)

                                                                                                            1, *                                           1                          2

                                                              1                                               2

Qudsi                                                                Center for Space Physics, BU                                                 qudsira@bu.edu

Outline:

  • Region of interest
  • Location of x-line
    • Different models
  • Data
  • Results
  • Discussions

Qudsi                                                                Center for Space Physics, BU                                                 qudsira@bu.edu

The BASICS

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Source: NASA

Qudsi                                                                Center for Space Physics, BU                                                 qudsira@bu.edu

Region of interest:

[Broll et al., 2017]

Source: wikipedia

Qudsi                                                                Center for Space Physics, BU                                                 qudsira@bu.edu

Location of x-line: Models

Local field bisection [Moore et al., 2002]

Maximum exhaust speed  [Swisdak and Drake, 2007]

Maximum magnetic shear [Trattner et al., 2007]

Maximum reconnecting field energy [Hesse et al., 2013]

Qudsi                                                                Center for Space Physics, BU                                                 qudsira@bu.edu

Magnetic shear:

\cos(\theta) = \left(\textbf{B}_{\rm sh} \cdot \textbf{B}_{\rm msp}\right)/ \left(|\textbf{B}_{\rm sh}| |\textbf{B}_{\rm msp}|\right)
B_{\rm rec} = |\textbf{B}_{\rm msp} \cdot \textbf{i}_{\rm xn}|

Local field bisection:

Reconnection field energy:

E \propto \left(B_{\rm sh}^2 \times B_{\rm msp}^2\right)

Exhaust speed:

V_{\rm A} = \left[\frac{B_{\rm sh} B_{\rm msp} \left(B_{\rm sh} + B_{\rm msp}\right)}{\left(n_{\rm p,msp}B_{\rm sh} + n_{\rm p,sh}B_{\rm msp}\right)} \right]^{1/2}

sh: magnetosheath

msp: magnetosphere

Qudsi                                                                Center for Space Physics, BU                                                 qudsira@bu.edu

DATA

Qudsi                                                                Center for Space Physics, BU                                                 qudsira@bu.edu

Data:

Solar

Wind

T-96 and IGRF Model

OMNI

Cooling-2001 Model

Magnetosheath

Magnetopause

Shue-1998 Model

Data

Solar Wind data: OMNI (propagated to the magnetopause)

Magnetosheath data: MMS (FPI and FGM)

Magnetospheric magnetic field: Models (T96 or T05 and IGRF)

Magnetosheath magnetic field: Models (Cooling model)

x

z

y

GSM coordinate system

Qudsi                                                                Center for Space Physics, BU                                                 qudsira@bu.edu

Methodology

Qudsi                                                                Center for Space Physics, BU                                                 qudsira@bu.edu

Methodology

Qudsi                                                                Center for Space Physics, BU                                                 qudsira@bu.edu

  • Look at the instances when MMS observed a jet reversal while crossing the magnetopause.

Magnetosheath

Magnetosphere

[Broll et al., 2017]

Qudsi                                                                Center for Space Physics, BU                                                 qudsira@bu.edu

Methodology

Qudsi                                                                Center for Space Physics, BU                                                 qudsira@bu.edu

  • Look at the instances when MMS observed a jet reversal while crossing the magnetopause.
  • For the given parameters of IMF, Magnetosheath and Magnetosphere and Magnetopause find the predicted x-line locations.
  • Find the distance of x-line from MMS, along the magenosheath field, for different models.
  • Look at the statistical distribution of distances (histogram etc.) for different models.

RESULTS

Qudsi                                                                Center for Space Physics, BU                                                 qudsira@bu.edu

The maximum shear model

The maximum exhaust velocity model

Qudsi                                                                Center for Space Physics, BU                                                 qudsira@bu.edu

DISCUSSIONS

Qudsi                                                                Center for Space Physics, BU                                                 qudsira@bu.edu

Discussions:

Most model fail when the z-component of magnetic field is positive. Though bisection model seems to perform better than other 3.

The spread in the histogram of shear model appear to be maximum.

Need a lot more reconnection events for a better understanding.

As expected, different models predict different location of x-lines for the same dataset.

Qudsi                                                                Center for Space Physics, BU                                                 qudsira@bu.edu

Thank You!

Qudsi                                                                Center for Space Physics, BU                                                 qudsira@bu.edu

Link to the presentation

MMS Reconnection Meeting

By Ramiz Qudsi

MMS Reconnection Meeting

A comparative study of reconnection X-line predictions on dayside magnetopause of Earth. Magnetic reconnection is a fundamental plasma process of key importance to several fields. Reconnection at Earth’s magnetopause drives magnetospheric convection and provides mass and energy input into the magnetosphere/ionosphere system. Despite this importance, the factors governing the location of dayside magnetopause reconnection are not well understood. Though a few models can predict X-line locations reasonably well the underlying physics is still unresolved. In this study we present results from an intensive analysis of over 100 reconnection regions observed by MMS to determine what quantities are most strongly associated with the occurrence of dayside magnetopause reconnection. We also attempt to answer under what upstream conditions are global X-line models least reliable.

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