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)
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Link to the presentation
1, * 1 2
1 2
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Outline:
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The BASICS
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Source: NASA
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[Broll et al., 2017]
Source: wikipedia
Magnetic Reconnection
Why Magnetic Reconnection?
Gotta work on something!
Why not?
Ubiquitous nature of reconnection
Energy dynamics
Dynamo effect
Region of interest:
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Location of x-line
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]
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Magnetic shear:
Local field bisection:
Reconnection field energy:
Exhaust speed:
sh: magnetosheath
msp: magnetosphere
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DATA
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)
Observational 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
Magnetopause stand-off point: Models (Shue Model)
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Magnetosheath
Magnetosphere
[Broll et al., 2017]
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RESULTS
The maximum shear model
The maximum exhaust velocity model
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DISCUSSIONS
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Discussions:
Most model fail when the z-component of magnetic field is positive. Though reconnection energy model seem 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.
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Link to the presentation
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Link to the presentation
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If Paul asks his question: