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Overview
! Big Picture and goal of my project
! Poynting Flux
! Southward IMF (generally well understood)
! Methodology
! Northward IMF (remotely understood but not clear)
! Case Studies
! Conclusion
! Questions
Big Picture
! From DMSP, determine where Poynting Flux (electromagnetic energy) is being deposited in reference to the auroral boundary.
! Determine the locations, associations and drivers of extreme Poynting Flux in or around the polar cap region.
! Improve the estimation of the local and large-scale electric and magnetic field estimates to provide estimates of the energy extracted from all energy sources to power the upper atmosphere.
What is Poynting Flux?
• Poynting Flux is electromagnetic-wave energy passing through some surface.
• Poynting Flux is derived, not a direct measure from spacecraft.
E B
PF
Note that the Hall currents are opposite in direc6on to the convec6on because they are carried by the electrons
Weimer, D. R. (2005), Improved ionospheric electrodynamic models and applica6on to calcula6ng Joule hea6ng rates, J. Geophys. Res., 110, A05306, doi:10.1029/2004JA010884.
Methodology
! DMSP F13 F15 F16.
! How Poynting Flux is derived.
! 12 separate cases.
! Timing of events.
y = 3.899x -‐ 63.543 R² = 0.06611
-‐160
-‐140
-‐120
-‐100
-‐80
-‐60
-‐40
-‐20
0 0.00 2.00 4.00 6.00 8.00 10.00
Poyn%n
g Flux (m
W/m
^2)
Alfven Mach #
Mach #
Mach #
Linear (Mach #)
Linear (Mach #)
y = -‐1.5057x -‐ 32.346 R² = 0.16412
-‐160
-‐140
-‐120
-‐100
-‐80
-‐60
-‐40
-‐20
0 0 5 10 15 20 25 30 35 40
Poyn%n
g Flux (m
W/m
^2)
IMF Bx (nT)
Mag IMF Bx
Mag IMF Bx
Linear (Mag IMF Bx)
y = -‐0.0932x + 8.7008 R² = 0.20978
-‐160
-‐140
-‐120
-‐100
-‐80
-‐60
-‐40
-‐20
0 0 200 400 600 800 1000
Poyn%n
g Flux (m
W/m
^2)
Solar Wind Speed
Solar Wind Speed
Speed
Linear (Speed)
y = -‐5.3459x -‐ 2.8035 R² = 0.47085
-‐160
-‐140
-‐120
-‐100
-‐80
-‐60
-‐40
-‐20
0 0.00 5.00 10.00 15.00 20.00
Poyn%n
g Flux (m
W/m
^2)
Ey: Solar Wind Electric Field from Bsw trans*Vsw
E SolarWindTrans
Eswtrans
Linear (Eswtrans)
Conclusions
! Poynting flux deposition during northward IMF can be extreme.
! The primary responding parameter is Low Earth Orbit (LEO) Delta By (eastward dB) associated with field aligned currents.
! An external driver is the fast delivery of the transverse IMF that has a good correlation with Poynting Flux.
! The next step in this project will be to look at a lot larger sample size of events that meet our parameterizations.
A Huge Thank You
! Delores Knipp
! Liam Kilcommons
! Erin Wood
! DMSP data providers
! NASA
! OMNIWeb