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Convection is brought closer to the exosphere by the cross-tail electric field ... are a function of L because the exosphere density drops off with altitude ... – PowerPoint PPT presentation

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Title: Outline


1
An Empirical Phase-Space Analysis of Ring-Current
Dynamics Solar Wind Control of Injection and
Decay
Paul OBrien and R. L. McPherron UCLA/IGPP tpoiii_at_
igpp.ucla.edu
  • Outline
  • Introduction and Review
  • Data Analysis
  • Linear Phase-Space Trajectory
  • Decay Depends on VBs
  • Physical Interpretation
  • Position of Convection Boundary
  • Conclusions

2
Meet the Ring Current
  • During a magnetic storm, Southward IMF reconnects
    at the dayside magnetopause
  • Magnetospheric convection is enhanced hot
    particles are injected from the ionosphere
  • Trapped radiation between L 2-10 sets up the
    ring current, which can take several days to
    decay away
  • We measure the magnetic field from this current
    as Dst

March 97 Magnetic Storm
Recovery
100
0
Dst (nT)
-100
-200
Injection
-300
91
92
93
94
95
96
97
98
99
Pressure Effect
10
VBs (mV/m)
5
0
91
92
93
94
95
96
97
98
99
60
40
Psw (nPa)
20
0
91
92
93
94
95
96
97
98
99
Day of Year
3
DDst Distribution (Main Phase)
No Data
DDst ? Q - Dst/t
Median Trajectory
No Data
4
Motion of Median Trajectory
VBs 0
VBs 1 mV/m
VBs 2 mV/m
VBs 3 mV/m
VBs 4 mV/m
VBs 5 mV/m
As VBs is increased, distributions slide left and
tilt, but linear behavior is maintained.
5
The Trapping-Loss Connection
  • The convection electric field shrinks the
    convection pattern
  • The Ring Current is confined to the region of
    higher nH, which results in shorter t
  • The convection electric field is related to VBs

t Decreases
Larger VBs
6
Fit of t vs VBs
  • The derived functional form can fit the data with
    physically reasonable parameters
  • Our 4.69 is slightly larger than 1.1 from Reiff
    et al.

?
7
How to Calculate the Wrong Decay Rate
  • Using a least-squares fit of DDst to Dst we can
    estimate t
  • If we do this without first binning in VBs, we
    observe that t depends on Dst
  • If we first bin in VBs, we observe that t depends
    much more strongly on VBs
  • A weak correlation between VBs and Dst causes the
    apparent t-Dst dependence

8
Summary
  • Dst follows a first order equation
  • dDst/dt Q(VBs) - Dst/t(VBs)
  • Injection and decay depend on VBs
  • Dst dependence is very weak or absent
  • We have suggested a mechanism for the decay
    dependence on VBs
  • Convection is brought closer to the exosphere by
    the cross-tail electric field

9
Phase Space Trajectories
Simple Decay
Oscillatory Decay
Dst(t)
Dst(t)
Variable Decay
Dst(tdt)-Dst(t)
Dst(tdt)-Dst(t)
Dst(t)
Dst(tdt)-Dst(t)
10
Q is nearly linear in VBs
  • The Q-VBs relationship is linear, with a cutoff
    below Ec
  • This is essentially the result from Burton et al.
    (1975)

11
Speculation on t(VBs)
The charge-exchange lifetimes are a function of L
because the exosphere density drops off with
altitude t is an effective charge-exchange
lifetime for the whole ring current. t should
therefore reflect the charge-exchange lifetime at
the trapping boundary
  • A cross-tail electric field E0 moves the
    stagnation point for hot plasma closer to the
    Earth. This is the trapping boundary (p is the
    shielding parameter)
  • Reiff et al. 1981 showed that VBs controlled the
    polar-cap potential drop which is proportional to
    the cross-tail electric field

12
Neural Network Verification
DDst NN(Dst,VBs,)
  • A neural network provides good agreement in phase
    space
  • The curvature outside the HTD area may not be real

Neural Network Phase Space
0
High Training Density
-50
Dst
-100
-150
-25
-20
-15
-10
-5
0
5
10
15
DDst
13
Small Big Storm Errors
  • More errors are associated with large VBs than
    with large Dst

14
Details of Model Errors in Simulated Real-Time
Mode
ACE availability was 91 (by hour) in 232 days
Predicting large Dst is difficult, but larger
errors may be tolerated in certain applications
15
Calculation of Pressure Correction
  • So far, we have assumed that the pressure
    correction was not important.This is true because

But now we would like to determine the
coefficients b and c. We can determine b by
binning in DP1/2 and removing Q(VBs)
We can determine c such that Dst decays to zero
when VBs 0
16
Small Big Storms
17
Comparisons to Other Models
ACE Gap
AK2 is the new model, Kyoto is the target, AK1 is
a strictly Burton model, and UCB has slightly
modified Q and t. AK2 has a skill score of 30
relative to AK1 and 40 relative to UCB for 6
months of simulated real-time data availability.
These numbers are even better if only active
times are used.
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