Post on 02-Jan-2016
description
Storm-dependent Radiation Belt Dynamics
Mei-Ching FokNASA Goddard Space Flight Center, USA
Richard Horne, Nigel Meredith, Sarah GlauertBritish Antarctic Survey, UK
AOGS 5th Annual General Meeting16-20 June 2008
Busan, Korea
ST03-A008
Motivation
Taken from Reeves et al., 2003
Outline
Model the radiation belt enhancements during the storms in October 2002
Two-step acceleration processes –– What causes post-storm enhancement in the outer belt?
Real-time running of the RBE model at NASA Goddard
The Radiation Belt Environment (RBE) model Model logic Model formulation Model input/output
The Radiation Belt Environment (RBE) Model
Solar Wind, Dst, Kp data
Radiation Belt Environment Model
Energetic Electron Flux(10 keV – 6 MeV)
Magnetic Field and Electric Field Models
Plasmasphere Model
WaveDiffusion Model
Plasma Sheet Model
Radiation Belt Environment Model: The Equation
€
fs = f s t,λ i,φi,M,K( )
€
λi
: phase space density of electrons
: magnetic latitude at the ionosphere
€
φi : magnetic local time at the ionosphere
M : magnetic moment
K : longitudinal invariant
€
˙ λ i , ˙ φ i : drift velocities (convection + magnetic drift + corotation)
€
∂fs
∂t+ ˙ λ i
∂fs
∂λ i
+ ˙ φ i∂fs
∂φi
=1
E + Eo( ) E E − 2Eo( )
∂
∂EE + Eo( ) E E − 2Eo( )DEE
∂fs
∂E
⎛
⎝ ⎜
⎞
⎠ ⎟
+1
T(α o)sin2α o
∂
∂α o
T(α o)sin2α oDα oα o
∂fs
∂α o
⎛
⎝ ⎜
⎞
⎠ ⎟−
fs
0.5τ b
⎛
⎝ ⎜
⎞
⎠ ⎟losscone
€
T(α o) =1
2Ro
ds
cosαsm
sm*
∫
b: bounce period
Radial diffusion is included implicitly in the time-varying magnetic and electric fields.
Radiation Belt Environment Model: The Input
Dst, Kp: Kyoto University Geomagnetic Data Service
Shifted solar wind data: ACE or WIND satellite
Magnetic field model: T96 or T04 model
Electric field model: Weimer model
Plasmasphere model: Ober and Gallagher model
Diffusion coefficients: Horne’s PADIE code
Distribution at the outer boundary (10 RE): kappa distribution Nps(t) = [(0.02 Nsw(t-2hr) + 0.316)] sqrt(amu) cm^-3Eo(t) = 0.016 Vsw(t-2hr) - 2.4 keV
The PADIE Code: Pitch Angle and Energy Diffusion of Ions and Electrons
Electron diffusion rates for whistler mode chorus waves (wave amplitude = 100 pT)
Taken from Horne et al., 2006
CRRES Lower-band Chorus Wave Data
Provided by N. Meredith
Radiation Belt Environment Model: The Output
RBE Output: 3-dimensional Electron Flux from 10 keV to 6 MeV at all pitch angles
800 keV electrons
Magnetic Storm on 23 - 27 October 2002
RBE Simulation of the Storm on 23 - 27 October 2002
Pre-storm
Early recovery
RBE Simulation of the Storm on 23 - 27 October 2002
Pre-storm
Storm on Oct 23-27, 2002: RBE Simulations versus LANL-SOPA Data
Storm on Oct 23-27, 2002: RBE Simulations versus SAMPEX Data
SAMPEX: electrons: 2 – 6 MeV RBE–T04 with WP interactions
Storm on Oct 23-27, 2002: RBE Simulations versus SAMPEX Data
SAMPEX: electrons: 2 – 6 MeV RBE–T04 with WP interactions RBE–T04 without WP interactions
Storm on Oct 23-27, 2002: RBE Simulations versus SAMPEX Data
SAMPEX: electrons: 2 – 6 MeV RBE–T04 with WP interactions RBE–T96 with WP interactions
Two-Step Acceleration of the Outer Belt
No WP interactions With WP interactions
RBE with T04
RBE with T96
The RBE Model Running in Real Time
Real-time ACE data:Nsw, Vsw, IMF (NOAA)
Real-time Dst (Kyoto U.) and Kp (NOAA)
Radiation Belt Environment (RBE) Model
Energetic Electron Flux(updated every 15 minutes)
Real-time GOES-11(E > 0.6 MeV)
Real-time GOES-12(E > 0.6 MeV)
http://mcf.gsfc.nasa.gov/RB_nowcast/
Summary
A data-driven physical model of the radiation belt (RBE model) has been developed to understand the radiation belt dynamics and provide prediction of the radiation belt environment.
Storm on 23-27 October 2002 was simulated. We found a two-step acceleration in the outer belt:
1. Particle injection and radial transport form a seed population
2. Further energization by interacting with waves
Storms that are not able to produce seed population or wave excitation have no radiation belt enhancement.
The RBE model is running in real-time at NASA Goddard and compared with GOES data:
http://mcf.gsfc.nasa.gov/RB_nowcast