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SHELLS-hires (1)

Specifying High-altitude Electrons using Low-altitude LEO Satellites

Model Description

The SHELLS electron radiation belt model was developed to easily and accurately describe the near-Earth electron flux environment both in real time and retrospectively in order to monitor and analyze space weather impacts to satellites on-orbit. The high energy electrons modeled by SHELLS can penetrate through satellite shielding and build up charge in dielectric materials and on spot shields sometimes resulting in a sudden electrical discharge that triggers anomalous satellite behavior. The model specifies electron flux at high altitude locations (L=3-6.3 and a range of near equatorial and off equatorial magnetic field values) by mapping electron fluxes measured at low altitudes (~850 km) by the POES/MetOp satellite constellation using a neural network derived algorithm.   

Model Figure(s) :

Model Inputs Description

SHELLS is driven by near real time measurements of low altitude electron fluxes and the Kp-index. More specifically, it uses the log10 of the integral electron fluxes measured by the MEPED instruments along each complete pass of a POES/MetOp satellite through the radiation belts (L=3-8). The data from each pass are binned into .25 L shell bins that are then mapped to a consistent longitude and hemisphere using statistical asynchronous regression to remove orbital variations (see Green et al. [2021] for details on the input data processing). Additionally, it uses the Kp index and the maximum Kp index in the last 3 days (here Kp is the standard index multiplies by 10)

Model Outputs Description

The general output of the SHELLS model is electron fluxes (#/cm2-s-str-keV) from L=3-6.3 and energies from 200-3000 keV with local pitch angles from 0-90 degrees. 

The SHELLS model provides 2 different real time run products. One is a dataset of electron flux along the trajectory of a GPS satellite. The output for this GPS product is a text file and L binned plots of the electron fluxes for the last 25 days. The output files contain time at a 5-minute cadence, the L shell based on the OP Quiet field (L), the flux (columns called E flux xxx keV) of electrons with local 90-degree pitch angle and energies 200,500,800,1000,2000 keV, the upper and lower quartiles of the flux (columns labeled upper q and lower q), and the local B field from the OP Quiet field model. 

The other dataset contains near equatorial electron flux at a fixed set of L-shells (3,3.5,4,4.5,5,5.5,6) and energies (200-3000 at a 200keV step). The daily JSON files update every hour and contain data at a 1-hour times cadence. The values included in the JSON file are time, Eflux[time,Ls,energy], L[time,L], Bmirror[time,L], upper q[time,L,energy], lower q[time,L,energy], Kp[time], and Kp max[time]. Here upper q is the upper quartile of the electron flux and lower q is the lower quartile. Kp is the Kp index and Kp max is the maximum in the prior 3 days.

Model Caveats


	
	
	
	

Change Log


	
	 
	

Model Acknowledgement/Publication Policy (if any)


	
	
	

Model Domains:

Magnetosphere.Inner_Magnetosphere.RadiationBelt

Space Weather Impacts:

Near-earth radiation and plasma environment (aerospace assets functionality)

Phenomena :

Particle_Dynamics
Seed_Population_for_the_Ring_Current_and_Radiation_Belt/Preconditioning

Simulation Type(s):

Empirical

Temporal Dependence Possible? (whether the code results depend on physical time?)

true

Model is available at?

CCMC

Source code of the model is publicly available?

false

CCMC Model Status (e.g. onboarding, use in production, retired, only hosting output, only source is available):

production

Code Language:

Python

Regions (this is automatically mapped based on model domain):

Contacts :

Janet.Green, ModelDeveloper
Paul.O'Brien, ModelDeveloper
Yihua.Zheng, ModelHostContact

Acknowledgement/Institution :

Space Hazards Applications, LLC
The Aerospace Corporation

Relevant Links :

Publications :

  • Claudepierre, S.G., & O'Brien, T. P. (2020). Specifying high-altitude electrons using low-altitude LEO systems: The SHELLS model. Space Weather, 18, e2019SW002402. https://doi.org/10.1029/2019SW002402
  • Green, J. C., O’Brien, T. P., Claudepierre, S. G., & Boyd, A. J. (2021). Removing orbital variations from low altitude particle data: Method and application. Space Weather, 19, e2020SW002638. https://doi.org/10.1029/2020SW002638
  • Boyd, A. J., Green, J. C., O’Brien, T. P., & Claudepierre, S. G. (2023). Specifying high altitude electrons using low-altitude LEO systems: Updates to the SHELLS model. Space Weather, 21, e2022SW003338. https://doi.org/10.1029/2022SW003338
  • Model Access Information :

    Access URL: https://iswa.gsfc.nasa.gov/iswa_data_tree/model/magnetosphere/SHELLS-hires-v1/
    Access URL Name: Continuous/RT Run (ISWA data tree)
    Repository ID: spase://CCMC/Repository/NASA/GSFC/CCMC
    Availability: online
    AccessRights: OPEN
    Format: HTML
    Encoding: None

    Access URL: https://iswa.gsfc.nasa.gov/IswaSystemWebApp/index.jsp?i_1=720&l_1=74&t_1=381&w_1=640&h_1=520&s_1=2
    Access URL Name: Continuous/RT Run (ISWA layout)
    Repository ID: spase://CCMC/Repository/NASA/GSFC/CCMC
    Availability: online
    AccessRights: OPEN
    Format: HTML
    Encoding: None

    Linked to Other Spase Resource(s) (example: another SimulationModel) :

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