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70 Years of Magnetospheric Modeling A Tutorial George Siscoe Center for Space Physics Boston University. Preliminaries. Historical Approach Five Model Uses 1. Models that Represent Empirical and AI 2 . Models that Explain Modular 3. Models that Reveal
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70 Years of Magnetospheric Modeling A Tutorial George SiscoeCenter for Space PhysicsBoston University
Preliminaries • Historical Approach • Five Model Uses • 1. Models that Represent • Empirical and AI • 2. Models that Explain • Modular • 3. Models that Reveal • Kinetic and MHD • 4. Models that Interpret • All Types • 5. Models that Predict • All Types • This Talk Considers only Modular and MHD Models that Explain and Reveal
Outline • Three Approaches • 1. Modular • 2. Regional MHD • 3. Global MHD • Future Directions
Modular 1930s: Inception of Chapman-Ferraro model
Midgley and Davis 1963 Midgley and Davis 1963 Mead 1964 Early ‘60s: Culmination of the C-F project
Midgley and Davis 1963 Mead 1964 Ness 1965 Fairfield 1968 Mid ‘60s: Discovery of the tail and the magnetosheath
Summary of Chapman-Ferraro Epoch: • Well posed, fully explicit formulation • Analytic solutions possible • Size & shape of the magnetopause found • Dependence on S/W ram pressure found • Dependence on dipole tilt found • Global force balance understood • But downhill from here • No storms • Empty tail • No magnetosheath
Luhmann et al., 1984 Modular Magnetosheath: Spreiter & Co.
Modules for the closed tail: • Current specification • C-F approach • Prescribed magnetopause • Analytic tail approximation • Convection added
Mead and Williams 1965 Olson and Pfitzer 1974 Bird 1979 Modular Current Specification
Unti and Atkinson 1968 Siscoe 1966 Chapman-Ferraro approach to modeling the closed tail Spreiter and Alksne 1969
Prescribed magnetopause approach to modeling the closed tail Schulz source surface model Voigt stretch model Schulz source surface model
Analytic tail approximationsand convection:The Birn-Schindler project
Summary of Closed-Tail Epoch: • Ill posed but fully explicit formulations • Results depend on assumptions and approach • Analytic solutions still possible but superceded by computational solutions • Global force balance understood • Magnetotail B-field modeled • In particular, Bz dependence on x modeled • Dipole tilt geometry modeled • Polar cap geometry and tilt dependence modeled • Role of field-aligned currents discovered • “Convection time dependence” discovered • Modules for open tail models developed • Initial state for regional MHD model developed • But still no solar wind coupling • No convection electric field
Modules for the Open Magnetosphere: • The Stern-singularity problem • The Toffoletto-Hill solution • Region 1 current modeling • The SSM (Peroomian) extension
The Stern-singularity problem E parallel Siscoe 1988
T-H T-H and SSM compared SSM (P)
Peroomian et al. 1991 Siscoe et al. 1991 Region 1 Currents: SSM (P)
Summary of Open-Tail Epoch: • Ill posed but fully explicit formulations • Results depend on assumptions and approach • Analytic solutions still possible but superceded by computational solutions • Magnetotail B-field modeled • Polar cap potential modeled • Stern singularity overcome in TH not in SSM • Region 1 currents in SSM not in TH • No plasma • No physics for field-aligned currents
Jaggi & Wolf 1973 Vasyliunas 1970 Magnetosphere-Ionosphere Coupling Modules
RCM Master Plan Rice Convection Model (RCM) The Wolf & Co. project
Equilibrium RCM Toffoletto 2000 Summary of MI Coupling Epoch: • Well posed fully explicit • Analytic solutions possiblesuperceded by computations • Assumed potential and plasma at boundaries • Inner magnetosphereplasma modeled • Physical region 2 currents • No region 1 currents • First RCM-MHD results
Regional MHD Plasmoid Kelvin-Helmholtz wave Flux transfer event
Plasmoid Simulation Lee et al. 1985
Kelvin-Helmholtz Simulation Otto & Fairfield 2000
FTE Simulation Scholer 1989
Global MHD • Open geometry • Magnetospheric sash • E-Parallel & reconnection
Raeder GGCM Web Site Open Geometry
-10 -5 -2 0 -1 2 -10 IMF 4 1 IMF -5 3 + 5 X=6 + + X=7 + -10 -5 + 0 2 4 6 X=8 IMF Magnetospheric Sash
Future Directions Hybrids Other Magnetospheres Deep Questions
Acknowledgements Bill White Keith Siebert Dan Weimer Bengt Sonnerup Nelson Maynard Gary Erickson NSF NASA DTRA