Solar Cycle Dependence of Mass Density and Ion Composition at Geosynchronous Orbit

6
Solar Cycle Dependence of Mass Density and Ion Composition at Geosynchronous Orbit Richard E. Denton, Dartmouth Kazue Takahashi, APL Michelle Thomsen, LANL

description

Solar Cycle Dependence of Mass Density and Ion Composition at Geosynchronous Orbit. Richard E. Denton, Dartmouth Kazue Takahashi, APL Michelle Thomsen, LANL. Solar Cycle Dependence. Mass density. MPA ion density. f10.7. f10.7. Same But Just on Dayside. - PowerPoint PPT Presentation

Transcript of Solar Cycle Dependence of Mass Density and Ion Composition at Geosynchronous Orbit

Page 1: Solar Cycle Dependence of Mass Density and Ion Composition at Geosynchronous Orbit

Solar Cycle Dependence of Mass Density and Ion Composition at Geosynchronous Orbit

Richard E. Denton, Dartmouth

Kazue Takahashi, APL

Michelle Thomsen, LANL

Page 2: Solar Cycle Dependence of Mass Density and Ion Composition at Geosynchronous Orbit
Page 3: Solar Cycle Dependence of Mass Density and Ion Composition at Geosynchronous Orbit

Solar Cycle DependenceMPA ion densityMass density

f10.7 f10.7

Page 4: Solar Cycle Dependence of Mass Density and Ion Composition at Geosynchronous Orbit

Same But Just on Dayside

Page 5: Solar Cycle Dependence of Mass Density and Ion Composition at Geosynchronous Orbit

MPA, total, low energy, and high energy – Still Dayside

Page 6: Solar Cycle Dependence of Mass Density and Ion Composition at Geosynchronous Orbit

Conclusions

• At geosynchronous orbit, the mass density peaks at solar maximum while ion density peaks at solar minimum, the opposite of the expected trend for electron density

• This implies a much higher concentration of O+ at solar maximum.

• VERY preliminary and not quite right: MPA underestimates ion density by a factor of 4 for O+. Assuming a H+/O+ plasma, we can use the average values at solar max and solar min to find nO+/ne = 0.42 and average ion mass M = 7 at solar max, and nO+/ne = 0.08 and M = 2.2 at solar min.