1. MP BACH MultiPixel Balloon-borne Air CHerenkov Detection of Iron Cosmic Rays Using Direct Cherenkov Radiation Imaged with a High Resolution Camera 1

3. Energy spectrum of Iron cosmic rays multiplied by E 2.5 from different observations. JACEE and RUNJOB, emulsion instruments, are a compilation of many balloon flights. CRN was conducted on the space shuttle. CREAM, ATTC and TRACER are balloon payloads flown from Antarctica and Sweden. BACH payload was flown from Ft Sumner. Sood pioneered the BACH technique. KASKADE (two different interaction models) and EAS-TOP (upper and lower limits) are air shower data. HESS data (two different interaction models) are ground level observations of Cerenkov light imaging. Current knowledge of the iron spectrum

5. Altitude (km) Distance from Axis (m) 35km 75km 8 -8 0 As the particle penetrates into denser air, the Cherenkov angle and intensity increase. First photons are emitted just on the axis defined by the particle path, but subsequent photons lie further and further from the axis when they reach any given depth in the atmosphere forming a circular spot or “pool” of light. This trend continues until the particle is roughly two scale heights (15 km) above an observer, when proximity finally wins out.

6. CORSIKA Simulations 6 Simulates detailed particle propagation and generates CK photons QGSJET Hadronic Interaction model

7. Light Pool at 35 km Altitude 7

8. Idealized Detector Images, xGeV Fe Non- Interacting 8

9. z y x θ φ (x o,y o ) (x 1,0) (x 2,0) Camera 1 Image Camera 2 Image Example MPBACH Simulated Event Cartoon degrees

10. Charge/Energy

11. Deflection in the Earth’s Magnetic Field * Energy & Charge dependence * 11

14. Extra slides

15. Pixilated Camera Image 15

16. εc is the CK emission vector as viewed from Camera 1 and 2 z y x θ φ (x o,y o ) (x 1,0) (x 2,0) θ cL Pathlength to emission point S εc b θ cH εc a Intersection of Plane C 1 and C 2 forms a line that lies along the particle trajectory cross product of these two normal C1 and C2 vectors gives a vector which is perpendicular to both of them and which is therefore parallel to the line of intersection of the two planes. So this cross product will give a direction vector for the line of intersection. Set z=0 and solve for x and y With only the DCs, reconstruct trajectory Camera 1 event plane Camera 2 event plane Directional cosine observations from the camera and camera location on the gondola

17. z y x θ φ (x o,y o ) (x 1,0) (x 2,0) θcθc Pathlength to emission point Particle trajectory passes through the x,y plane at location x o,y o The particle incident angle with respect to z is θ and φ is the polar θ c = Cerenkov angle which is a function of z (air density) S is the trajectory straight path-length from the x-y plane intersection to the CK emission point as viewed by camera 1 εc is the CK emission vector as viewed from Camera 1 y x Camera 2Camera 1 z x1x1 No Magnetic Field It can be shown that S is related to the other quantities as S εc

18. If the steepening at the cosmic ray knee is caused by a magnetic rigidity dependent mechanism, as a result of an acceleration process limited in a rigidity dependent manner or rigidity dependent propagation, there should be systematic changes in the cosmic ray composition through this region. It is difficult to see how SN could accelerate protons to energies much beyond ~10 15 eV/particle. Heavier cosmic rays, for example iron nuclei, could reach energies over an order of magnitude higher than this via the same mechanism. The objective of this project is to improve our knowledge of the Iron Flux from 5x10 3 to 3x10 6 GeV

19. z y x θ φ (x o,y o ) (x 1,0) (x 2,0) θ cL Pathlength to emission point S εc b θ cH εc a Explicitly determine the relationship for the x,y crossing point at z=0

20. Directional cosine observations from the camera and camera location on the gondola The trajectory vector S has been determine and is then used to calculate the Cerenkov angle at each intersection point The index of refraction at each intersection altitude point must be determined to calculate the energy z y x θ φ (x o,y o ) (x 1,0) (x 2,0) θcbθcb Pathlength to emission point S εc b θcaθca εc a

21. ThetaC (degrees) Altitude (km)

22. Results The calculated energy uses only the directional cosines, camera location and atmospheric model