Experimentation and numerical simulation of meteoroid ablation

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Presentation transcript:

Experimentation and numerical simulation of meteoroid ablation Lorenzo Limonta, Sigrid Close Space Environment and Satellite Systems Lab

Motivation

Overview Questions: Methods: Simultaneous optical and radar detection What is the global distribution of meteoroid masses entering Earth’s atmosphere? How are meteor size, mass, and velocity related to measurable parameters? Can we better constrain Composition Luminous efficiency τ Ionization probability β Methods: Simultaneous optical and radar detection Modeling Ablation model: from mass and velocity to plasma size, density, and brightness Scattering model: from plasma size and density to radar cross section

Data collection Joint optical and radar experiment conducted at PFISR spring 2014 Two sensitive CMOS cameras, one with a long pass filter (λ > 475 nm) High power PFISR radar capable of detecting meteor head echoes Pointing 75deg elevation, 15 deg azimuth Field of fiew ~9x9 deg

Collected data 03/30/2014 03/31/2014 04/01/2014 04/02/2014 Identified Objects 49 95 136 59 True positive 43 88 94 55 False Positive 6 7 42 4 False Negative N/A Common Events 13 11

Ablation process Courtesy of National Astronomical Observatory of Japan

Ablation process Mass loss models: Optical: Radar: If dv/dt small, v ~ constant  τ(v) ~ constant  I  dm/dt Radar: Under same assumptions: q/β  dm/dt  Radar relation more complicated

Theoretical framework Need solving 2-d coupled equations: Fluid solver gives boundary conditions for ablation solver Ablation solver modifies fluid mesh Fluid solver simplification: Hypersonic flow for stagnation point Similarity solution from 2-D Euler to map distributions of variables from stagnation point Restrict to events below 90 km of altitude Restrict to event with magnitude below 5

Theoretical Framework Ablation: Extreme conditions Unknown parameters Multispeces  different ablation rates Governing equations: Internal energy balance: Specific Heat:

Event of interest

Conclusions Conclusions: Future work: Working model for a simplified 2-d numerical simulation Shown effects of shelled-multi-composition meteoroid models on mass loss Not sufficient to completely capture what detected Shown effects of rotation on mass loss Future work: Crack propagation and fragmentation model (in collaboration with prof. Chiaramonte of Princeton University) Plasma PIC