Ground Flash Fraction Retrieval Algorithm GLM Science Meeting Huntsville, AL September 24, 2013 Dr. William Koshak, NASA-Marshall Space Flight Center Dr.

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Presentation transcript:

Ground Flash Fraction Retrieval Algorithm GLM Science Meeting Huntsville, AL September 24, 2013 Dr. William Koshak, NASA-Marshall Space Flight Center Dr. Richard Solakiewicz, Chicago State University

Summary of Main Advances  Mathematical Advances to Analytic Perturbation Method  Derived closed form solution for ground flash fraction … no numerical scanning of H function.  Derived explicit analytic forms for the perturbation vectors.  Derived a way to determine flash type of specific flashes.  APM Error Analysis Completed Via Simulations  DEMO Completed  Journal Paper Completed & Ready for Submission (JTECH)

MIX Instrument Observes N MGAs. Invert this Distribution to Find Ground Flash Fraction α

APM SOLUTION PROCESS (truth) (model)

PROBABILITY FLASH, HAVING MGA = x, IS A GROUND FLASH: APM SOLUTION SUMMARY PERTURBATION GIVES:

Simulate Population from OTD Data (Flash Type Categorized by NLDN)

Simulate Population from LIS Data (Flash Type Categorized by NLDN)

EFFECT OF RANDOM ERROR (a = g, b = c) NONE 8 km2 16 km2 32 km264 km2

EFFECT OF RANDOM ERROR (a and b from method) NONE 8 km2 16 km2 32 km264 km2

EFFECT OF SYSTEMATIC ERROR (a = g, b = c) NONE 8 km2 16 km2 -8 km2-16 km2 DIGITAL (16 km2 finite footprint)

EFFECT OF SYSTEMATIC ERROR (a and b from method) NONE 8 km2 16 km2 -8 km2-16 km2 DIGITAL (16 km2 finite footprint)

EFFECT OF CLIMATOLOGY SAMPLE SIZE Ng = 40,000 Nc = 120,000 Ng = 10,000 Nc = 30,000 Ng = 5,000 Nc = 5,000 Ng = 1,000 Nc = 1,000 Ng = 500 Nc = 500 Ng = 200 Nc = 200

EFFECT OF OBSERVATION SAMPLE SIZE N N = 5,000N = 7,500N = 2,500 N = 1,000 N = 500

NOMINAL (LIS data) # Observations: N = 5000 # in Climate Sampling: Ng = 40,000 Nc = 120,000 Instr. Measurement Error: Random = ±32 km2 Systematic = 16 km2 digital gpop mean = km2 cpop mean = km2 difference = km2 Mean Error = Std = 0.022

NOMINAL (OTD data) # Observations: N = 5000 # in Climate Sampling: Ng = 40,000 Nc = 120,000 Instr. Measurement Error: Random = ±128 km2 Systematic = 64 km2 digital gpop mean = km2 cpop mean = km2 difference = km2 Mean Error = Std = 0.014

CAN HANDLE ARBITRARY DISTRIBUTIONS (AS USUAL, CG & IC DISTRIBUTIONS NEED TO BE DISTINCT)

PERFORMANCE OF SPECIFIC FLASH TYPING Mean Fraction Correct = Std = LIS data Mean Fraction Correct = Std = OTD data

FUNCTIONAL DEMO NOW EXISTS

Thank You