4.6 Article

Climatological analyses of LMA data with an open-source lightning flash-clustering algorithm

期刊

JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES
卷 121, 期 14, 页码 8625-8648

出版社

AMER GEOPHYSICAL UNION
DOI: 10.1002/2015JD024663

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资金

  1. UAH NSF DC3 award
  2. National Science Foundation's Physical and Dynamical Meteorology (NDF PDM) Program [AGS-1063573]
  3. NSF [AGS-1010657]
  4. NOAA [NA14OAR4320125]
  5. Directorate For Geosciences
  6. Div Atmospheric & Geospace Sciences [1429925, 1063966] Funding Source: National Science Foundation
  7. Directorate For Geosciences
  8. Div Atmospheric & Geospace Sciences [1460585, 1352144] Funding Source: National Science Foundation

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Approximately 63 million lightning flashes have been identified and analyzed from multiple years of Washington, D. C., northern Alabama, and northeast Colorado lightning mapping array (LMA) data using an open-source flash-clustering algorithm. LMA networks detect radiation produced by lightning breakdown processes, allowing for high-resolution mapping of lightning flashes. Similar to other existing clustering algorithms, the algorithm described herein groups lightning-produced radiation sources by space and time to estimate total flash counts and information about each detected flash. Various flash characteristics and their sensitivity to detection efficiency are investigated to elucidate biases in the algorithm, detail detection efficiencies of various LMAs, and guide future improvements. Furthermore, flash density values in each region are compared to corresponding satellite estimates. While total flash density values produced by the algorithm in Washington, D. C. (similar to 20flasheskm(-2)yr(-1)), and Alabama (similar to 35flasheskm(-2)yr(-1)) are within 50% of satellite estimates, LMA-based estimates are approximately a factor of 3 larger (50flasheskm(-2)yr(-1)) than satellite estimates in northeast Colorado. Accordingly, estimates of the ratio of in-cloud to cloud-to-ground flashes near the LMA network (similar to 20) are approximately a factor of 3 larger than satellite estimates in Colorado. These large differences between estimates may be related to the distinct environment conducive to intense convection, low-altitude flashes, and unique charge structures in northeast Colorado.

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