4.7 Article

Duration, spatial size and radiance of lightning flashes over the Asia-Pacific region based on TRMM/LIS observations

Journal

ATMOSPHERIC RESEARCH
Volume 223, Issue -, Pages 98-113

Publisher

ELSEVIER SCIENCE INC
DOI: 10.1016/j.atmosres.2019.03.013

Keywords

Flash duration; Flash spatial size; Flash radiance; TRMM/LIS

Funding

  1. National Key Research and Development Program of China [2017YFC1501503]
  2. National Natural Science Foundation of China [41675005, 91537209]
  3. Basic Research Fund of Chinese Academy of Meteorological Sciences [2016Z002]
  4. Japan National Space Development Agency (NASDA)
  5. National Aeronautics and Space Administration's (NASA) Office of Earth Science

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The geographical distributions of flash duration, length, footprint and radiance, as well as their correspondence with thunderstorm structures, are investigated for the first time in the Asia-Pacific region ranging from 70 degrees E to 160 degrees E and from 18 degrees N to 36 degrees N and in six specially chosen regions by employing flash data collected by the Lightning Imaging Sensor (LIS) aboard the Tropical Rainfall Measuring Mission (TRMM) satellite and TRMM-based radar precipitation feature (RPF) data from 2002 to 2014. The flash length, footprint and radiance values are, on average, the largest over the deep ocean, followed by offshore waters and land. Flash duration is the longest over the offshore waters near the east coast of China, followed by the deep ocean and land. The Tibet Plateau and the northern part of the Indian Peninsula have the weakest flash properties in the study region. Furthermore, the geographic distributions of the flash properties exhibit evident seasonal changes. The monotonic relationship between flash spatial size and radiance is stronger than the monotonic relationships between flash duration and spatial size or radiance. Based on a comparison of the seasonal and regional changes in flash properties with RPF properties, convective intensity is proposed to play a crucial role in characterizing the flash spatial size and radiance, according to their inverse correlation in most regions. However, the climatological correspondence between flash duration and thunderstorm structures remains poorly constrained. We have launched a discussion of the possible association between thunderstorm structures and flash properties.

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