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Robert J. Trapp, Karen A. Kosiba, James N. Marquis, Matthew R. Kumjian, Stephen W. Nesbitt, Joshua Wurman, Paola Salio, Maxwell A. Grover, Paul Robinson, and Deanna A. Hence

Electrification, Lightning, And Mesoscale/microscale Processes with Adaptive Ground Observations (RELAMPAGO) field program, funded primarily by the National Science Foundation ( Nesbitt et al. 2016 ), and the complementary Clouds, Aerosols, and Complex Terrain Interactions (CACTI) field program funded by the Department of Energy Atmospheric Radiation Measurement (DOE-ARM) program ( https://www.arm.gov/publications/programdocs/doe-sc-arm-19-028.pdf ). The detailed justification for RELAMPAGO-CACTI, as well as

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James N. Marquis, Adam C. Varble, Paul Robinson, T. Connor Nelson, and Katja Friedrich

(1315–1415 local time) (e.g., Fig. 1a ). At least five precipitation cores reached a maximum C-band radar reflectivity greater than 50 dB Z at low levels and persisted for a duration between 1 and 2.5 h. A mesoscale radiosonde network consisted of hourly launches between 1300 and 1900 UTC from six mobile facilities ( Schumacher 2019 ; Wurman and Kosiba 2021a ) and every three hours from the U.S. Department of Energy Atmospheric Radiation Measurement (ARM) Mobile Facility (AMF) instrument site

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