WebFeb 1, 2013 · Total lightning refers to all lightning in and between thunderstorms including in-cloud (IC) and cloud-to-ground (CG) lightning activity. The National Lightning Detection … WebJun 28, 2016 · Abstract. Total lightning has been shown to correlate well with thunderstorm dynamics. Thus, correlations may exist between in-cloud convective turbulence and total lightning activity. Over the continental United States, the NEXRAD Turbulence Detection Algorithm (NTDA) provides three-dimensional (3D) fields of in-cloud Eddy Dissipation Rate …
What is the relationship between lightning and thunder - Brainly
WebJul 11, 2024 · artodell. A single stroke of lightning can heat the air around it to 30,000°C (54,000°F)! This extreme heating causes the air to expand explosively fast. The expansion … WebJan 4, 2013 · [1] Phased array radar with unprecedented high temporal and spatial resolution is used for the first time to analyze structures of thunderstorms producing lightning narrow bipolar events (NBEs). Locations of NBEs generally correspond well with the deepest convection, but in some thunderstorms extending higher than 15 km, positive NBEs … caa licensing and training standards
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WebAug 26, 2011 · Lightning is fast and very hot while thunder can usher in heavy rain and strong winds, but lightning is more dangerous and destructive than thunder. 4. Lightning is formed when water and ice particles collide with warm, moist air and build up static energy while thunder is formed by the fast expansion of gases in the electrical charge of lightning. WebJun 19, 2010 · For lightning systems over land, the total area of radar echo above 35 dBZ has a closer relationship with lightning flash rate at the temperature between −5°C and −15°C than other parameters. Area of lower radar reflectivity at colder temperature, e.g., area of 20 dBZ at −40°C, is also highly correlated with lightning frequency. WebJun 8, 2016 · 4. Lightning and thunder. The best known of the light signatures of a storm is lightning. It results from the ionization of the air in a scenario that can be summarized as follows . Collisions between different ice particles are accompanied by exchanges of electrical charges whose polarity depends on temperature. ca a lighter melt wax