Vanna C. Chmielewski- Feb 1- Convective Meteorology
Anomalous charge structures, those containing net positive charge in the mid-levels (-10 °C to -30 °C) and promoting positive cloud-to-ground flashes, have been associated with updrafts producing abundant supercooled liquid water. However, surrounding the updraft core many processes act to limit supercooled liquid water content (e.g. locally lower updraft velocities, ingestion of cloud ice, entrainment) […]