On the microphysical effects of observed cloud edge charging. (13th May 2015)

• Record Type: Journal Article
• Authors: Harrison, R. G.; Nicoll, K. A.; Ambaum, M. H. P.
• Is Part Of: Quarterly journal of the Royal Meteorological Society. Volume 141:Number 692(2015:Oct.)
• Page Start: 2690
• Page End: 2699
• Publication Date: 2015-05-13
• Subjects: atmospheric electricity -- cloud microphysics -- solar–terrestrial coupling -- teleconnections; Meteorology -- Periodicals; 551.5
• DOI: 10.1002/qj.2554
• Languages: English
• ISSNs: 0035-9009

Abstract

Abstract : Liquid layer clouds are abundant globally. Lacking strong convection, they do not become electrified by the usual thunderstorm mechanisms of collisional electrification between hydrometeors of different phases. Instead, the background global circuit current flow in fair weather is largely unaffected by the layer cloud's presence, and, if the layer cloud is extensive horizontally, the vertical fair weather conduction current passes through the cloud. A consequence of the vertical current flow is that, at the cloud–air boundary where there is a conductivity transition and droplets form or evaporate, droplet charging occurs. Charge can affect both droplet evaporation and droplet–droplet collisions. Using new radiosonde instrumentation, the charge observed at layer cloud edges is evaluated for both these microphysical droplet processes. This shows that the charging is more likely to affect collision processes than activation, for small droplets. Enhancing the collection efficiency of small droplets modifies their evolution and propagates through the size distribution to shorten the autoconversion time‐scale to rain drops, and the cloud radiative properties. Because the conduction current density is influenced by both external (e.g. solar modulation of high‐energy particles) and internal (e.g. El Niño–Southern Oscillation) factors, current flow leading to layer cloud edge charging provides a possible route for expressing solar influences on the climate system and a teleconnection mechanism for communicating internal climate variability.