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The phenomenon is characterized by almost continuous lightning, mostly within the clouds. The lightning produces a great quantity of ozone, though whether or not this contributes to the ozonosphere is a topic of disagreement, given the instability of the storm. [9] [10]
Lightning flashes in the sky over Kemah, Texas, made the nighttime clouds appear as if they were mountains on July 27.
Smooth channel lightning is an informal term referring to a type of cloud-to-ground lightning strike that has no visible branching and appears like a line with smooth curves as opposed to the jagged appearance of most lightning channels. They are a form of positive lightning generally observed in or near the convective regions of severe ...
Indicates that the air below the cloud is dry; can also signify the downdraft region of a storm. Wall clouds A supercell forms and a wall cloud pushes north of Beardstown, Ill. Friday, March 31 ...
Representation of upper-atmospheric lightning and electrical-discharge phenomena Discovery image of a TLE on Jupiter by the NASA Juno probe. [1]Upper-atmospheric lightning and ionospheric lightning are terms sometimes used by researchers to refer to a family of short-lived electrical-breakdown phenomena that occur well above the altitudes of normal lightning and storm clouds.
In June 2019, while shooting the Milky Way at Capo Spartivento in southern Sardinia, Italy, I noticed a distant storm approaching from Africa, presumably Tunisia, with lightning striking every 2 ...
A cumulonimbus incus is a mature thunderstorm cloud generating many dangerous elements. Lightning: this storm cloud is capable of producing bursts of cloud-to-ground lightning. Hail: hailstones may fall from this cloud if it is a highly unstable environment (which favours a more vigorous storm updraft).
To form a storm, this layer must be very large and the temperature at the top of the cloud must be below −20C. Mountains can help trigger atmospheric convection in three ways: [ 2 ] direct lifting at the level of free convection in unstable air, lifting with a synoptic wind that arrives w/ a component perpendicular to the slopes.